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34 Sentences With "fall steeply"

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

But whatever the baseline, these numbers seem destined to fall steeply as a new generation rises.
Gazprom's head Alexei Miller has said Russian gas transit to Europe via Ukraine would fall steeply after 2020.
The interest rates brokers charged for Snap shares on Tuesday suggest demand is extremely high and that those borrowing the stock expect its price to fall steeply.
Vale, the world's largest iron ore exporter, has seen its production of the steel-making raw material fall steeply after a dam holding mining waste collapsed in January.
A senior U.S. sales manager has quit Volkswagen's North America operations, Automotive News reported, just as the carmaker's deliveries in the world's second-largest auto market fall steeply.
The company contacted the SIX Swiss Exchange after its stock started to fall steeply on Wednesday, with trading halted after a 9.2 percent drop and before its statement on Raxone.
BERLIN, Jan 6 (Reuters) - A senior U.S. sales manager has quit Volkswagen's North America operations, Automotive News reported, just as the carmaker's deliveries in the world's second-largest auto market fall steeply.
"Demand growth is falling and some volumes could return to the market after outages ... If prices begin to fall steeply again, then we will be able to and should continue consultations," Novak said.
Renzi, who came to power in February 2014 promising to kickstart a chronically stagnant economy, has seen his popularity ratings fall steeply over the last year as economic and job growth has remained listless.
Analyst Toni Sacconaghi of Bernstein cut both his second-quarter and full-year forecasts for iPhones but said he did not expect Apple's 2018 profit to fall steeply because of changes to U.S. tax law that will bring the company's rate down to 18 percent.
The northern slopes drop steeply to Glen Nevis, and there are two corries which end abruptly in cliffs which fall steeply into the Nevis gorge.
Llechog is a top of Garnedd Ugain on the Snowdon massif in Wales. It is the top of a long crest of cliffs that start in Llanberis and finishes on Garnedd Ugain. The nearby Clogwyn Station is a stop of the Snowdon mountain railway. The summit is a rocky peak sitting out from cliffs which fall steeply down to the Nant Peris valley.
The Stol massif stretches from Žirovnica in Slovenia to the Austrian market town of Feistritz im Rosental in the north. The summit is part of the Karawanks main ridge and the watershed between the Sava and Drava rivers. In the north, the Dachstein limestone rocks fall steeply to an over depth. The massif comprises several subpeaks, such as Mali Stol ('Little Chair'), at .
This Munro Top stands at the northern end of the ridge above the crags of Sròn na Creise which fall steeply to the valley of the River Etive. Sròn na Creise offers a challenging scrambler's route to the summit, but needs care in winter as several serious accidents have occurred on the crags.Mountaineering Council of Scotland. Details accidents on Sròn na Creise.
The hills fall steeply towards the north, but more gently north-eastward toward the coast. In the northeast of the area several sandy bays have formed at the mouths of so-called torrents. On the coastal hills can still be found towers built between the 16th and 18th century. Nestling amidst the hills, is the Ermita de Betlem, a hermitage inhabited by a monks.
On the southeast side, the rivers fall steeply through volcanic ash deposits where vegetