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"indenting" Synonyms
gouging denting marking depressing nicking notching cutting dinting pitting furrowing scratching grooving hollowing gashing incising engraving slitting snicking scoring carving ordering requesting requisitioning claiming demanding applying for calling for putting in for asking for putting in an order for putting in a request for putting in a claim for booking securing reserving engaging obtaining soliciting seeking commissioning tabbing padding spacing moving to the right moving further from the margin starting in from the margin impressing etching imprinting inscribing stamping printing branding chiseling(US) chiselling(UK) ingraining infixing engraining embossing debossing punching setting curling curving winding twisting coiling bending arching turning spiraling(US) spiralling(UK) looping crooking snaking meandering twirling corkscrewing zigzagging twining entwining rolling sculpting sculpturing chipping fashioning forming hewing whittling hacking slashing shaping graving slicing More
"indenting" Antonyms
flushing outdenting raising unindenting

307 Sentences With "indenting"

How to use indenting in a sentence? Find typical usage patterns (collocations)/phrases/context for "indenting" and check conjugation/comparative form for "indenting". Mastering all the usages of "indenting" from sentence examples published by news publications.

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She underscores the clay's susceptibility to pressure by puncturing or indenting it.
Indenting makes the start of each new paragraph clear to the reader, and makes lists crisper and easier to appreciate visually.
But Jennifer Garner is indenting your Instagram a bit early, with a cute throwback photo from when she attended the Met Gala.
It took an animal to beat a woman they were sex trafficking with a bat 28 times, indenting part of her body.
It took an animal to beat a woman — they were sex trafficking — with a bat 28 times, indenting part of her body.
He has a tic, omnipresent in "All That Man Is," of indenting new sentences in new lines, as if he were writing kids' poetry.
Image: HBOIt's one of the greatest battles ever fought among coders: Should you use the tab button or five spaces when you're indenting in source-code?
The beta program will include new features like speech bubbles, indenting, and different colors determined by whether you follow someone or are replying, according to a Twitter representative.
For 18 months Amazon has sold a counterfeit of Agatha Christie's "Murder on the Orient Express" despite warnings in reader reviews that it is a "monstrosity," dispensing with such standard features as proofreading and paragraph indenting.
It took an animal to beat a woman they were sex trafficking with about 28 times and indenting part of her body, and it took an animal to kidnap, drugged, and rape a 14-year-old Houston girl.
While indenting the first line of every new paragraph is no longer the standard for digital publishing, adding that bit of space is the standard practice for text layout in books, in most legal and legislative documents, and in many other forms of writing.
The paper is thick enough for you to bear down hard without indenting other pages and without ink bleeding through, and the book gets the "Frame" part of its name because the perforated pages can easily be torn out for hanging on the fridge or even framing for proper presentation.
The off-side rule (blocks determined by indenting) can be implemented in the lexer, as in Python, where increasing the indenting results in the lexer emitting an INDENT token, and decreasing the indenting results in the lexer emitting a DEDENT token. These tokens correspond to the opening brace `{` and closing brace `}` in languages that use braces for blocks, and means that the phrase grammar does not depend on whether braces or indenting are used. This requires that the lexer hold state, namely the current indent level, and thus can detect changes in indenting when this changes, and thus the lexical grammar is not context-free: INDENT–DEDENT depend on the contextual information of prior indent level.
Mindya Cove, named for Mindya, Bulgaria, is cove indenting the island's northwest coast for .
The coastline of the island is developed, with many inlets indenting the coastline in the west.
The coastline of the island is developed, with many inlets indenting the coastline, particularly in its northern part.
Lewis Bay is a bay indenting the north coast of Ross Island, Antarctica, between Mount Bird and Cape Tennyson.
Simple Outline XML (SOX) is a compressed way of writing XML. SOX uses indenting to represent the structure of an XML document, eliminating the need for closing tags.
Mechanical scanning probe lithography (m-SPL) is a nanomachining or nano-scratching top- down approach without the application of heat. Thermo-mechanical SPL applies heat together with a mechanical force, e.g. indenting of polymers in the Millipede memory.
The holotype was collected on April 11, 1975 from limestone talus on the north-facing wall of a canyon indenting the East side of Goat Mountain. It is deposited at the Academy of Natural Sciences of Drexel University ANSP 340724.
Mandible Cirque () is a cirque indenting the coast of Daniell Peninsula west- southwest of Cape Phillips, in Victoria Land, Antarctica. It was named in 1966 by the New Zealand Antarctic Place-Names Committee for its appearance in plan and oblique views suggestive of a mandible.
Land Bay () is an ice-filled bay, about wide, indenting the coast of Marie Byrd Land, Antarctica, just eastward of Groves Island. It was discovered by the United States Antarctic Service (1939–41), and takes its name from Land Glacier which descends into the bay.
Rum Cove () is a cove indenting the northwest coast of James Ross Island between Tumbledown Cliffs and Cape Obelisk. Named in 1983 by the United Kingdom Antarctic Place-Names Committee (UK-APC) in association with the names of other alcoholic spirits on this coast.
This also gives the advantage of the firing pin indenting the primer in a similar fashion from shot to shot as the primer cup is in direct contact with the bolt face. As with any reloading all care must be taken and manufacturer's recommendations followed.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Bourchier Cove (, ) is the 2.35 km wide cove indenting for 860 m the northwest coast of Smith Island in the South Shetland Islands, Antarctica. Entered between Jireček Point and Villagra Point.
Location of Rugged Island in the South Shetland Islands Topographic map of Livingston Island and Smith Island Hersilia Cove is the 650 m wide cove indenting for 800 m the north coast of Rugged Island in the South Shetland Islands, Antarctica west of Herring Point.
The sea, the ship and the sailor. Tales of adventure from log books and original narratives. Salem, Massachusetts: Marine Research Society, 1925 (map following p. 14)) is a wide bay indenting for the southwest coast of West Falkland in the Falkland Islands, South Atlantic.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Glozhene Cove (, ) is the 700 m wide cove indenting for 400 m the northwest coast of Smith Island, South Shetland Islands west of Cape Smith. Bulgarian early mapping in 2009.
Potter Cove is a cove indenting the south-west side of King George Island to the east of Barton Peninsula, in the South Shetland Islands of Antarctica. Potter Cove was known to sealers as early as 1821, and the name is now well established in international usage.
Suspiros Bay is a small bay indenting the west end of Joinville Island just south of Madder Cliffs. The name was proposed by Captain Emilio L. Diaz, commander of the Argentine Antarctic task force (1951–52). The toponym alludes to the difficulties encountered in surrounding the bay.
Location of Liège Island in the Antarctic Peninsula region. Palakariya Cove (, ) is a 3.2 km wide cove indenting for 2 km the northwest coast of Liège Island in the Palmer Archipelago, Antarctica. Entered south of Bebresh Point. The cove is named after Palakariya River in western Bulgaria.
Location of Hurd Peninsula in the South Shetland Islands. On the cove's beach. Topographic map of Livingston Island and Smith Island. Argentina Cove is a 1.28 km wide embayment indenting for 330 m the southeast coast of Hurd Peninsula, Livingston Island in the South Shetland Islands, Antarctica.
Gouvernøren Harbor () is a small harbor indenting the east side of Enterprise Island just west of Pythia Island in Wilhelmina Bay, off the west coast of Graham Land, Antarctica. The name was applied by whalers using the harbor because the whaling vessel Gouvernøren I was wrecked there in 1916.
Moubray Bay () is a bay in the western Ross Sea, indenting the coast of Victoria Land, Antarctica, between Cape Roget and Cape Hallett. It was discovered in 1841 by Sir James Clark Ross and named by him for George H. Moubray, clerk in charge of the expedition ship .
Gaul Cove Gaul Cove () is a cove indenting the northeast side of Horseshoe Island, off the coast of Graham Land, Antarctica. It was named by the UK Antarctic Place-Names Committee for Kenneth M. Gaul, first leader of the Falkland Islands Dependencies Survey Horseshoe Island station in 1955.
Kapellet Canyon is a canyon with steep rock and ice walls indenting the eastern side of Jøkulkyrkja Mountain, in the Mühlig-Hofmann Mountains of Queen Maud Land. It was plotted from surveys and aerial photographs by the Sixth Norwegian Antarctic Expedition (1956–60) and named Kapellet (the chapel).
The Småkovane Cirques () are two cirques, separated by a narrow ridge, indenting the northeast side of Breplogen Mountain in the Mühlig-Hofmann Mountains of Queen Maud Land. They were plotted from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Småkovane ("the small closets").
Gin Cove () is a cove in Antarctica indenting the northwest coast of James Ross Island to the north of Tumbledown Cliffs. In association with the names of other alcoholic beverages on this coast, named "Gin Cove" by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1983.
Location of Greenwich Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Berende Cove (, ) is the 3.3 km wide cove indenting for 1.15 km the southwest coast of Greenwich Island in the South Shetland Islands, Antarctica. Entered south of Pelishat Point.
Katedralen Canyon () is an ice-filled canyon with steep rock cliffs indenting the northwest side of Jøkulkyrkja Mountain, in the Mühlig-Hofmann Mountains of Queen Maud Land, Antarctica. It was plotted from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Katedralen (the cathedral).
Location of Liège Island in the Antarctic Peninsula region. Coria Cove is the 1 km wide cove indenting for 1.15 km the east coast of Liège Island in the Palmer Archipelago, Antarctica. The cove is centred at , which is 7.2 km southwest of Neyt Point. British mapping in 1978.
Akkuratnaya Cove () is a small cove east-southeast of Nadezhdy Island, indenting the north side of the Schirmacher Hills, Queen Maud Land. First photographed from the air by the Third German Antarctic Expedition, 1938-39\. Mapped by the Soviet Antarctic Expedition in 1961 and named Bukhta Akkuratnaya ("accurate cove").
Location of Trinity Peninsula. Chudomir Cove (, ) is the 4.3 km wide cove indenting for 3.4 km the southeast coast of Trinity Peninsula, Antarctic Peninsula, and entered southwest of Pitt Point and northeast of Kiten Point. The cove is named after the Bulgarian writer Chudomir (Dimitar Chorbadzhiyski, 1890–1967).
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Vedena Cove (, ) is the 1.73 km wide cove indenting for 560 m the northwest coast of Smith Island in the South Shetland Islands, Antarctica west of Delyan Point. Its head is fed by Saparevo Glacier.
Map of Thurston Island. Satellite image of Thurston Island. Potaka Inlet is a narrow ice-filled inlet about 8 nautical miles (15 km) long, indenting the north side of Thurston Island immediately east of Starr Peninsula. First delineated from air photos taken by U.S. Navy Operation Highjump in December 1946.
Location of Trinity Peninsula. Smokinya Cove (, ) is the 3.5 km wide cove on Prince Gustav Channel indenting for 2.2 km the southeast coast of Trinity Peninsula in Graham Land, Antarctica. It is entered north of Azimuth Hill. The cove is named after the seaside locality of Smokinya in Southeastern Bulgaria.
Depeaux Point forms the south end of the island. Port Circumcision is a cove indenting the southeast side of Petermann Island. It was discovered on January 1, 1909. In the Roman Catholic calendar, this date is the Feast of the Circumcision of Christ, for which Captain Charcot named the cove.
The scalloped bays indenting Lake Taupo's northern and western coasts are typical of large volcanic caldera margins. The caldera they surround was formed during the huge Oruanui eruption. New Zealand has been the site of many large explosive eruptions during the last two million years, including several of supervolcano size.Heather Catchpole.
Location of Livingston Island in the South Shetland Islands. Topographic map of Livingston Island and Smith Island. Maleshevo Cove (, ) is a 2.5 km wide cove indenting for 1.1 km the north coast of Livingston Island in the South Shetland Islands, Antarctica. It is entered between Lukovit Point and Siddins Point.
Location of Livingston Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Skravena Cove (, ) is a 2.1 km wide cove indenting for 1 km the north coast of Livingston Island in the South Shetland Islands, Antarctica. Entered between Avitohol Point and Kuklen Point.
Location of Davis Coast. Vinitsa Cove (, ‘Zaliv Vinitsa’ \'za-liv 'vi-ni- tsa\\) is the 3.75 km wide cove indenting for 1.9 km Davis Coast in Graham Land, Antarctica east of Cape Page and west of Havilland Point. The cove is named after the settlement of Vinitsa in Southern Bulgaria.
Oom Bay is a well-defined bay, 2 mi wide, indenting the Mawson coast between Cape Bruce and Campbell Head. Discovered in February 1931 by the British Australian and New Zealand Antarctic Research Expedition (BANZARE) under Douglas Mawson, who named it for Lieutenant K.E. Oom, RAN, cartographer with the expedition.
Location of Greenwich Island in the South Shetland Islands. Galápagos Cove is the small, 210 m wide cove indenting for 70 m the northeast coast of Greenwich Island in the South Shetland Islands, Antarctica and entered between Spark Point and Figueroa Point. The feature is named after the Galápagos Islands, Ecuador.
Location of Weddell Island in the Falkland Islands Satellite image of Weddell Island French Harbour is the 500 m wide bay indenting for 3.1 km the west coast of Weddell Island in the Falkland Islands.French Harbour. Falkland Islands. GeoNames Geographical Database It is entered 5.5 km north of Weddell Point, and centred at .
Location of Weddell Island in the Falkland Islands Satellite image of Weddell Island Chatham Harbour (former name States Bay, ) is the large bay indenting the central part of Weddell Island in the Falkland Islands.Chatham Harbour. Falkland Islands. GeoNames Geographical Database It is entered east of Beacon Point and west of Loop Head.
Location of Weddell Island in the Falkland Islands Satellite image of Weddell Island Quaker Harbour is the irregularly shaped bay indenting for 3.7 km the north coast of Weddell Island in the Falkland Islands.Quaker Harbour. Falkland Islands. GeoNames Geographical Database It is centred at , and has its head fed by Pitt Creek.
Høgskotet Spur ("High Bulkhead Spur") is a high rock spur on the north side of Borg Mountain. Borghallet, a gently sloping plain, lies north of the mountain. Rindebotnen Cirque ("Mountain Cirque") is a cirque indenting its northeast wall. Kvasstind Peak ("Sharp Peak") is a sub-peak on the northeast part of Borg Mountain.
Collins Harbour () is a bay indenting the south coast of King George Island immediately east of Fildes Peninsula, in the South Shetland Islands. The name appears on a chart by Scottish geologist David Ferguson, who roughly charted the bay in 1913–14, but may reflect an earlier naming. Bellingshausen Station is located here.
Location of Biscoe Islands in the Antarctic Peninsula region. Suregetes Cove (, ) is the 2.47 km wide cove indenting for 1.9 km the N coast of Krogh Island in Biscoe Islands, Antarctica. It is entered east of Kuvikal Point and west of Zagrade Point. The cove is named after the Thracian god Suregetes.
It is 920 m wide and indenting for 180 m the southeast coast of Hurd Peninsula east-northeast of Binn Peak and south-southwest of Nusha Hill. The area was visited by early 19th century sealers. The cove is descriptively named by Spain in connection with a rock glacier draining into it.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Kozloduy Cove (, ) is a 1.4 km wide cove indenting for 1.25 km the east coast of Robert Island, South Shetland Islands between Kitchen Point and Perelik Point. Bulgarian early mapping in 2009.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Nevestino Cove (, ) is the 1.55 km wide cove indenting for 1.5 km the north coast of Robert Island, South Shetland Islands between Catharina Point and Hammer Point. Bulgarian early mapping in 2009.
Corozal Bay is an inlet of Chetumal Bay, indenting northern Belize. Several resort areas are located on the coast of the bay, most notably Corozal Town. The New River (Belize) flows north into the bay. The town of Consejo is located north-northeast of the bay, on the much larger Chetumal Bay.
Location of Hurd Peninsula in the South Shetland Islands. Española Cove (in the left background) from Charrúa Ridge. Topographic map of Livingston Island and Smith Island. Española Cove is a 1.2 km wide embayment indenting for 250 m the northwest coast of Hurd Peninsula, Livingston Island in the South Shetland Islands, Antarctica.
Gerlache Inlet () is an inlet wide in the northwest corner of Terra Nova Bay, indenting the Northern Foothills just south of Mount Browning, along the coast of Victoria Land, Antarctica. The name appears to have been applied by the British National Antarctic Expedition, 1901–04, and honors Belgian Antarctic explorer Lieutenant Adrien de Gerlache.
Marian Cove () is a cove indenting the southwest part of King George Island between Collins Harbour and Potter Cove, in the South Shetland Islands, Antarctica. The name was used by Scottish geologist David Ferguson in a 1921 report based upon his investigations of King George Island in 1913–14, but may reflect an earlier naming.
Location of Stresher Peninsula on Graham Land, Antarctic Peninsula. Auvert Bay is a bay wide, indenting the coast for between Cape Evensen and Cape Bellue, along the northwest coast of Stresher Peninsula, Graham Land in Antarctica. It was discovered by the French Antarctic Expedition, 1908-10, and named "Baie Auvert" ("bay far from anywhere").
Location of Livingston Island in the South Shetland Islands. Topographic map of Livingston Island and Smith Island. Prisoe Cove (, ‘Zaliv Prisoe’ \'za-liv pri-'so-e\\) is the 3.7 km wide cove indenting for 1.75 km the north coast of Livingston Island in the South Shetland Islands, Antarctica. Entered between Agüero Point and Avitohol Point.
Location of Anvers Island in the Antarctic Peninsula region. Lapeyrère Bay () is long and wide, and lies north of Gourdon Peninsula, indenting the northeast coast of Anvers Island, in the Palmer Archipelago, Antarctica. Its head is fed by Iliad Glacier. The bay was roughly charted by the German expedition under Eduard Dallmann, 1873–74.
Location of Nelson Island in the South Shetland Islands. Varvara Cove (, ) is the 3.3 km wide cove indenting for 1.9 km the southwest coast of Nelson Island in the South Shetland Islands, Antarctica. Entered southeast of The Toe and northwest of Ross Point. The cove is named after the settlement of Varvara in southeastern Bulgaria.
Location of Nelson Island in the South Shetland Islands. Hall Cove ( \'za-liv 'hol\\) is the 2.85 km wide cove indenting for 1 km the northwest coast of Nelson Island in the South Shetland Islands, Antarctica. Entered northeast of Smilets Point and southwest of Retamales Point. The area was visited by early 19th century sealers.
Fredric W. Hillard, Type-writing machine, , granted Feb. 10, 1903. The tab mechanism came into its own as a rapid and consistent way of uniformly indenting the first line of each paragraph. Often a first tab stop at 5 or 6 characters was used for this, far larger than the indentation used when typesetting.
Location of Livingston Island in the South Shetland Islands. Brunow Bay from Catalunyan Saddle, Tangra Mountains, with Bransfield Strait and Antarctic Peninsula in the background. Topographic map of Livingston Island. Brunow Bay is a 2.33 km wide bay indenting for 1.5 km the southeast side of Livingston Island in the South Shetland Islands, Antarctica.
Location of Varna Peninsula in the South Shetland Islands. Hydra Cove is a small cove indenting for 200 m the northwest coast of Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica and entered north of Gargoyle Bastion. The feature is named after the Lernaean Hydra, a monster with nine heads slain by Hercules.
Location of Varna Peninsula in the South Shetland Islands. Topographic map of Livingston Island. Lister Cove is a 2.1 km wide cove indenting for 1.55 km the northeast coast of Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica south of Pomorie Point and north of Karavelova Point. The cove is fed by Rose Valley Glacier.
Map of Thurston Island. Satellite image of Thurston Island. Morgan Inlet is an ice-filled inlet about long, with two branches, indenting the east end of Thurston Island, Antarctica, between Lofgren Peninsula and Tierney Peninsula. The south side of the larger north arm of the inlet is an area of icy rock exposures called the King Cliffs.
Island Arena () is a broad valley occupied by a lateral lobe of the Darwin Glacier, Antarctica, indenting the north side of the Darwin Mountains between Colosseum Ridge and Kennett Ridge. An islandlike nunatak, Richardson Hill, rises above the ice of the valley. The descriptive name was given by the Victoria University of Wellington Antarctic Expedition (1962–63).
Location of Greenwich Island in the South Shetland Islands. Kramolin Cove (on the opposite coast, to the right of Yovkov Point). Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Kramolin Cove (, ) is the 1.92 km wide cove indenting for 900 m the southwest coast of Greenwich Island in the South Shetland Islands, Antarctica.
Location of Livingston Island in the South Shetland Islands. Bruix Cove (in the background) from Miziya Peak, surmounted by Delchev Peak and Ruse Peak. Topographic map of Livingston Island. Bruix Cove is the 1.93 km wide cove indenting for 1.75 km the south coast of Moon Bay in eastern Livingston Island, the South Shetland Islands in Antarctica.
Location of Weddell Island in the Falkland Islands Satellite image of Weddell Island New Year Cove is the 1.7 km wide bay indenting for 2.45 km the southeast coast of Weddell Island in the Falkland Islands.New Year Cove. Falkland Islands. GeoNames Geographical Database It is entered north of Hadassah Point and south of Circum Point and centred at .
Location of Liège Island in the Antarctic Peninsula region. Beripara Cove (, ) is the 2.45 km wide cove indenting for 1.8 km the southeast coast of Liège Island in the Palmer Archipelago, Antarctica. It is entered north of Balija Point and south of Leshko Point. The cove is named after the ancient Thracian settlement of Beripara in Northern Bulgaria.
Casey Bay is a large Antarctic bay indenting the coast of Enderby Land between Tange Promontory and Dingle Dome. The feature was observed from Australian National Antarctic Research Expeditions aircraft in 1956. It was named by the Antarctic Names Committee of Australia for the Rt. Hon. Richard G. Casey (later Lord Casey), Australian Minister for External Affairs, 1951–60.
Location of Anvers Island in the Antarctic Peninsula region. Galata Cove (, ) is the 1.93 km wide cove indenting for 2.18 km the northeast coast of Anvers Island in the Palmer Archipelago, Antarctica. It is entered south of Frolosh Point and north of Deliradev Point. The cove is named after the Galata Point on the Bulgarian Black Sea coast.
Location of Danco Coast on Graham Land, Antarctic Peninsula . Duarte Cove is the 6 km embayment indenting for 4.9 km Danco Coast between Sladun Peninsula and Relyovo Peninsula. Entered south of Cierva Point and north of Renzo Point. The feature is named after Captain José Duarte, commander of the transport ship Maipo in the 1949 Chilean Antarctic expedition.
The forewings are fuscous, lighter on the dorsal area and with a moderate whitish streak from the base along the fold throughout, somewhat suffused on the termen. The plical and second discal stigmata form small roundish spots of darker fuscous suffusion indenting lower and upper margins of this respectively. The hindwings are rather dark grey.Meyrick E. 1921b.
Location of Trinity Peninsula. Slomer Cove (, ‘Zaliv Slomer’ \'za-liv 'slo- mer\\) is the 11.2 km wide cove indenting for 5.9 km the northwest coast of Trinity Peninsula, Antarctic Peninsula south of Cape Kjellman and north of Auster Point. The cove is named after the settlement of Slomer in northern Bulgaria. This name originates from Bulgaria.
Troyan: Manfred Wörner Foundation, 2009. Letelier Bank () is lying off Ash Point, while Bascopé Point () is situated to the southwest, with the wide Rojas Cove () indenting for the coast between that point and Guesalaga Peninsula. The area was visited by early 19th century sealers. Ash Point was charted and named descriptively by the Discovery Investigations in 1935.
Location of Davis Coast. Hvoyna Cove (, ‘Zaliv Hvoyna’ \'za-liv 'hvoy-na\\) is the 1.7 km wide cove indenting for 1 km Davis Coast in Graham Land, Antarctica. It is part of Jordanoff Bay entered east of Wennersgaard Point and west of Kamenar Point. The cove is named after the settlement of Hvoyna in Southern Bulgaria.
Some of these, such as the main islands (North and South), Stewart Island, New Caledonia, and the Chatham Islands, are settled. Other smaller islands are eco-sanctuaries with carefully controlled access. The scalloped bays indenting Lake Taupo's northern and western coasts are typical of large volcanic caldera margins. The caldera they surround was formed during the huge Oruanui eruption.
LED was a programmer's editor by Norsk Data running on the ND-500 computers running Sintran III. It featured automatic indenting, pretty- printing of source code, and integration with the compiler environment. It was sold as an advanced alternative to PED. There are several remaining copies, and it is installed on the NODAF public access ND-5700.
The son of Edward Honey, and Mary Honey, née Bolton, Edward George Honey was born at Elsternwick, Victoria on 18 September 1885.Births: Honey, The Argus, (Monday, 21 September 1885), p.1. Edward Senior ran an indenting agency at 31 Queen St, Melbourne. His only brother, William Henry Honey (1879-1959) was an author and publisher (W.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Cabut Cove is the 1.08 km wide cove indenting for 1 km the northwest coast of Smith Island in the South Shetland Islands, Antarctica and entered between Markeli Point and Jireček Point. Part of its coast is formed by the terminus of Yablanitsa Glacier.
Location of Two Hummock Island in the Antarctic Peninsula region. Urania Cove (, ) is the 1.6 km wide cove indenting for 1.35 km the west coast of Two Hummock Island in the Palmer Archipelago, Antarctica north of Buache Peak and west of Modev Peak.Urania Cove. SCAR Composite Gazetteer of Antarctica The feature is named after Urania, the muse of astronomy in Greek mythology.
Location of Weddell Island in the Falkland Islands Satellite image of Weddell Island Gull Harbour (former names States Harbour, Great Harbour) is the 1.3 km wide bay indenting for 2.8 km the east coast of Weddell Island in the Falkland Islands.Gull Harbour. Falkland Islands. GeoNames Geographical Database It is entered north of Gull Point and south of Mark Point, and is centred at .
A Russian ship in Mikkelsen Harbor Mikkelsen Harbor () is a small bay indenting the south side of Trinity Island between Skottsberg Point and Borge Point, in the Palmer Archipelago, Antarctica. It provides excellent anchorage for ships, and was frequently used by sealing vessels in the first half of the nineteenth century and by Norwegian whaling vessels at the beginning of the twentieth century.
Map of Gerlache Strait region, showing Paradise Harbor. Cartographic base: Antarctic Digital Database www.add.scar.org/ Paradise Harbor, also known as Paradise Bay, is a wide embayment behind Lemaire and Bryde Islands in Antarctica, indenting the west coast of Graham Land between Duthiers and Leniz Points. The name was first applied by whalers operating in the vicinity and was in use by 1920.
From View Point looking east across Duse Bay Duse Bay () is a bay indenting the south side of Trinity Peninsula between View Point and the western side of Tabarin Peninsula. It was discovered by a party under J. Gunnar Andersson, of the Swedish Antarctic Expedition, 1901–04, and was named by Otto Nordenskiöld, the leader of that expedition, for Lieutenant S.A. Duse.
The Aurkvaevane Cirques are a set of three cirques with moraine-covered floors, indenting the west side of Kvaevefjellet Mountain in the Payer Mountains of Queen Maud Land. They were discovered and plotted from air photos by the Third German Antarctic Expedition, 1938–39, and re-plotted from air photos and from surveys, and named, by the Sixth Norwegian Antarctic Expedition, 1956–60.
Gwadar Bay Gwadar Bay Gwadar Bay () is located in the Gulf of Oman on the maritime border of Pakistan and Iran. The name is from Persian, Khalij-e Gavader or "Gulf of Gwadar" on the Arabian Sea. It is an inlet of the Arabian Sea indenting the sandy Makran coast at the Iran–Pakistan border. It is about long and wide.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Linevo Cove (, ‘Zaliv Linevo’ \'za-liv 'li-ne-vo\\) is the 900 m wide cove on Boyd Strait indenting for 560 m the southeast coast of Smith Island in the South Shetland Islands, Antarctica, and entered northeast of Kubadin Point. Its head is fed by Ritya Glacier.
1:250,000 scale topographic map of the Yule Bay area. Yule Bay is a bay indenting the coast of northern Victoria Land between Cape Hooker and Cape Dayman. An inner (western) portion of the bay is circumscribed by Bates Point and Ackroyd Point. Discovered by Captain James Clark Ross, 1841, who named it for Henry B. Yule, Second Master on .
Location of Snow Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Barutin Cove (, ‘Zaliv Barutin’ \'za-liv 'ba-ru-tin\\) is the 2.05 km wide cove indenting for 1.03 km the southwest coast of Snow Island in the South Shetland Islands, Antarctica. It is entered north of Monroe Point and south of Vokil Point.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Pakusha Cove (, ‘Zaliv Pakusha’ \'za-liv pa-'ku-sha\\) is the 970 m wide cove on Boyd Strait indenting for 450 m the southeast coast of Smith Island in the South Shetland Islands, Antarctica, and entered northeast of Varbak Point. Its head is fed by Nosei Glacier.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Brashlyan Cove (, ‘Zaliv Brashlyan’ \'za-liv bra-'shlyan\\) is the 1.3 km wide cove on Osmar Strait indenting for 480 m the southeast coast of Smith Island in the South Shetland Islands, Antarctica, and entered northeast of Dupnitsa Point. Its head is fed by Gramada Glacier.
Location of Two Hummock Island in the Antarctic Peninsula region. Lesura Cove (, ‘Zaliv Lesura’ \'za-liv le-'su-ra\\) is the 1.97 km wide cove indenting for 1.2 km the south coast of Two Hummock Island in the Palmer Archipelago, Antarctica. It is entered west of Veyka Point. The point is named after the settlement of Lesura in Northwestern Bulgaria.
Location of Liège Island in the Antarctic Peninsula region. Vapa Cove (, ) is the 1.65 km wide cove indenting for 1.1 km the west coast of Liège Island in the Palmer Archipelago, Antarctica. It is entered north of Polezhan Point and south of Disilitsa Point, and has its head fed by Pleystor Glacier. The cove is named after Vapa Peak in Rila Mountain, Bulgaria.
Kvarsnes Bay is a small bay at the southwest side of Kvarsnes Foreland, and is named in association with it. Rund Bay ("Round Bay") is a small bay indenting the south shore of Edward VIII Bay immediately east of Kvarsnes Foreland. These features were mapped and named by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition, 1936–37.
Location of Rugged Island in the South Shetland Islands. Topographic map of Livingston Island and Smith Island. Bogomil Cove (, ) is a 970 m wide cove indenting for 770 m the west coast of Rugged Island off the west coast of Byers Peninsula of Livingston Island in the South Shetland Islands, Antarctica. It is entered north of Kokalyane Point and south of Ugain Point.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Vrabcha Cove (, ) is the 900 m wide cove indenting for 1 km the west coast of Heywood Island off the northwest coast of Robert Island in the South Shetland Islands, Antarctica. The cove is named after the settlement of Vrabcha in western Bulgaria.
Holme Bay is a bay in Antarctica in Mac. Robertson Land, wide, containing many islands, indenting the coast north of the Framnes Mountains. Holme Bay is largely snow-free and was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition in January-February 1937, and named Holmevika because of its island-studded character (holme means "islet" in Norwegian) .
Location of Low Island in the South Shetland Islands. Malina Cove (, ) is the 1.65 km wide cove indenting for 1.25 km the west coast of Low Island in the South Shetland Islands, Antarctica. It is entered south of Jameson Point and north of Ugorelets Point. The cove is named after the settlements of Gorna (Upper) Malina and Dolna (Lower) Malina in western Bulgaria.
Location of Livingston Island in the South Shetland Islands. Vasilev Bay from Miziya Peak, with Saedinenie Snowfield in the foreground and Siddins Point in the background. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Vasilev Bay is the 9.6 km wide embayment indenting for 3.8 km the north coast of Livingston Island in the South Shetland Islands, Antarctica.
Buying agents or purchasing agents are people or companies that offer to buy goods or property on behalf of another party. Indent agents or indenting agents (or firms) are alternative terms for buying agents. An indent is an order for goods under specified conditions of sale. There are agents for all kinds of products, from raw material commodities through to specialized custom equipment.
Location of Varna Peninsula on Livingston Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Dragon Cove is a 550 m wide cove indenting for 600 m the northeast coast of Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica entered between Sigritsa Point and Ficheto Point. Surmounted by Sayer Nunatak on the southwest.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Hisarya Cove (, ) is the 950 m wide cove on the northwest side of Osmar Strait indenting for 500 m the southeast coast of Smith Island in the South Shetland Islands, Antarctica south of Dupnitsa Point and 7.6 km northeast of Cape James. Its head is fed by Letnitsa Glacier.
Mansa Cove is the cove indenting for the east coast of the small () ice-free promontory forming the north extremity of Ioannes Paulus II Peninsula, western Livingston Island in the South Shetland Islands, Antarctica and ending up in Cape Shirreff. The feature was descriptively named by the 1984-85 Chilean Antarctic Expedition from the stillness of its waters (‘Quiet Bay’ in Spanish).
Location of Hurd Peninsula in the South Shetland Islands. Topographic map of Livingston Island and Smith Island. Las Palmas Cove is a 1.97 km wide embayment indenting for 500 m the northwest coast of Hurd Peninsula on Livingston Island in the South Shetland Islands, Antarctica. It is part of South Bay, Livingston Island entered between Henry Bluff and Salisbury Bluff.
Moraine Canyon () is a canyon with very steep rock walls, long, indenting northern Nilsen Plateau just west of Fram Mesa, in the Queen Maud Mountains of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was so named by the Advisory Committee on Antarctic Names because the canyon floor is completely covered by glacial moraine.
Location of Anvers Island in the Antarctic Peninsula region. Fournier Bay () is a bay long and wide, indenting the northeast coast of Anvers Island immediately west of Briggs Peninsula and south of Dralfa Point, in the Palmer Archipelago, Antarctica. Its head is fed by Rhesus, Thamyris, Kleptuza and Altimir Glaciers. The bay was probably first seen by a German expedition, 1873–74, under Eduard Dallmann.
Location of Kiev Peninsula in Graham Land, Antarctic Peninsula. Girard Bay () is a bay long and wide, indenting the northwest coast of Kiev Peninsula, Graham Land, between Cape Cloos and Mount Scott. It was discovered by the Belgian Antarctic Expedition, 1897–99, and was named by the French Antarctic Expedition, 1903–05, under Jean-Baptiste Charcot, for Jules Girard of the Paris Société de Géographie.
Drew Cove () is a cove indenting the west side of Mitchell Peninsula on the Budd Coast. It was first mapped from air photos taken by U.S. Navy Operation Highjump and Operation Windmill in 1947 and 1948, and was named by the Advisory Committee on Antarctic Names for Chief Construction Electrician John W. Drew, U.S. Navy, a member of the Wilkes Station party of 1958.
Location of Desolation Island in the South Shetland Islands. Desolation Island). Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Kozma Cove (Zaliv Kozma \'za-liv koz-'ma\\) is a 1.8 km wide cove indenting for 1.2 km the north coast of Desolation Island between the two arms of that V-shaped island situated in the entrance to Hero Bay, Livingston Island, Antarctica.
Malmgren Bay () is a bay indenting the west side of Renaud Island immediately north of Speerschneider Point, in the Biscoe Islands of Antarctica. It was first accurately shown on an Argentine government chart of 1957. The bay was named by the UK Antarctic Place-Names Committee in 1959 for Finn A.E.J. Malmgren, the Swedish author in 1927 of an important study on the properties of sea ice.
Maury Bay () is an ice-filled bay indenting the coast of Antarctica just east of Cape Lewis. It was mapped by G.D. Blodgett in 1955 from aerial photographs taken by U.S. Navy Operation Highjump (1946–47), and named by the Advisory Committee on Antarctic Names for William Lewis Maury, lieutenant on the brig during the United States Exploring Expedition (1838–42) under Lieutenant Charles Wilkes.
Location of Nordenskjöld Coast on Antarctic Peninsula. Desislava Cove (, ‘Zaliv Desislava’ \'za-liv de-si-'sla-va\\) is the 3.3 km wide cove indenting for 3 km Nordenskjöld Coast in Graham Land west of Cape Worsley. It was formed as a result of the retreat of Aleksiev Glacier and Kladorub Glacier in the early 21st century. The feature is named after the Bulgarian sebastokratorissa Desislava (13th century).
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Kruni Cove (, ‘Zaliv Kruni’ \'za-liv 'kru-ni\\) is the 900 m wide cove indenting for 1.15 km the east coast of Robert Island in the South Shetland Islands, Antarctica. It is entered south of Kitchen Point and north of Galiche Rock off Somovit Point.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Tsepina Cove (, ‘Zaliv Tsepina’ \'za-liv 'tse-pi-na\\) is the 1 km wide cove indenting for 850 m the east coast of Robert Island in the South Shetland Islands, Antarctica. It is entered south of Galiche Rock off Somovit Point, and north of Batuliya Point.
Location of Nelson Island in the South Shetland Islands. Bononia Cove (, ‘Zaliv Bononia’ \'za-liv bo'no-ni-ya\\) is the 3.1 km wide cove indenting for 1.1 km the southeast coast of Nelson Island in the South Shetland Islands, Antarctica. It is entered west of Ivan Alexander Point. The cove's shape is enhanced as a result of glacier retreat in the late 20th and early 21st century.
Ambush Bay () is a bay 3.5 nautical miles (6 km) wide indenting the north coast of Joinville Island immediately east of King Point. Ofelia Island lies in the southwest part of the bay. The feature was surveyed by the Falkland Islands Dependencies Survey (FIDS) in 1953. The name arose because the bay is a trap for the unwary if its shallow and foul nature is not known.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Nikolov Cove (, ‘Nikolov Zaliv’ i-'ko-lov 'za-liv\\) is the 950 m wide cove on Boyd Strait indenting for 500 m the southeast coast of Smith Island in the South Shetland Islands, Antarctica, and entered northeast of Velikan Point and southwest of Razdel Point. Its head is fed by Ovech Glacier.
Location of Trinity Peninsula. Retizhe Cove (, ‘Zaliv Retizhe’ \'za-liv re- ti-'zhe\\) is the 5.8 km wide cove indenting for 6.2 km on the south coast of Trinity Peninsula in Graham Land, Antarctica. Part of Duse Bay, entered between Boil Point to the west and Garvan Point to the east. The cove is named after the Retizhe River in Pirin Mountain, Southwestern Bulgaria.
Location (in red) of Anvers Island in the Antarctic Peninsula region Goten Peninsula (, ) is the mostly ice-covered peninsula wide and indenting for northwestwards between Perrier Bay and Esquivel (Ricke) Bay on the northwest coast of Anvers Island in the Palmer Archipelago, Antarctica. It ends up in Quinton Point to the northwest. The peninsula is named after Goten Peak in western Balkan Mountains, Bulgaria.
Location of Brabant Island in the Antarctic Peninsula region. Kayak Bay () is a bay, wide, on the inner (west) side of Pampa Passage, indenting the east coast of Brabant Island in the Palmer Archipelago in Antarctica north of Momino Point and south of Bov Point. Malpighi Glacier and Mackenzie Glacier flow into the bay. The feature was roughly mapped in 1898 by the Belgian Antarctic Expedition.
Location of Biscoe Islands in the Antarctic Peninsula region. Transmarisca Bay (, ‘Zaliv Transmarisca’ \'za-liv trans-ma-'ri-ska\\) is the 4.3 km wide bay indenting for 3.2 km the north coast of Krogh Island in Biscoe Islands, Antarctica. It is entered east of Edholm Point and west of Kuvikal Point. The bay is named after the ancient Roman town of Transmarisca in Northeastern Bulgaria.
Location of Rugged Island in the South Shetland Islands. Topographic map of Livingston Island. Nishava Cove (, ) is a 1.33 km wide cove indenting for 1 km the north coast of Rugged Island off the west coast of Byers Peninsula of Livingston Island in the South Shetland Islands, Antarctica. It is entered between Chiprovtsi Islets and Chiprovtsi Point on the east, and Cape Sheffield on the west.
Location of Low Island in the South Shetland Islands. Kazichene Cove (, ) is a 2.2 km wide cove on the southeast side of Osmar Strait indenting for 1.3 km the northwest coast of Low Island in the South Shetland Islands, Antarctica. It is esouth of Lyutibrod Rocks and Fernandez Point, and north of Solnik Point. The cove is named after the settlement of Kazichene in western Bulgaria.
Location of Byers Peninsula on Livingston Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Belene Cove (, ) is the 520 m wide cove indenting for 690 m the northwest coast of Ray Promontory, part of Svishtov Cove in Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica. The cove is entered between Isbul Point and Start Point.
Location of Byers Peninsula on Livingston Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Baba Tonka Cove (, ) is the 1.1 km wide cove indenting for 750 m the north coast of Byers Peninsula between Villard Point and Varadero Point on Livingston Island in the South Shetland Islands, Antarctica. The area was visited by early 19th century sealers.
Location of Pefaur (Ventimiglia) Peninsula on Danco Coast, Antarctic Peninsula. Latinka Cove (, ‘Zaliv Latinka’ \'za-liv la-'tin-ka\\) is the 1.95 km wide cove indenting for 1.65 km the northwest coast of Pefaur (Ventimiglia) Peninsula, Danco Coast on the Antarctic Peninsula. It is entered east of Eckener Point and west of Binkos Point. The head of the cove is fed by Poduene Glacier.
Location of Barison Peninsula on Graham Coast, Antarctic Peninsula. Macrobius Cove (, ‘Zaliv Macrobius’ \'za-liv ma-'kro-biy\\) is the 2.8 km wide cove indenting for 3.4 km the west coast of Barison Peninsula, Graham Coast on the Antarctic Peninsula northeast of Eijkman Point and east of Bablon Island. It is part of Leroux Bay. The head of the cove is fed by Chernomen Glacier.
Location of Magnier Peninsula on Graham Coast, Antarctic Peninsula. Finaeus Cove (, ‘Zaliv Finaeus’ \'za-liv fi-'ney\\) is the 3.8 km wide cove indenting for 2.8 km the northeast coast of Magnier Peninsula, Graham Coast on the Antarctic Peninsula. It is part of Leroux Bay, entered southeast of Vartop Point and northwest of Krasava Point. The head of the cove is fed by Muldava Glacier.
Different techniques are used to quantify material characteristics at smaller scales. Measuring mechanical properties for materials, for instance, of thin films, cannot be done using conventional uniaxial tensile testing. As a result, techniques testing material "hardness" by indenting a material with a very small impression have been developed to attempt to estimate these properties. Hardness measurements quantify the resistance of a material to plastic deformation.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Devesil Bight (, ) is the 5.8 km wide embayment indenting for 2.2 km the southeast coast of Robert Island in the South Shetland Islands, Antarctica between Kermen Peninsula and the 2.7 km peninsula ending up in Robert Point. Entered between Edwards Point and Robert Point.
The TTK Group was founded in 1928 as an indenting agency by T.T. Krishnamachari. The current executive chairman of TTK Prestige T.T.Jagannathan along with Sandhya Mendonca has co- authored a book titled "Disrupt and Conquer - How TTK Prestige Became a Billion-Dollar Company". The book is a journey about the company’s many milestones and how it had fought bankruptcy to become a successful company.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Micalvi Cove is a 1.9 km wide cove indenting for 1.35 km the southwest coast of Robert Island in the South Shetland Islands, Antarctica next northwest of Kermen Peninsula, and entered between Edwards Point and Zahari Point. Avren Rocks are situated in the interior of the cove.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Mitchell Cove is the 2.8 km wide bay indenting for 3 km the southwest coast of Robert Island in the South Shetland Islands, Antarctica southeast of Alfatar Peninsula, and entered between Debelyanov Point and Negra Point. The area was visited by early 19th century sealers.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Ivan Asen Cove (, ‘Zaliv Ivan Asen’ \'za-liv i-'van a-'sen\\) is the 1.16 km wide cove on Osmar Strait indenting for 800 m the southeast coast of Smith Island in the South Shetland Islands, Antarctica, and entered northeast of Ivan Asen Point. Its head is fed by Dragoman Glacier.
The Gulf of Mexico is the largest body of water indenting the continent, followed by Hudson Bay. Others include the Gulf of Saint Lawrence and the Gulf of California. Before the Central American isthmus formed, the region had been underwater. The islands of the West Indies delineate a submerged former land bridge, which had connected North and South America via what are now Florida and Venezuela.
Bartlett Inlet () is a largely ice-filled inlet, about wide, indenting the north coast of Edward VII Peninsula just east of Cape Colbeck. It was mapped from surveys by the United States Geological Survey and from U.S. Navy air photos (1959–65), and named by the Advisory Committee on Antarctic Names for Lieutenant Eugene F. Bartlett, MC, U.S. Navy, officer in charge at Byrd Station, 1960.
Location of Nordenskjöld Coast. Odrin Cove (, ) is the 10 km wide bay indenting for 7 km Nordenskjöld Coast in Graham Land, Antarctica, and entered southwest of Fothergill Point and northeast of Spoluka Point. Its head is fed by Zaychar Glacier, Sinion Glacier, Akaga Glacier and the glacier featuring Arrol Icefall. The bay is named after the settlements of Odrintsi in Northeastern and Southern Bulgaria.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Yundola Cove (, ) is a 1.34 km wide cove indenting for 670 m the north coast of Robert Island in the South Shetland Islands, Antarctica west of Lavrenov Point. The feature is named after Yundola Saddle between Rila Mountain and the Rhodope Mountains in southern Bulgaria.
Location of Greenwich Island in the South Shetland Islands. Hardy Cove (on the right) from Bransfield Strait. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Hardy Cove is the 950 m wide cove indenting for 1.37 km the east coast of Greenwich Island in the South Shetland Islands, Antarctica and surmounted by Parchevich Ridge to the north and Ilarion Ridge to the south.
Location of Desolation Island in the South Shetland Islands. Desolation Island with Cora Cove in the centre from Vidin Heights, Livingston Island. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Cora Cove is the 750 m wide cove in the northwest part of Blythe Bay indenting for 590 m the southeast coast of Desolation Island off Livingston Island in the South Shetland Islands, Antarctica.
Location of Greenwich Island in the South Shetland Islands. Jambelí Cove is the 620 m wide cove indenting for 140 m the north coast of Greenwich Island in the South Shetland Islands, Antarctica and entered between Spark Point and Orión Point. The area was visited by 19th century sealers operating from nearby Clothier Harbour. The feature is named after the Jambelí Archipelago in Ecuador.
Location of Biscoe Islands in the Antarctic Peninsula region Clio Bay (, ) is the 1.8 km wide bay indenting for 1.7 km the west coast of Lavoisier Island in Biscoe Islands, Antarctica. It is formed as a result of the retreat of Lavoisier Island's ice cap in the early 21st century.Clio Bay. SCAR Composite Gazetteer of Antarctica The feature is named after Clio, the muse of history in Greek mythology.
Hamilton Bay () is a small bay at the mouth of Salomon Glacier, indenting the southeast coast of South Georgia northeast of the mouth of Drygalski Fjord. It was surveyed by the South Georgia Survey in the period 1951–57, and named by the UK Antarctic Place-Names Committee for James E. Hamilton (1893–1957), Colonial Naturalist to the Falkland Islands, who was seconded for service with the Discovery Investigations, 1925–28.
Instead of using a shearing action as with scissors, diagonal pliers cut by indenting and wedging the wire apart. The jaw edges are ground to a symmetrical "V" shape, thus the two jaws can be visualized to form the letter "X", as seen end-on when fully occluded. The pliers are made of tempered steel, and inductive heating and quenching are often used to selectively harden the jaws.
Location of Anvers Island in the Antarctic Peninsula region. Perrier Bay () is a bay 6 nautical miles (11 km) wide indenting the northwest coast of Anvers Island in the Palmer Archipelago, Antarctica between Obitel Peninsula and Goten Peninsula. It is entered north of Giard Point and south of Quinton Point. Masteyra Island is lying in the north part of the bay, and Trebishte Island and Vromos Island in its south part.
Haydn Inlet () is an ice-filled inlet indenting the west coast of Alexander Island, Antarctica, lying between Mozart Ice Piedmont and Handel Ice Piedmont. Schubert Inlet lies to the south and the Lassus Mountains are immediately north. Haydn Inlet is long and wide at the mouth, narrowing toward the head. It was first seen from the air and roughly mapped by the United States Antarctic Service, 1939–41.
Mascías Cove () is a cove indenting the west coast of Graham Land, Antarctica, immediately east of Mount Banck. It was first roughly charted by the Belgian Antarctic Expedition under Gerlache, 1897–99, and later, by the Scottish geologist David Ferguson, 1913–14. It was named for Lieutenant Eladio Mascías of the tug Chiriguano which made a survey of the area during the Argentine Antarctic Expedition of 1949–50.
Location of Churchill Peninsula in Graham Land, Antarctic Peninsula. Brentopara Inlet (, ‘Zaliv Brentopara’ \'za-liv bren-to-'pa-ra\\) is the 7 km wide inlet indenting for 6.2 km the east coast of Churchill Peninsula, Oscar II Coast in Graham Land. It is part of Adie Inlet entered southeast of Cavarus Point and northwest of Astro Cliffs. The feature is named after the ancient Thracian town of Brentopara in Southern Bulgaria.
Location of Churchill Peninsula in Graham Land, Antarctic Peninsula. Zimen Inlet (, ‘Zimenski Zaliv’ \'zi-men-ski 'za-liv\\) is the 12.8 km wide inlet indenting for 9.3 km the east coast of Churchill Peninsula, Oscar II Coast in Graham Land. It is part of Adie Inlet entered south of Slav Point and north of Cavarus Point. The feature is named after the settlement of Zimen in Southeastern Bulgaria.
Location of Nordenskjöld Coast. Pizos Bay (, ‘Zaliv Pizos’ \'za-liv 'pi-zos\\) is the 10.65 km wide bay indenting for 9 km Nordenskjöld Coast in Graham Land, Antarctica northwest of Samotino Point and southeast of Porphyry Bluff. Part of Larsen Inlet, formed as a result of glacier retreat in the last decade of 20th century. The feature is named after the ancient settlement of Pizos in southern Bulgaria.
In contrast to the cultivated west coast of the island, the eastern half is a mixture of freshwater lochs, moorland, bog and deeply indenting sea lochs. Craigstrome is near Ruabhal, Benbecula's highest hill at . The township of Lionacleit houses the island's main secondary school, which also doubles as a community centre, with a swimming pool, cafeteria, sports facilities, a small museum and a library."Sgoil Lionacleit" Comhairle nan Eilean Siar.
Location of Livingston Island in the South Shetland Islands. Topographic map of Livingston Island and Smith Island Zornitsa Cove (, ‘Zaliv Zornitsa’ \'za- liv zor-'ni-tsa\\) is the 7 km wide cove indenting for 3.1 km the north coast of Livingston Island in the South Shetland Islands, Antarctica. Entered between Rowe Point and Scesa Point on the west side of Ioannes Paulus II Peninsula. Bulgarian mapping in 2009.
Several skerries buffer the southern coast of the island. The coastline of Innaarsuit Island is developed, with several small inlets indenting the shore in the east, west, and northwest. The Innaarsuit settlement is located near the mouth of one of the inlets, in the northwestern part of the island. The island is nearly split in half in the center, with only a narrow isthmus joining the southern and northern halves.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Yarebitsa Cove (, ‘Zaliv Yarebitsa’ \'za-liv ya-'re-bi-tsa\\) is the 900 m wide cove on Osmar Strait indenting for 570 m the southeast coast of Smith Island in the South Shetland Islands, Antarctica, and entered northeast of Skalina Point and southwest of Ivan Asen Point. Its head is fed by Armira Glacier.
Location of Brabant Island in the Antarctic Peninsula region. Apiaria Bight (, ‘Zaliv Apiaria’ \'za-liv a-pi-'a-ri-ya\\) is the 5.7 km wide embayment indenting for 1.7 km the northwest coast of Pasteur Peninsula on Brabant Island in the Palmer Archipelago, Antarctica. It is entered northeast of Metchnikoff Point and southwest of Cape Roux, and has Soatris Island lying near the southwest side of its entrance.
Location of Anvers Island in the Antarctic Peninsula region. Obitel Peninsula (, ) is the mostly ice-covered peninsula wide 6.9 km and indenting for 6.6 km northwestwards between Hamburg Bay and Perrier Bay on the northwest coast of Anvers Island in the Palmer Archipelago, Antarctica. It ends up in Bonnier Point to the west and Giard Point to the north. The peninsula is named after the settlement of Obitel in Northeastern Bulgaria.
Location of Biscoe Islands in the Antarctic Peninsula region. Misionis Bay (, ‘Zaliv Misionis’ \'za-liv mi-si-'o-nis\\) is the 1.6 km wide bay indenting for 2.35 km the northeast coast of Pickwick Island in the Pitt group of Biscoe Islands, Antarctica. It is entered east of Kusev Point and west of Plakuder Point. The bay is named after the ancient and medieval town of Misionis in Northeastern Bulgaria.
The descriptive name was applied by FIDS personnel who surveyed the headland in 1948. Whistling Bay is an open bay, 4 nautical miles (7 km) wide and indenting 2.5 nautical miles (4.6 km) between Longridge Head and Cape Saenz. It was first roughly surveyed in 1936 by BGLE personnel, then resurveyed in 1948 by FIDS, who named it for an unidentified whistling sound heard there at the time of the survey.
Location of Loubet Coast on the Antarctic Peninsula. Tlachene Cove (, ‘Zaliv Tlachene’ \'za-liv 'tla-che-ne\\) is the 4 km wide cove indenting for 3.6 km Loubet Coast on the Antarctic Peninsula. It is part of Darbel Bay, entered southwest of Kudelin Point and northeast of Gostilya Point. The cove was formed as a result of the retreat of Hopkins Glacier during the last two decades of the 20th century.
Location of Stresher Peninsula on Graham Land, Antarctic Peninsula. Crates Bay (, ‘Zaliv Krates’ \'za-liv 'kra-tes\\) is the 8 km wide bay indenting for 6 km the northeast coast of Stresher Peninsula, Graham Coast on the Antarctic Peninsula. It is part of Holtedahl Bay, entered southeast of Starmen Point and northwest of the headland formed by Lens Peak. Conway Island lies in the central part of the bay.
Location of Greenwich Island in the South Shetland Islands. Gruev Cove from Bransfield Strait, with Parchevich Ridge on the left and Bogdan Ridge on the right. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Gruev Cove (, ) is the 300 m wide cove indenting for 650 m the east coast of Greenwich Island, in the South Shetland Islands south of Santa Cruz Point and north of Parchevich Ridge.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Clothier Harbour is the 1.5 km wide bay indenting for 1 km the north coast of Robert Island in the South Shetland Islands, Antarctica between Hammer Point on the northeast and Onogur Islands on the southwest. The harbour was used as a safe base by American sealing ships in 1820–21.
Beall Island is an Antarctic rocky island, long, with small coves indenting the east and west sides, lying northwest of Mitchell Peninsula in the Windmill Islands. It was first mapped from air photos taken by USN Operation Highjump and Operation Windmill in 1947 and 1948. It was named by the US-ACAN for James M. Beall, U.S. Weather Bureau observer with Operation Windmill who assisted staff aerology officers with forecasting duties.
Location of Hurd Peninsula on Livingston Island in the South Shetland Islands. Topographic map of Livingston Island and Smith Island. Buena Nueva Cove is a small open cove, 900 m wide and indenting for 200 m the northwest coast of False Bay, Livingston Island in the South Shetland Islands, Antarctica southeast of MacGregor Peaks and east of Castro Peak on Hurd Peninsula. The area was visited by early 19th century sealers.
Farmers department store within Westfield Newmarket A company founded by Robert Laidlaw in 1909 as "Laidlaw Leeds" sold agricultural related goods through mail order catalogues, following a successful American model. It was bought by Farmers Union members in 1910. For example the Clevedon branch approved formation of a farmers union indenting and trading association at its 1910 meeting. In 1916 it was renamed as the Farmers Union Trading Co (Auckland) Ltd.
Snow Island in the South Shetland Islands Livingston, Greenwich, Robert, Snow and Smith Islands Brauro Cove (, ‘Ivaylov Zaliv’ \i-'vay-lov 'za-liv\\) is the 1.93 km wide cove indenting for 620 m the northwest coast of Snow Island in the South Shetland Islands, Antarctica. It is entered southwest of Mezdra Point and northeast of Irnik Point.Brauro Cove. SCAR Composite Gazetteer of Antarctica The feature is named after the Thracian goddess Brauro.
Location of Nelson Island in the South Shetland Islands. Edgell Bay () is a bay long and wide, indenting the northeast side of Nelson Island, in the South Shetland Islands. This bay appears in rough outline on Powell's chart of the South Shetland Islands published in 1822. It was recharted during 1934–35 by Discovery Investigations personnel on the Discovery II, who named it for Vice Admiral Sir John Augustine Edgell, Royal Navy.
Location of Pernik Peninsula on Loubet Coast, Antarctic Peninsula. Chepra Cove (, ‘Zaliv Chepra’ \'za-liv che-'pra\\) is the 1.7 km wide cove indenting for 2.3 km the west coast of Pernik Peninsula on Loubet Coast in Graham Land, Antarctica. It is a part of Lallemand Fjord entered south of Holdfast Point, and has its head fed by Koriten Glacier. The cove is named after the cave of Chepra in Southeastern Bulgaria.
Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Iquique Cove is a small, wide cove indenting for the east coast of Discovery Bay, Greenwich Island in the South Shetland Islands, Antarctica. Iquique Cove is sheltered on the northwest by Guesalaga Peninsula, and the small González Island () is situated on the south side of the cove's entrance. The cove is used by ships servicing the Chilean Antarctic base Arturo Prat.
Location of Nelson Island in the South Shetland Islands. Tuida Cove (, ‘Zaliv Tuida’ \'za-liv tu-'i-da\\) is the 4.13 km wide cove indenting for 1.56 km the southeast coast of Nelson Island in the South Shetland Islands, Antarctica. It is entered east of Ivan Alexander Point and west of Slavotin Point. The cove's shape is enhanced as a result of glacier retreat in the late 20th and early 21st century.
Location of Smith Island in the South Shetland Islands. Topographic map of Smith Island. Zapalnya Cove (, ‘Zaliv Zapalnya’ \'za-liv za-'pal-nya\\) is the 1.37 km wide cove on Boyd Strait indenting for 550 m the southeast coast of Smith Island in the South Shetland Islands, Antarctica, and entered northeast of Razdel Point and southwest of Medovene Point. The cove is named after the historical settlement of Zapalnya in Southern Bulgaria.
This technique requires placing an ultrasound probe on the central cornea. While this is a convenient way to determine the axial length for most normal eyes, errors in measurement almost invariably result from the probe indenting the cornea and shallowing the anterior chamber. Since the compression error is variable, it cannot be compensated for by a constant. IOL power calculations using these measurements will lead to an overestimation of the IOL power.
Location of Liège Island in the Antarctic Peninsula region. Boisguehenneuc Bay (, ‘Zaliv Boisguehenneuc’ \'za-liv bo-a-ge-e-'nyok\\) is the 6.9 km wide bay indenting for 2.4 km the northwest coast of Liège Island in the Palmer Archipelago, Antarctica. It is entered northeast of Bebresh Point and southwest of the west extremity of Kran Peninsula, with its head fed by Shterna Glacier. Raklitsa Island is lying in the central part of the bay.
Location of Anvers Island in the Antarctic Peninsula region. Gerritsz Bay (, ‘Zaliv Gerritsz’ \'za-liv 'ge-rits\\) is the 4 km wide bay indenting for 2.15 km the north coast of Anvers Island in the Palmer Archipelago, Antarctica. It is entered east of Oberbauer Point and west of the northwest extremity of the small peninsula forming Cape Grönland. The point is so named in order to preserve the historical memory of the area.
Location of Anvers Island in the Antarctic Peninsula region. Dalchev Cove (, ‘Dalchev Zaliv’ \'dal-chev 'za-liv\\) is the 3.72 km wide cove indenting for 2.45 km the northwest coast of Parker Peninsula on the northeast coast Anvers Island in the Palmer Archipelago, Antarctica. It is the part of Fournier Bay entered east of Studena Point, having its head fed by Altimir Glacier. The cove is named after the Bulgarian sculptor Lyubomir Dalchev (1902-2002).
Location of Snow Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Ivaylo Cove (, ‘Ivaylov Zaliv’ \i-'vay-lov 'za-liv\\) is the 500 m wide cove indenting for 900 m the east coast of Snow Island in the South Shetland Islands, Antarctica. Bounded by the small Hall Peninsula on the west and southwest, Ogygia Island on the south and Cacho Island on the northeast.
Location of Low Island in the South Shetland Islands. Smochevo Cove (, ‘Zaliv Smochevo’ \'za-liv 'smo-che-vo\\) is the 1.6 km wide cove on the southeast side of Osmar Strait indenting for 850 m the northwest coast of Low Island in the South Shetland Islands, Antarctica. Entered south of Cape Wallace, Zebil Island and Glumche Island, and north of Fernandez Point. The cove is named after the settlement of Smochevo in Western Bulgaria.
Location of Clarence Island in the South Shetland Islands. Clarence Island seen from north-northeast with l(left to right) Lebed Point, Istros Bay, Sugarloaf Island and Cape Lloyd. Istros Bay (, ) is the 3.2 km wide bay indenting for 1.4 km the east coast of Clarence Island in the South Shetland Islands, Antarctica. It is entered north of Lebed Point and south of Sugarloaf Island, and has its head fed by Highton Glacier.
Location of Trinity Peninsula. Ognen Cove (, ‘Zaliv Ognen’ \'za-liv 'og-nen\\) is the 2.8 km wide cove indenting for 1.55 km the northwest coast of Trinity Peninsula in Graham Land, Antarctica. It is part of Charcot Bay entered west of Nikyup Point, and formed as a result of the retreat of Andrew Glacier in the second half of 20th century. The cove is named after the settlement of Ognen in Southeastern Bulgaria.
108 Additionally, legal trouble arose regarding the patents of Chichester Bell and Charles Sumner Tainter,Welch p. 107 in that Edison's original patent was for recording via indenting the surface, while the Bell-Tainter patents allowed for incising the recording surface.Welch p. 23 A negotiation for Gouraud's resignation brought the desired results, and as they were in America, the Edison and Bell-Tainter interests were merged into a new company in Britain.
Location of Robert Island in the South Shetland Islands. Carlota Cove (on the left) from English Strait, with Fort William in the foreground. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Carlota Cove is the 1.9 km wide cove indenting for 1.14 km the northwest coast of Alfatar Peninsula, Robert Island in the South Shetland Islands, Antarctica next east of Coppermine Peninsula, and entered between Fort William and Misnomer Point.
Location of Greenwich Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Guayaquil Bay is the 2.59 km wide bay indenting for 1.25 km the north coast of Greenwich Island in the South Shetland Islands, Antarctica and entered between Agüedo Point and Orión Point. The bay is used by ships servicing the Ecuadorian Antarctic base Pedro Vicente Maldonado situated 560 m south-southwest of Orión Point.
Nelson Island in the South Shetland Islands Quesada Cove (, ) is the 2.5 km wide cove indenting for 1 km the north coast of Nelson Island in the South Shetland Islands, Antarctica west of Cariz Point and east of Meana Point. It is formed as a result of the retreat of Nelson Island's ice cap in the last decade of 20th century.Quesada Cove. SCAR Composite Gazetteer of Antarctica The area was visited by early 19th century sealers.
Map of Thurston Island. Satellite image of Thurston Island. Glacier Bight is an open embayment about wide, indenting the north coast of Thurston Island between Hughes Peninsula and Noville Peninsula. It was first delineated from air photos taken by U.S. Navy Operation Highjump in December 1946, and was named by the Advisory Committee on Antarctic Names for the icebreaker USS Glacier, the first ship ever to make its way to this coastal area, in February 1960.
Location of Anvers Island in the Antarctic Peninsula region. Hamburg Bay () is a bay indenting the northwest coast of Anvers Island in the Palmer Archipelago, Antarctica immediately south of Bonnier Point, Obitel Peninsula. Emen Island and Petrelik Island are located in the southwest part of the bay. The bay was discovered but incompletely defined by a German expedition in 1873–74 under the command of Eduard Dallmann, who named it for Hamburg, Germany, the home port of the expedition.
Kirwan Inlet () is an inlet in the southeast corner of Alexander Island, wide at its mouth and indenting , opening on George VI Sound. The inlet is ice filled and merges almost imperceptibly with the rising ice slopes of Alexander Island to the west. It was roughly mapped in 1949 by the Falkland Islands Dependencies Survey, and named by the UK Antarctic Place-Names Committee for Laurence P. Kirwan, Director and Secretary of the Royal Geographical Society.
Location of Ioannes Paulus II Peninsula on Livingston Island in the South Shetland Islands. Stoyanov Cove and Ioannes Paulus II Peninsula in the background, from Catalunyan Saddle; Burdick Ridge in the foreground. Topographic map of Livingston Island and Smith Island Stoyanov Cove (, ) is the 2.6 km wide cove indenting for 1.1 km the north coast of Livingston Island in the South Shetland Islands, Antarctica. Entered between Sandanski Point and Agüero Point on Ioannes Paulus II Peninsula.
Stefansson Bay is a bay indenting the coast for between Law Promontory and Fold Island. Mawson of the British Australian New Zealand Antarctic Research Expedition (BANZARE) applied the name to a sweep of the coast west of Cape Wilkins which he observed on about February 18, 1931. Exploration by DI personnel on the William Scoresby, 1936, and the Lars Christensen expedition 1936–37, defined this section of the coast more accurately. It was named for Vilhjalmur Stefansson, Arctic explorer.
Location of Liège Island in the Antarctic Peninsula region. Bolbabria Cove (, ‘Zaliv Bolbabria’ \'za-liv bol-'ba-bri-ya\\) is the 2 km wide cove indenting for 1.85 km the west coast of Liège Island in the Palmer Archipelago, Antarctica. It is entered north of Disilitsa Point and south of the westerly offshoot of Beaumont Hill, and has its head fed by Zbelsurd Glacier. The cove is named after the ancient Thracian settlement of Bolbabria in Western Bulgaria.
Legru Bay () is a bay wide, indenting the south coast of King George Island, South Shetland Islands, Antarctica, immediately northeast of Martins Head. The French Antarctic Expedition, 1908–10, under Jean-Baptiste Charcot applied the name "Cap Legru" to a feature which has now been identified as Martins Head. As the latter has priority, Charcot's name has been transferred to this bay in order to retain the name in the area in which it was originally given.
Location of Graham Coast on the Antarctic Peninsula. Bigo Bay () is a bay long and wide, indenting the west coast of Graham Land between Cape Garcia and Magnier Peninsula surmounted by the Magnier Peaks and Lisiya Ridge. The French Antarctic Expedition, 1908–10, first sighted this bay but charted it as the southern part of Leroux Bay. The British Graham Land Expedition, 1934–37, determined that the peninsula surmounted by the Magnier Peaks separates this bay from Leroux Bay.
Location of Low Island in the South Shetland Islands. Teshel Cove (, ‘Zaliv Teshel’ \'za-liv 'tr-shel\\) is the 1.4 km wide cove indenting for 1.6 km the west coast of Low Island in the South Shetland Islands, Antarctica. Situated north of Malina Cove and south by west of Kazichene Cove, 8.3 km north of Cape Garry and 6.7 km south by west of Cape Wallace. The cove is named after the settlement of Teshel in southern Bulgaria.
Location of Astrolabe Island in the Antarctic Peninsula region. Astrolabe Island with Mokren Bight on the right. Mokren Bight (, ‘Zaliv Mokren’ \'za-liv 'mo-kren\\) is a 2 km wide embayment indenting for 850 m the west coast of Astrolabe Island in Bransfield Strait off Trinity Peninsula, Antarctica. Entered northwest of Gega Point and southeast of the small peninsula featuring Petleshkov Hill, projecting westwards and ending in Damga Point to the south and Raduil Point to the north.
Location of Byers Peninsula on Livingston Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Raskuporis Cove (, ) is the 1.77 km wide cove indenting for 700 m the south coast of Byers Peninsula on Livingston Island in the South Shetland Islands, Antarctica. Entered west of Sevar Point and east of Devils Point, and connected to Osogovo Bay to the northwest by the 20 m wide passage of Hell Gates.
Location of Byers Peninsula on Livingston Island in the South Shetland Islands. Topographic map of Livingston Island Kukuzel Cove (, ) is the 1.18 km wide cove indenting for 620 m the north coast of Byers Peninsula between Lair Point and Villard Point on Livingston Island in the South Shetland Islands, Antarctica. The area was visited by early 19th century sealers. The cove is “named after the famous Bulgarian church music composer and singer St. Yoan Kukuzel (1280–1360).”Kukuzel Cove.
TTK Services Pvt Ltd, is an Indian business conglomerate with a presence across the world, In different segments of industry including virtual assistant services and Real estate services, headquartered in Bangalore, Karnataka. TTK Services Pvt Ltd is a company of the TTK Group; The TTK Group was founded in 1928 as an indenting agency by Mr. T.T. Krishnamachari. The Group also has other subsidiaries like TTK Healthcare Limited, TTK Protective Devices Limited, Cigna TTK Limited and Prestige Smart Kitchen.
The displaced material forms ridges adjacent to grooves, which may be removed by subsequent passage of abrasive particles. Cutting occurs when material is separated from the surface in the form of primary debris, or microchips, with little or no material displaced to the sides of the grooves. This mechanism closely resembles conventional machining. Fragmentation occurs when material is separated from a surface by a cutting process and the indenting abrasive causes localized fracture of the wear material.
Location of Clarence Island in the South Shetland Islands. Clarence Island seen from northeast with (left to right) Cape Bowles, Istros Bay, Sugarloaf Island, Smith Cove, Kakrina Point, Kutela Cove and Cape Lloyd. Smith Cove (, ) is the 1.17 km wide cove indenting for 1.33 km the east coast of Clarence Island in the South Shetland Islands, Antarctica. It is entered north of Ilyo Point and south of Kakrina Point, and has its head fed by Banari Glacier.
Location of Clarence Island in the South Shetland Islands. Clarence Island seen from northeast with (left to right) Cape Bowles, Istros Bay, Sugarloaf Island, Smith Cove, Kakrina Point, Kutela Cove and Cape Lloyd surmounted by Jubilee Peak. Kutela Cove (, ‘Zaliv Kutela’ \'za-liv ku-'te-la\\) is the 330 m wide cove indenting for 750 m the east coast of Clarence Island in the South Shetland Islands, Antarctica. It is entered just south of Cape Lloyd.
Peterson Island is an Antarctic rocky island, long, with two inlets indenting the north side, lying immediately west of Browning Peninsula in the south part of the Windmill Islands. It was first mapped from air photos taken by USN Operation Highjump and Operation Windmill in 1947 and 1948. It was named by the US-ACAN for Lt. Mendel L. Peterson, USN, supply officer with Operation Windmill which established astronomical control stations in the area in January 1948.
Armour Inlet () is an ice-filled inlet indenting the north side of Siple Island just west of the Armour Peninsula, along the coast of Marie Byrd Land. The inlet was first roughly delineated from air photos taken by U.S. Navy Operation Highjump in January 1947, and named by the Advisory Committee on Antarctic Names for the Armour Institute of Technology, Chicago, which donated funds to the United States Antarctic Service, 1939–41, for purchase of the Snow Cruiser.
Location of Nordenskjöld Coast. Mundraga Bay (, ) is the 28.6 km wide bay indenting for 23 km Nordenskjöld Coast in Graham Land, Antarctica. It is entered east of Fothergill Point and west of Cape Sobral. Local coastline is modified as a result of the Larsen A Ice Shelf disintegration and the subsequent retreat of the inflowing Darvari Glacier, Boryana Glacier, Desudava Glacier, Dinsmoor Glacier, Bombardier Glacier and Edgeworth Glacier in the 1990s and the early 21st century.
Harald Bay is a bay about wide indenting the coast between Archer Point and Williamson Head in Oates Land, Antarctica. It contains Kartografov Island. The bay was photographed from the air by U.S. Navy Operation Highjump in 1947. It was sketched and photographed by Phillip Law, leader of the Australian National Antarctic Research Expeditions (Magga Dan) on February 20, 1959, and was named by the Antarctic Names Committee of Australia for Captain Harald Moller Pederson, master of the Magga Dan during the expedition.
Map of Thurston Island. Satellite image of Thurston Island. Henry Inlet is a narrow, ice-filled inlet about long, indenting the north coast of Thurston Island, Antarctica, immediately east of Hughes Peninsula. The inlet was first plotted from air photos taken by U.S. Navy Operation Highjump, 1946–47, and was named by the Advisory Committee on Antarctic Names for Robert Henry, a photographer's mate with the U.S. Navy Bellingshausen Sea Expedition, who in February 1960 recorded features along Eights Coast from helicopters.
It used copper foil as the recording medium, with various styli, corresponding to various instruments or aircraft controls, indenting the foil. The foil was periodically advanced at set time intervals, giving a history of the aircraft’s instrument readings and control settings. The unit was developed at Farnborough for the Ministry of Aircraft Production. At the war's end the Ministry got Harrison and Husband to sign over their invention to it and the Ministry patented it under British patent 19330/45.
McCarthy Inlet () is an ice-filled inlet which is the largest and northernmost of three inlets indenting the eastern side of Berkner Island, Antarctica. It was discovered by U.S. ground and flying personnel at Ellsworth Station (1957–58) under Captain Finn Ronne of the U.S. Navy Reserve (USNR), and was named by the Advisory Committee on Antarctic Names for Lieutenant Commander Charles J. McCarthy, USNR, commander of the U.S. Navy Squadron VX-6 aircraft unit at Ellsworth Station during this period.
Schott Inlet () is a small ice-filled inlet indenting the east side of Merz Peninsula close south of Cape Darlington, along the east coast of Palmer Land. Discovered and photographed from the air in December 1940 by the United States Antarctic Service (USAS). Charted in 1947 by a joint party consisting of members of the Ronne Antarctic Research Expedition (RARE) under Ronne and the Falkland Islands Dependencies Survey (FIDS). Named by the FIDS for Gerhard Schott, internationally known German oceanographer.
Location of Oscar II Coast on Antarctic Peninsula. Artanes Bay (, ‘Zaliv Artanes’ \'za-liv 'ar-ta-nes\\) is the 14 km wide cove indenting for 6.2 km Oscar II Coast in Graham Land, Antarctica, and entered west of Cape Fairweather and east of Shiver Point. It was formed as a result of the break- up of Larsen Ice Shelf in the area in 2002, and subsequent retreat of Rogosh Glacier. The feature is named after the ancient settlement of Artanes in northwestern Bulgaria.
The outer waterways of Tasiusaq Bay separate the island from small skerries and Kangaarsuk Island in the south, from Illunguit Island in the southwest, and from Paagussat Island in the west.Upernavik, Saga Map, Tage Schjøtt, 1992 Tasiusaq Island is mountainous in its center. Tunullersuaq is the highest mountain, at . The Tasiusaq village is located in the lower part of the island, at the shores of one of the small bays indenting the coastline in the northwest, near Nuunnguaq, the western cape.
Location of Brabant Island in the Antarctic Peninsula region. Buragara Cove (, ‘Zaliv Buragara’ \'za-liv bu-ra-'ga-ra\\) is the 2.08 km wide cove indenting for 1.4 km the west coast of Brabant Island in the Palmer Archipelago, Antarctica. It is part of Dallmann Bay, entered northeast of Zabel Point and southwest of Devene Point. The feature was formed near the start of the 21st century as a result of the retreat of Rush Glacier, which feeds its head.
Spilhaus Inlet () is an ice-filled inlet which is the southernmost of the three inlets indenting the east side of Berkner Island, Filchner Ice Shelf. Discovered by U.S. ground and aviation personnel from Ellsworth Station (1957–58) under Captain Finn Ronne, USNR. Named by Advisory Committee on Antarctic Names (US-ACAN) in 1988 after Athelstan Spilhaus (b. 1911), meteorologist and oceanographer; member of the U.S. National Committee for the IGY, 1957–58, and of the National Science Board, 1966–72.
Location of Two Hummock Island in the Antarctic Peninsula region. Kotev Cove (, ‘Kotev Zaliv’ \'ko-tev 'za-liv\\) is the 1.81 km wide cove indenting for 1.8 km the northeast coast of Two Hummock Island in the Palmer Archipelago, Antarctica. It is entered northwest of Butrointsi Point. The cove is named after Vasil Kotev, commander motor boats and sledges at St. Kliment Ohridski base in 2007/08 and subsequent seasons, and base commander during parts of the 2009/10 and 2011/12 seasons.
Indenting of the sleeper was the problem; where the traffic was heavy, it became necessary to provide a sole plate under the rails to spread the load on the tie, partly vitiating the cost saving. However, in main line situations, this form found almost universal adoption in North America and Australia, and in much of continental Europe. The United Kingdom persisted with bullhead rail in main line use, with widespread introduction of flat-bottom rail only starting in about 1947.
Killermet Cove () is the southernmost of two coves indenting the west side of Bryde Island, off the west coast of Graham Land, Antarctica. The cove appears on an Argentine government chart of 1950. It was so named by the UK Antarctic Place-Names Committee in 1960 because three members of the Falkland Islands Dependencies Survey were chased into this cove in their dinghies by six killer whales while circumnavigating Bryde Island in May 1957. The three members' names were Evans, Hobbs and O'Neill.
Lützow-Holm Bay is a large bay, about wide, indenting the coast of Queen Maud Land in Antarctica between Riiser-Larsen Peninsula and the coastal angle immediately east of the Flatvaer Islands. It was discovered by Captain Hjalmar Riiser-Larsen in two airplane flights from his expedition vessel, the Norvegia, on February 21 and 23, 1931. The name honours Commander Finn Lützow- Holm of the Royal Norwegian Navy Air Service, a pilot for Captain Riiser- Larsen on the Aagaard in 1935.
Several features in and around Lützow-Holm Bay have been charted and named by various expeditions and survey groups, particularly a number of smaller bays indenting its shores. Unless otherwise specified, the following features were mapped and given Norwegian language names by Norwegian cartographers from air photos taken by the Lars Christensen Expedition (LCE) of 1936–37. Many other features were given Japanese language names by personnel from Japanese Antarctic Research Expedition headquarters, following the JARE expeditions of 1957–62.
Location of Oscar II Coast on Antarctic Peninsula. Borima Bay (, ) is the 6.5 km wide cove indenting for 8 km Oscar II Coast in Graham Land, Antarctica south of Diralo Point and north of Caution Point. It is part of Exasperation Inlet, Weddell Sea formed as a result of the disintegration of Larsen Ice Shelf in the area in 2002 and the subsequent retreat of Jorum Glacier and Minzuhar Glacier. The feature is named after the settlement of Borima in northern Bulgaria.
Location of Alexander Island in the Antarctic Peninsula region Satellite image of Alexander Island Kolokita Cove (, ‘Zaliv Kolokita’ \'za-liv ko-lo-'ki-ta\\) is the 2.7 km wide embayment indenting for 1.55 km the northwest coast of Alexander Island in Antarctica. It is entered east of the coastal point formed by Hopkins Ridge and west of Piyanets Ridge, and has its head fed by Coulter Glacier. The feature is named after Kolokita Point on the Bulgarian Black Sea Coast.
Location of Alexander Island in the Antarctic Peninsula region Satellite image of Alexander Island Farmakida Cove (, ‘Zaliv Farmakida’ \'za-liv far-ma-'ki- da\\) is the 7 km wide cove indenting for 3.3 km the northeast coast of Alexander Island in Antarctica. It is entered south of Nicholas Point, and has its head fed by Roberts Ice Piedmont. It is surmounted by Mount Calais on the southwest. The feature is named after the ancient Thracian fortress of Farmakida in Southeastern Bulgaria.
Location of Graham Coast on the Antarctic Peninsula. Nevsha Cove (, ‘Zaliv Nevsha’ \'za-liv 'nev-sha\\) is the 2.5 km wide cove indenting for 3 km Graham Coast on the Antarctic Peninsula north of Plas Point. It is part of the south arm of Beascochea Bay. The head of the cove is fed by Funk Glacier, and its shape was enhanced as a result of that glacier's retreat during the last decade of 20th century and the first decade of 21st century.
Location of Felipe Solo (Obligado) Peninsula in Graham Land, Antarctic Peninsula. Urovene Cove (, ‘Zaliv Urovene’ \'za-liv u-ro-'ve-ne\\) is the 2.65 km wide cove indenting for 2.75 km the southwest coast of Felipe Solo (Obligado) Peninsula, Graham Coast on the Antarctic Peninsula. It is part of Barilari Bay, entered southeast of Laskar Point and northwest of Duyvis Point. The cove was formed as a result of glacier retreat during the last three decades of the 20th century.
Location of Wilkins Coast on Antarctic Peninsula. Delisle Inlet (, ‘Zaliv Delisle’ \'za-liv dyo-'lil\\) is the 8.4 km wide ice-filled inlet indenting for 12.7 km the southeast side of Kenyon Peninsula, Wilkins Coast on the Antarctic Peninsula. It is entered southwest of Cape Keeler and northeast of Cape Mayo. The feature is named after the French cartographer Guillaume Delisle (also spelled Guillaume de L'Isle; 1675–1726) whose 1700 map of South America featured the Antarctic island of Roché (South Georgia).
Location of Wilkins Coast on Antarctic Peninsula. Bertius Inlet (, ‘Zaliv Bertius’ \'za-liv 'ber-tiy\\) is the 8.3 km wide ice-filled inlet indenting for 9 km Wilkins Coast on the Antarctic Peninsula. It is entered south of Cape Walcott and north of Cape Hinks, and has its head fed by Lurabee Glacier. The feature is named after the Flemish geographer and cartographer Petrus Bertius (Pieter de Bert, 1565–1629) who published an early separate map of Terra Australis Incognita in 1616.
The conferment issued in 1765 of the market right contributed as the most important renewal for Wadern. The then created marketplace and the established market fountain are even today visible signs of this market right. With indenting French revolutionary troops the feudalism was dissolved and the possession went over to French state possession, thus also castle Dagstuhl which baron Wilhelm Albert de Lasalle took over from Luisenthal in 1807. Castle Münchweiler was bought back in 1801 by his former owner again.
Sutures are placed by mounting a needle with attached suture into a needle holder. The needle point is pressed into the flesh, advanced along the trajectory of the needle's curve until it emerges, and pulled through. The trailing thread is then tied into a knot, usually a square knot or surgeon's knot. Ideally, sutures bring together the wound edges, without causing indenting or blanching of the skin, since the blood supply may be impeded and thus increase infection and scarring.
Location of Varna Peninsula in the South Shetland Islands. Griffin Cove (third left) from Miziya Peak, with Williams Point and Zed Islands in the background. Griffin Cove is the 800 m wide cove indenting for 260 m the northwest coast of Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica and entered between Gargoyle Bastion to the northeast and Organpipe Point to the southwest. The feature is named after the griffin, a legendary bird often portrayed as a monster.
For instance, the standard included a line-continuation character, but chose the ampersand, , which was also used for string concatenation. Using these in a single line could lead to very confusing code. By this time, the release of the first microcomputer systems in 1975 had quickly led to the introduction of Altair BASIC, the first version of what would soon be known as Microsoft BASIC. MS BASIC was patterned on BASIC-PLUS, and thus ultimately the Fifth Edition, but lacked indenting, MAT, and other features.
Location of Nordenskjöld Coast on Antarctic Peninsula. Solari Bay (, ‘Zaliv Solari’ \'za-liv so-'la-ri\\) is the 11.2 km wide bay indenting for 4.5 km Nordenskjöld Coast in Graham Land north of Balvan Point and south of the east extremity of Richard Knoll. It was formed as a result of the break-up of Larsen Ice Shelf in the area in the late 20th century, and subsequent retreat of Drygalski Glacier. The feature is named after the settlement of Solari in Northern Bulgaria.
Location of Oscar II Coast on Antarctic Peninsula. Domlyan Bay (, ‘Zaliv Domlyan’ \'za-liv 'dom-lyan\\) is the 4.75 km wide bay indenting for 5.5 km Oscar II Coast in Graham Land south of Radovene Point and north of Kalina Point. It is part of Exasperation Inlet, formed as a result of the break-up of Larsen Ice Shelf in the area, and the retreat of Melville Glacier in the early 21st century. The feature is named after the settlement of Domlyan in Southern Bulgaria.
Location of Oscar II Coast on Antarctic Peninsula. Durostorum Bay (, ‘Zaliv Durostorum’ \'za-liv du-ro-'sto-rum\\) is the 6.7 km wide bay indenting for 3.9 km Oscar II Coast in Graham Land southeast of Sandilh Point and northwest of Ranyari Point. It is part of Exasperation Inlet, formed as a result of the break-up of Larsen Ice Shelf in the area and the retreat of Pequod Glacier in the early 21st century. Named after the ancient town of Durostorum in Northeastern Bulgaria.
The wingspan is 30–36 mm. The forewings have a broad silvery white costal streak from one-eight to the apex, broadest at one-fourth from the base, there angled and gradually narrowing to a point at the apex. There is a broad brownish suffusion beneath the costal streak towards the base and a transversely oval, black-edged, brownish spot at two- thirds, indenting the costal streak. Some whitish suffusion is found before the tornus and there is a blackish dentate subterminal line, edged posteriorly with brownish.
Location of Rugged Island in the South Shetland Islands. Topographic map of Livingston Island and Smith Island Smyadovo Cove (, ) is a 900-meter wide cove indenting for 850 m the west coast of Rugged Island off the west coast of Byers Peninsula of Livingston Island in the South Shetland Islands, Antarctica. Entered north of Ugain Point and south of the southwest extremity of the small peninsula forming Cape Sheffield. Part of the cove's interior and entrance is occupied by Toledo Island and Prosechen Island.
Icebreaker research vessel using the Bay of Whales ice harbor Bay of Whales The Bay of Whales was a natural ice harbor, or iceport, indenting the front of Ross Ice Shelf just north of Roosevelt Island, Antarctica. It is the southernmost point of open ocean not only of the Ross Sea, but worldwide. The Ross Sea extends much further south—as far as the Gould Coast, some from the South Pole—but most of that area is covered by the Ross Ice Shelf rather than open sea.
Location of Davis Coast on the Antarctic Peninsula. Jordanoff Bay (, ) is the 5 km wide bay indenting for 4.9 km Davis Coast in Graham Land on the Antarctic Peninsula, and entered northeast of Wennersgaard Point and southwest of Tarakchiev Point. Its head is fed by Sabine Glacier. The bay is named for the Bulgarian-American pioneer of aviation Assen Jordanoff (1896–1967) who built the first Bulgarian engine-powered airplane in 1915 and took part in the construction of B-17 Flying Fortress and other US planes.
Location of Elephant Island in the South Shetland Islands Gurkovska Cove (, ‘Zaliv Gurkovska’ \'za-liv 'gur-kov-ska\\) is the 3 km wide cove indenting for 2.5 km the east extremity of Elephant Island in the South Shetland Islands, Antarctica. It is entered southwest of Cape Valentine and northeast of Walker Point. Its southwest side is occupied by Slavyanka Beach. The feature was formed as a result of the retreat of The Stadium (a glacier feeding the cove's head) in the first decade of 21st century.
A quarterly philatelic magazine, Philapost, was launched in 2008. The Department of Post has also developed software for philatelic inventory management, known as "Philsim". It is used for all activities relating to philately, including forecasting, indenting, invoicing, monitoring supply and demand and recording sales and revenue for commemorative stamps and other philatelic products at philately bureaus and counters (and definitive stamps and stationery at circle stamp depots and head post offices). The National Philatelic Museum of India was inaugurated on 6 July 1968 in New Delhi.
Hindwing with a black triangular basal patch, central area tawny red often inclining to yellow at inner margin, somewhat indenting the basal patch at upperside of cell. Hind margin with a black border about 2 mm wide, its inner edge deeply indented by the red colour in 4 and 5, above this point somewhat convex, and below running horizontally across to inner margin. Underside very like that of bonasia alicia Forewing. Basal half pale reddish yellow with dusky indications of the basal black of upperside.
Location of Varna Peninsula in the South Shetland Islands. Charybdis Cove (second left) from Miziya Peak, with Zavala Island to the left and Zed Islands in the background. Charybdis Cove is the 1.2 km wide cove indenting for 580 m the northwest coast of Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica and entered between Organpipe Point to the north and Slab Point to the south. The feature is named after the Charybdis, a mythical Greek sea monster which wrecked ships and devoured sailors.
Location of Greenwich Island in the South Shetland Islands Wulfila Glacier (in the background) from Livingston Island in 2004 Livingston, Greenwich, Robert, Snow and Smith Islands Doris Cove (, ) is the 1.3 km wide cove indenting for 600 m the southwest coast of Greenwich Island in the South Shetland Islands, Antarctica south of Oborishte Ridge and northwest of Ephraim Bluff. It is formed as a result of the retreat of Wulfila Glacier in the first two decades of 21st century.Doris Cove. SCAR Composite Gazetteer of Antarctica The area was visited by early 19th century sealers.
Dublitskiy Bay () is a bay 12 nautical miles (22 km) wide indenting the ice shelf fringing the coast of Queen Maud Land. The bay lies 70 nautical miles (130 km) north of the Sigurd Knolls, and is separated from Kamenev Bight by Cape Krasinskiy. The feature was photographed from the air by the Sixth Norwegian Antarctic Expedition in 1958–59 and mapped from these photos. It was also mapped in 1961 by the Soviet Antarctic Expedition and named for K.A. Dublitskiy, former captain of the icebreaker Fyodor Litke.
Heidemann Bay () is a bay, long, indenting the seaward end of Breidnes Peninsula in the Vestfold Hills of Antarctica, just south of Davis Station. It was mapped by Norwegian cartographers from air photos taken by the Lars Christensen Expedition, 1936–37. The bay was first visited by an Australian National Antarctic Research Expeditions party from the Kista Dan on January 11, 1957, and was named for Frank Heidemann, second mate of the Kista Dan. Heidemann Bay which was gouged by glaciers is flanked by two small peninsulas which rise approximately 20 metres above sea level.
Mikkelsen Bay is a bay, wide at its mouth and indenting , entered between Bertrand Ice Piedmont and Cape Berteaux along the west coast of Graham Land, Antarctica. First seen from a distance in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot, but not recognized as a large bay. First surveyed in 1936 by the BGLE under Rymill, and resurveyed by the Falkland Islands Dependencies Survey in 1948–49. The name was proposed by members of BGLE for Ejnar Mikkelsen, Danish Arctic explorer and Inspector for East Greenland, 1934–50.
Location of Danco Coast on the Antarctic Peninsula. Charlotte Bay is a bay on the west coast of the Antarctic Peninsula indenting the west coast of Graham Land in a southeast direction for , between Reclus Peninsula and Cape Murray. Its head is fed by the glaciers Nobile, Bozhinov, Krebs, Wellman and Renard. The bay was discovered by Adrien de Gerlache during the 1897–99 Belgian Antarctic Expedition and named after Charlotte Dumeiz, the fiancée of Georges Lecointe, Gerlache's executive officer, hydrographer and second-in-command of the expedition.
The following year, the Volunteer Force was abolished and replaced with the Territorial Force. Malone was placed in command of a new Territorial unit, the 11th Regiment (Taranaki Rifles). It was during this time that he introduced the use of the "lemon squeezer" hat to the Territorial Force. By having his troops push out its crown and indenting its sides, the hat mirrored the outline of Mount Taranaki, thereby providing a link for the regiment to its parent region, and, more practically, allowed rain to easily run off the hat.
Location of Oscar II Coast on Antarctic Peninsula. Sexaginta Prista Bay (, ‘Zaliv Sexaginta Prista’ \'za-liv sek-sa-'gin-ta 'pris-ta\\) is the 6.5 km wide bay indenting for 4 km Oscar II Coast in Graham Land southwest of Delusion Point and northeast of Radovene Point. It is part of Exasperation Inlet, formed as a result of the break-up of Larsen Ice Shelf in the area and the retreat of Mapple Glacier in the early 21st century. The feature is named after the ancient Roman town of Sexaginta Prista in Northeastern Bulgaria.
Location of Blagoevgrad Peninsula in Graham Land, Antarctic Peninsula. Yamforina Cove (, ‘Zaliv Yamforina’ \'za-liv yam-fo-'ri-na\\) is the 4.55 km wide cove indenting for 3.1 km the east coast of Blagoevgrad Peninsula on Oscar II Coast in Graham Land, Antarctica. It is entered south of Daskot Point and north of Kesten Point, and was formed as a result of the break-up of Larsen Ice Shelf in the area in 2002, and subsequent deglaciation. The feature is named after the ancient Thracian settlement of Yamforina in southwestern Bulgaria.
Penguin Composition Rules were the guidelines written by typographer Jan Tschichold for use in composing the pages and typography of Penguin Books. The rules were embodied in a four-page booklet of typographic instructions for editors and compositors. The booklet includes headings for various aspects of composition: Text Composition; Indenting of Paragraphs; Punctuation Marks and Spelling; Capitals, Small Capitals, and Italics; References and Footnotes; Folios; The Printing of Plays; The Printing of Poetry; Make-up. Beyond this specific set of guidelines, Tschichold made further changes to Penguin's graphic standards.
Beascochea Bay Beascochea Bay () is a bay, long and wide, indenting the Graham Coast of Graham Land, Antarctica, between Kiev Peninsula and Barison Peninsula, and entered south of Cape Perez. The glaciers Lever, Funk, Cadman, Talev and Butamya feed the bay. It was discovered but incompletely defined by the Belgian Antarctic Expedition, 1897–99; was resighted by the French Antarctic Expedition, 1903–05, and named by Jean-Baptiste Charcot for Commander Beascochea, Argentine Navy. The bay was then more accurately charted by the British Graham Land Expedition, 1934–37.
Map of Admiralty Bay Admiralty Bay () is an irregular bay, wide at its entrance between Demay Point and Martins Head, indenting the southern coast of King George Island for , in the South Shetland Islands of Antarctica. The name appears on a map of 1822 by Captain George Powell, a British sailor, and is now established in international usage. The Henryk Arctowski Polish Antarctic Station is situated on the bay, as is the Comandante Ferraz Brazilian Antarctic Base. It has been designated an Antarctic Specially Managed Area (ASMA 1).
Location of Danco Coast. Hughes Bay is a bay lying between Cape Sterneck and Cape Murray along the west coast of the Antarctic Peninsula. It is wide and lies south of Chavdar Peninsula and north of Pefaur (Ventimiglia) Peninsula, indenting the Danco Coast on the west side of Graham Land for . The name has appeared on maps for over 100 years, and commemorates Edward Hughes, master of the Sprightly, a sealing vessel owned by the London whaling company Samuel Enderby & Sons, which explored in this area in 1824–25.
Location of Velingrad Peninsula on Graham Coast, Antarctic Peninsula. Dimitrov Cove (, ) is the 6.8 km wide cove indenting for 4.8 km the northwest coast of Velingrad Peninsula on Graham Coast in Graham Land, Antarctica, which is entered between Pripek Point to the west and Biser Point to the east. Hoek Glacier and Rusalka Glacier flow into the cove, their termini separated by Veshka Point, while Camacúa Island is lying at the cove's entrance. The cove is named after the Bulgarian historian Bozhidar Dimitrov for his support for the Bulgarian Antarctic programme.
Nanoindentation improves on these macro- and micro-indentation tests by indenting on the nanoscale with a very precise tip shape, high spatial resolutions to place the indents, and by providing real-time load-displacement (into the surface) data while the indentation is in progress. Figure 1. Schematic of load-displacement curve for an instrumented nanoindentation test In nanoindentation small loads and tip sizes are used, so the indentation area may only be a few square micrometres or even nanometres. This presents problems in determining the hardness, as the contact area is not easily found.
Atomic force microscopy or scanning electron microscopy techniques may be utilized to image the indentation, but can be quite cumbersome. Instead, an indenter with a geometry known to high precision (usually a Berkovich tip, which has a three-sided pyramid geometry) is employed. During the course of the instrumented indentation process, a record of the depth of penetration is made, and then the area of the indent is determined using the known geometry of the indentation tip. While indenting, various parameters such as load and depth of penetration can be measured.
Location of Hurd Peninsula in the South Shetland Islands Johnsons Dock from Charrúa Ridge George Powell's 1822 chart of the South Shetland Islands and South Orkney Islands featuring Johnsons Dock Topographic map of Livingston Island and Smith Island Johnsons Dock is a sheltered 500 m wide cove indenting for 900 m the northwest coast of Hurd Peninsula on Livingston Island in the South Shetland Islands, Antarctica. It is part of South Bay entered north of Ballester Point. Surmounted by Charrúa Ridge on the northeast. The cove was frequented by early 19th century sealers.
II (New York:MacMillan 1903) Without air shafts, the 1867 requirement failed to increase natural light or fresh air ventilation in the crowded tenement "dark bedroom".Riis, Jacob A. How the Other Half Lives: Studies among the tenements of New York (New York:Scribners, 1890) Responding to the new requirements, a magazine, Plumbing and Sanitation Engineer, held a tenement design contest in 1879. James Ware's winning dumbbell design represented a compromise between legal health standards and commercial viability. By indenting the sides of the structure three feet, he opened a slender airshaft between abutting buildings.
Not only this, the state also has the distinction of possessing three mass nesting beaches of endangered olive ridley sea turtles which makes it the largest nesting ground of the species. The state has three mass nesting beaches of endangered olive ridley sea turtles which when combined together makes it the world's largest nesting ground for this species. Indenting Orissa's ocean coast is Chilika lagoon, a semi-saline wetland used by many species of migratory birds, and also which the endangered Irrawaddy dolphin uses as part of its range. In spite of considerable human interactivity here, the rare dolphin survives.
Håhellerskarvet, meaning "shark cave mountain" in Norwegian, is a high partially ice-covered mountain between Austreskorve Glacier and Lunde Glacier in the Mühlig-Hofmann Mountains of Queen Maud Land, East Antarctica. Other nearby geographic features include Håhelleren Cove, indenting the north side of Håhellerskarvet, Håhelleregga Ridge, an irregular rock ridge just north of Håhellerskarvet, Håhellerbotnen Cirque, a large cirque on the east side of Håhelleregga Ridge, and Jøkulkyrkja, a broad, ice-topped mountain located east of Lunde Glacier. All of these geographic features were plotted from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60).
Porpoise Bay is an ice-filled embayment about wide indenting the coast of Antarctica between Cape Goodenough and Cape Morse. The United States Exploring Expedition (1838–42) under Charles Wilkes applied the name "Porpoise Bay", after the USEE brig "Porpoise", to a large bay at about 66°S, 130°E. US-ACAN's identification of Porpoise Bay is based on the correlation of Wilkes' chart (1840) with G.D. Blodgett's reconnaissance map (1955) compiled from air photos taken by USN Operation Highjump (1946–47). The name has been applied to the large embayment lying close southwest in keeping with Wilkes' original naming.
Location of Rozhen Peninsula on Livingston Island in the South Shetland Islands. Gela Point with Chavei Cove on the right, from Bransfield Strait Topographic map of Livingston Island and Smith Island Chavei Cove (, ‘Zaliv Chavei’ \'za-liv cha-'ve-i\\) is the 2.2 km wide cove indenting for 900 m the southeast coast of Rozhen Peninsula on Livingston Island in the South Shetland Islands, Antarctica entered east of Gela Point. It is formed as a result of the retreat of Prespa Glacier in the early 21st century. The feature is named after the settlement of Chavei in northern Bulgaria.
The Arduino integrated development environment (IDE) is a cross-platform application (for Windows, macOS, and Linux) that is written in the programming language Java. It originated from the IDE for the languages Processing and Wiring. It includes a code editor with features such as text cutting and pasting, searching and replacing text, automatic indenting, brace matching, and syntax highlighting, and provides simple one-click mechanisms to compile and upload programs to an Arduino board. It also contains a message area, a text console, a toolbar with buttons for common functions and a hierarchy of operation menus.
Allegro Valley () is a steep-sided, glacier-filled valley indenting the east side of Daniels Range just north of White Spur, in the Usarp Mountains, Antarctica. The northern party of the New Zealand Geological Survey Antarctic Expedition, 1963-64, experienced fine weather here after several days of unpleasant travel; therefore, the expedition members named it after John Milton's poem L'Allegro in antithesis to Penseroso Bluff, to the north. The valley is situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. Its south wall is known as the White Spur.
Aside from its unique answer judging mechanisms, TUTOR's original set of control structures was rather sparse. In the mid 1970s, this shortcoming was addressed by introducing `if`, `endif` blocks with optional `elseif` and `else` sections. The semantics of these control structures was routine, but the syntax inherited the mandatory indentation of the Tutor Language, presaging that of Python and adding a unique nonblank indent character to distinguish indenting from continuation lines. This is illustrated in the following example, from page S5 of the Summary of TUTOR Commands and System Variables (10th ed) by Elaine Avner, 1981: if n8<4 .
The forewings are fuscous-grey with a suffused white streak along the costa from the base to near the apex, with suffused whitish lines along the veins running into it. There is an irregular suffused white streak from the base along the fold throughout, and then along the termen to the apex. The dorsal area beneath this is mostly suffused with whitish anteriorly, posteriorly with a defined whitish line along vein 1b. The plical and second discal stigmata are indicated as cloudy round grey spots indenting the lower and upper margins of the plical streak respectively.
D. & J. Fowler Ltd. was a wholesale grocery company in Adelaide, South Australia, founded as a retail establishment by David Fowler in 1854, before becoming a leading wholesale and indenting firm in South Australia. They were the creators and owners of the well-known Lion brand, which included confectionery, flour, coffee, canned fruit and other goods; Lions brand flour endures, under different ownership today. The firm's interests and holdings were extensive, including the Adelaide Milling Company (purchased 1895), the Robur Tea Company (1931) and its subsidiary the Oriental Tea Company, Adelaide Bottle Company (1912) and others.
Location of Elephant Island in the South Shetland Islands Sintika Cove (, ‘Zaliv Sintika’ \'za-liv 'sin-ti-ka\\) is the 4 km wide cove indenting for 2.35 km the southeast coast of Elephant Island in the South Shetland Islands, Antarctica. It is entered north of Endurance Point and south of the end of Endurance Glacier, and surmounted by Mount Elder on the southwest. The feature was formed as a result of the retreat of Endurance Glacier in the first decade of 21st century. The cove is named after the ancient Thracian region of Sintika in Southwestern Bulgaria.
Brahms Inlet () is an ice-filled inlet, long and wide, indenting the north side of Beethoven Peninsula on Alexander Island between Harris Peninsula and Derocher Peninsula, while the headland Mazza Point lies immediately northeast of the inlet and Mount Grieg lies immediately southeast of the base of Brahms Inlet. It was observed from the air and first mapped by the Ronne Antarctic Research Expedition (RARE), 1947–48, and re-mapped from the RARE air photos by Derek J.H. Searle of the Falkland Islands Dependencies Survey in 1960. It was named by the UK Antarctic Place-Names Committee after Johannes Brahms, the German composer.
Hushen Glacier () is a glacier lying at the southwestern part of the base of the Mendelssohn Inlet, an inlet lying between Derocher Peninsula and Eroica Peninsula indenting the north face of Beethoven Peninsula, in the southwestern portion of Alexander Island, Antarctica. The glacier flows northeast while joining Reuning Glacier which discharges into the south part of Mendelssohn Inlet. It was mapped by the United States Geological Survey from U.S. Navy aerial photographs taken 1967–68 and from Landsat imagery taken 1972–73, and was named by the Advisory Committee on Antarctic Names for W. Timothy Hushen, Director of the Polar Research Board at the National Academy of Sciences, 1981–88.
Location of Greenwich Island in the South Shetland Islands George Powell's 1822 chart of the South Shetland Islands and South Orkney Islands featuring Yankee Harbour (as 'Hospital Cove') Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Yankee Harbour is a small inner harbour entered from Shopski Cove between Glacier Bluff and Spit Point, indenting the south-west side of Greenwich Island in the South Shetland Islands, Antarctica. It is long in west-south-west to east-north-east direction, and wide, and is bounded by Provadiya Hook to the south-west, Parvomay Neck to the north and east, and Kladara Beach to the south.
Lauritzen Bay is a bay about wide, occupied by bay ice and ice shell, indenting the coast of Antarctica between Cape Yevgenov and Coombes Ridge. The Matusevich Glacier Tongue joins Coombes Ridge in forming the west side of the bay. It was photographed from the air by U.S. Navy Operation Highjump in 1947, and was sketched and photographed by Phillip Law, leader of the Australian National Antarctic Research Expedition (ANARE) on the Magga Dan on February 20, 1959. It was then named by the Antarctic Names Committee of Australia for shipowner Knud Lauritzen of Copenhagen, Denmark, who supplied the Magga Dan and other vessels used by ANARE since 1954.
Location of Greenwich Island in the South Shetland Islands Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Discovery Bay is a bay long and wide, indenting the north side of Greenwich Island, in the South Shetland Islands of Antarctica. It had been known to sealers in the area since about 1821. It was charted and named in 1935 by Discovery Investigations personnel on the Discovery II. The Chilean Antarctic Expedition of 1947, under the command of Captain Federico Guesalaga Toro, decided to rename the name Bahía Chile as the site of Chile's first permanent Antarctic base, Base Soberanía, now Capitán Arturo Prat Base.
Nelson Island in the South Shetland Islands Argonavt Cove (, ‘Zaliv Argonavt’ \'za-liv ar-go-'navt\\) is the 1.85 km wide cove indenting for 950 m the north coast of Nelson Island in the South Shetland Islands, Antarctica. It is entered east of Retamales Point and west of Baklan Point. The cove is named after the ocean fishing trawler Agonavt of the Bulgarian company Ocean Fisheries – Burgas that operated in Antarctic waters off South Georgia and the South Orkney Islands during its fishing trip under Captain Kosyo Angelov from December 1978 to July 1979. A designated onboard team of marine biologists undertook fisheries research in the process.
Wohlschlag Bay () is a large bay indenting the west side of Ross Island between Harrison Bluff and Cape Royds. It was first charted by the Discovery Expedition under Robert Falcon Scott, 1901–1904, then named by the Advisory Committee on Antarctic Names (US-ACAN) in 1964 for Donald E. Wohlschlag, professor of biology at Stanford University, who outfitted the biology laboratories on the USNS Eltanin and at McMurdo Station. Romanes Beach is a beach on the north shore of Wohlschlag Bay just south of Harrison Bluff. It was mapped by a party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1958–59, landed there by the .
Location of Half Moon Island in the South Shetland Islands Menguante Cove (on the far side of Half Moon Island) from Kuzman Knoll, Livingston Island, with Greenwich Island in the background Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands Menguante Cove is a 1.47 km wide embayment indenting for 1.22 km the east coast of the horseshoe-shaped Half Moon Island in the South Shetland Islands, Antarctica. The area was visited by early 19th century sealers operating from nearby Yankee Harbour, and later by whalers; a whaling dory lies on the main landing beach on the southeast coast of the cove.Half Moon Island. Visitor Site Guidelines.
The U.S. is so destitute that a transcontinental railroad is never constructed past Iowa, while the Confederacy built seven. The only community of Americans who are generally prosperous are the Mormons in the western State of Deseret, who still practice polygamy. Otherwise, only successful landowners and the few lucky winners of the highly popular national lottery are able to rise above the semi-destitute lives of average citizens; most able-bodied adults are reduced to "indenting" themselves to businesspeople in exchange for the meager economic security that such affords. U.S. citizens are more hostile to Blacks than Confederates, seeing them as a major cause of the Union's downfall, and unwanted competition over the few available jobs.
Map of Thurston Island Satellite image of Thurston Island Peale Inlet is an ice-filled inlet about 16 nautical miles (30 km) long, lying immediately west of Noville Peninsula and indenting the north side of Thurston Island. Delineated from aerial photographs taken by U.S. Navy Operation Highjump in December 1946. Named by Advisory Committee on Antarctic Names (US-ACAN) for Titian Ramsay Peale, noted artist-naturalist who served on the sloop of war Peacock of the United States Exploring Expedition under Wilkes, 1838–42. The Peacock, accompanied by the tender Flying Fish, sailed along the edge of the pack ice to the north of Thurston Island for several days in March 1839.
Moutonnée Lake is a sub-glacial lake that lies within Moutonnee Valley, marginal to the George VI Ice Shelf, south of Ablation Point indenting the east coast of Alexander Island, facing the west coast of Palmer Land, Antarctica. Following limnological and tidal studies by the British Antarctic Survey (BAS) from 1971, it was named by the United Kingdom Antarctic Place- Names Committee (UK-APC) from the presence of roche moutonnées on its shores. As with nearby Ablation and Hodgson Lakes, Moutonnée receives large masses of ice from the adjacent George VI Ice Shelf in George VI Sound, making life in the lake unsustainable. The site lies within Antarctic Specially Protected Area (ASPA) No.147.
Schubert Inlet () is an ice-filled inlet, 14 nautical miles (26 km) long and 5 nautical miles (9 km) wide, indenting the west coast of Alexander Island lying between the Colbert north of the inlet and the Walton Mountains south of the inlet. Schubert Inlet receives ice flowing into it throughout the whole year mainly because the inlet is adjacent to the Wilkins Ice Shelf (which lies immediately west). The inlet was first mapped from air photos taken by the Ronne Antarctic Research Expedition in 1947–48, by Searle of the Falkland Islands Dependencies Survey in 1960. Named by the United Kingdom Antarctic Place-Names Committee for Franz Schubert (1797–1828), Austrian composer.
These are also defined in the grammar and processed by the lexer, but may be discarded (not producing any tokens) and considered non-significant, at most separating two tokens (as in `if x` instead of `ifx`). There are two important exceptions to this. First, in off-side rule languages that delimit blocks with indenting, initial whitespace is significant, as it determines block structure, and is generally handled at the lexer level; see phrase structure, below. Secondly, in some uses of lexers, comments and whitespace must be preserved – for examples, a prettyprinter also needs to output the comments and some debugging tools may provide messages to the programmer showing the original source code.
The Korsunsky work-of-indentation approach is a method of extracting a value of hardness for a small volume of material from indentation test data. Instead of relying on measurements or assumptions pertaining to the area of contact between indenter and sample, the method uses the load-displacement data registered in the continuously recorded indentation testing (CRIT) that is particularly widely applied in nanoindentation experiments. In particular, the method re-defines hardness and expresses it in terms of the energy (work) associated with indenting the surface of a material by the probe. The work-of- indentation used in the analysis may refer to the total, elastic or dissipated energy, depending on the formulation.
Darwin tcsh man page This allows indenting here documents in shell scripts (primarily for alignment with existing indentation) without changing their value: A script containing: LANG=C tr a-z A-Z <<\- END_TEXT Here doc with <<\- A single space character (i.e. 0x20 ) is at the beginning of this line This line begins with a single TAB character i.e 0x09 as does the next line END_TEXT echo The intended end was before this line echo and these were not processed by tr echo +++++++++++++++ LANG=C tr a-z A-Z << END_TEXT Here doc with << A single space character (i.e. 0x20 ) is at the beginning of this line This line begins with a single TAB character i.
His first successful recording and reproduction of intelligible sounds, achieved early in the following December, used a thin sheet of tin foil wrapped around a hand- cranked grooved metal cylinder. Tin foil was not a practical recording medium for either commercial or artistic purposes and the crude hand-cranked phonograph was only marketed as a novelty, to little or no profit. Edison moved on to developing a practical incandescent electric light and the next improvements to sound recording technology were made by others. Following seven years of research and experimentation at their Volta Laboratory, Charles Sumner Tainter, Alexander Graham Bell, and Chichester Bell introduced wax as the recording medium and engraving, rather than indenting, as the recording method.
The Gulf of Honduras is shown in the center-right The Gulf of Honduras is shown in the center of this map The Gulf or Bay of Honduras is a large inlet of the Caribbean Sea, indenting the coasts of Belize, Guatemala, and Honduras. From north to south, it runs for approximately 200 km (125 miles) from Dangriga, Belize, to La Ceiba, Honduras. The inner Gulf of Honduras is lined by the Belize Barrier Reef which forms the southern part of the 900 km (600 mile) long Mesoamerican Barrier Reef System, the second-largest coral reef system in the world. The Belize Barrier Reef includes a number of small islands, called cays, and collectively known as the Pelican Cays.
Expansion tools incorporate similar design features to WLSPA, using an internal piston assembly, except the main differences are that the piston is bi-directional, and does not detach to be left downhole. A hardened set of contoured pads expand when the piston is "stroked", indenting a small circle in the inner wall of the casing, and expanding the overall casing to make full contact with cement, packing material, or directly with the formation wall. The original design and concept of the tool was to stop surface casing pressure without impacting production by leaving hardware in the well bore. They can also be used in other applications like plugging and abandoning or drilling intervention operations like setting whipstocks.
Location of Livingston Island in the South Shetland Islands South Bay from Lyaskovets Peak George Powell's 1822 chart of the South Shetland Islands and South Orkney Islands featuring South Bay Topographic map of Livingston Island South Bay () is a wide bay indenting for the south coast of Livingston Island in the South Shetland Islands, Antarctica. The bay is lying northwest of False Bay and east of Walker Bay, and is entered between Hannah Point and Miers Bluff. The glaciers Kamchiya, Pimpirev, Perunika, Contell, Johnsons and Hurd Ice Cap feed the bay. South Bay was known to both American and British sealers as early as 1820, and the name has been well established in international usage for over 100 years.
A streaked morph of the nominate subspecies of tawny eagle. In flight, the tawny eagle appears as a large raptor with a noticeably protruding head on a long neck, with a deep chest, long and broad wings with a somewhat narrower seven-fingered hand. The trailing edge of the wing is slightly curved outwards, indenting at the junction of primaries and secondaries, whilst the rounded, medium-length tail is usually held spread. The deep beats of the kinked wings can make their flight appear rather heavy and slow but they are quicker and more expansive in wing movements and often less forceful-looking than larger Aquila like steppe eagles and can be very agile when chasing other raptors to rob them.
The Mariner Islands are a group of rocky islands and rocks forming the north- central group of the Highjump Archipelago, bounded by Edisto Channel on the west, Gossard Channel on the south, and Remenchus Glacier on the east. They were mapped from air photos taken by U.S. Navy Operation Highjump, 1946–47, and named by the Advisory Committee on Antarctic Names to commemorate the discovery of a large ice-free region at the west end of the Knox Coast by the crew of a Martin PBM Mariner seaplane commanded by D.E. Bunger. During photographic reconnaissance of this coastal area in January 1947, the aircraft landed on one of the inlets indenting the Bunger Hills and ground-level photographs and water samples were obtained at that time.
GNU nano implements several features that Pico lacks, including syntax highlighting, line numbers, regular expression search and replace, line-by-line scrolling, multiple buffers, indenting groups of lines, rebindable key support, and the undoing and redoing of edit changes. On 11 August 2003, Chris Allegretta officially handed the source code maintenance of nano to David Lawrence Ramsey. On 20 December 2007, Ramsey stepped down as nano's maintainer. On version 2.6.0 in June 2016, the current principal developer and the other active members of the nano project decided in consensus to leave the GNU project, because of their objections over the Free Software Foundation's copyright assignment policy, and their belief that decentralized copyright ownership does not impede the ability to enforce the GNU General Public License.
Location of Alexander Island in the Antarctic Peninsula region The north extremity of Alexander Island with Skaidava Bay in the centre and Rouen Mountains on the right Skaidava Bay (, ‘Zaliv Skaidava’ \'za-liv ska-i-'da- va\\) is the 10.5 km wide bay indenting for 3.2 km the north coast of Alexander Island, Antarctica 25 km west of the island's northeast extremity Cape Arauco. It is surmounted on the south by Mount Bayonne, the north extremity of Rouen Mountains. The vicinity was visited on 6 January 1988 by the geological survey party of Christo Pimpirev and Borislav Kamenov (First Bulgarian Antarctic Expedition), and Philip Nell and Peter Marquis (British Antarctic Survey). The feature is named after the ancient Thracian settlement and Roman fortress of Skaidava in Northeastern Bulgaria.
Location of Ioannes Paulus II Peninsula on Livingston Island in the South Shetland Islands Black Point from Cape Shirreff, with Tangra Mountains in the background Porlier Bay in the background (on the right) from Catalunyan Saddle, with Burdick Ridge in the foreground Topographic map of Livingston Island Porlier Bay (, ) is the 3 km wide bay indenting for 1.6 km the north coast of Ioannes Paulus II Peninsula on Livingston Island in the South Shetland Islands, Antarctica. It is entered between Punta del Medio and Black Point, and includes Spiller Cove on the southeast. The area was visited by early 19th-century sealers. The feature is named after Brigadier Rosendo Porlier y Asteguieta (1771–1819), commander of the Spanish naval squadron whose flagship San Telmo sank off the island with 644 men on board including Porlier in September 1819.
By mid-April 1877, Charles Cros had realized that a phonautograph recording could be converted back into sound by photoengraving the tracing into a metal surface to create a playable groove, then using a stylus and diaphragm similar to those of the phonautograph to reverse the recording process and recreate the sound. Before he was able to put his ideas into practice, the announcement of Thomas Edison's phonograph, which recorded sound waves by indenting them into a sheet of tinfoil from which they could be played back immediately, temporarily relegated Cros's less direct method to obscurity. Ten years later, the early experiments of Emile Berliner, the creator of the disc Gramophone, employed a recording machine which was in essence a disc form of the phonautograph. It traced a clear sound-modulated spiral line through a thin black coating on a glass disc.
These records could be multiplied at will to any extent, and each copy would sound precisely like the original. It was based on the Leon Scott Phonautograph, which was invented nearly forty years before, and which traced sound as curvilinear lines upon the smoked surface of a brass cylinder by means of a diaphragm with a stylus attached to its center. Early in 1877, or six months before the discovery of the phonograph principle by indenting tin-foil or wax, Charles Cros, of Paris, had conceived and placed on file the theory that if the curvilinear record of a Scott Phonautograph be photo-engraved, and such an engraving be made to act again on a stylus attached to a diaphragm, the original sound would be reproduced with absolute accuracy. This was the first conception of a sound-reproducing machine.
Schokalsky Bay with icebergs calved from the Hampton Glacier. Schokalsky Bay () is the easternmost bay of Alexander Island, Antarctica, 9 nautical miles (17 km) wide at its entrance and indenting 6 nautical miles (11 km) lying between Mount Calais and Cape Brown along the east coast of Alexander Island whilst adjacent to the George VI Ice Shelf in George VI Sound. Hampton Glacier discharges tremendous amounts of ice into the head of Schokalsky Bay at a steep gradient causing the ice there to be extremely broken and irregular, and discourages use of this bay and glacier as an inland sledging route onto northeast Alexander Island. The bay was first sighted from a distance in 1909 and roughly charted by the French Antarctic Expedition under Charcot who, thinking it to be a strait, gave the name "Detroit Schokalsky" after Yuliy M. Shokal'skiy, Russian geographer, meteorologist and oceanographer.
Location of Robert Island in the South Shetland Islands Coppermine Peninsula from English Strait, with Fort William in the foreground Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Coppermine Peninsula is the 1.7 km long, 500 m wide and rising to 105 m rugged rocky promontory forming the northwest extremity of Alfatar Peninsula and Robert Island in the South Shetland Islands, Antarctica and lying between English Strait to the west and Carlota Cove to the east. It is linked to Alfatar Peninsula to the southeast by a narrow isthmus bounded by Carlota Cove to the north and the 1 km wide and 460 m indenting Coppermine Cove () to the south. The feature is named in association with the adjacent Coppermine Cove, a descriptive name given by sealers in about 1821 from the copper-coloured staining of the lavas and tuffs in the area.
Instantaneous discs are so called because they can be played immediately after recording without any further processing, unlike the delicate wax master discs which had to be plated and replicated as pressings before they could be played non- destructively. By late 1929, instantaneous recordings were being made by indenting, as opposed to engraving, a groove into the surface of a bare aluminum disc. The sound quality of these discs was inadequate for broadcast purposes, but they were made for sponsors and performers who wanted to have recordings of their broadcasts, a luxury which was impractically expensive to provide by the wax mastering, plating and pressing procedure. Only a very few pre-1930 live broadcasts were deemed important enough to preserve as pressings, and many of the bare aluminum discs perished in the scrap metal drives of World War II, so that these early years of radio are mostly known today by the syndicated programs on pressed discs, typically recorded in a small studio without an audience, rather than by recordings of live network and local broadcasts.

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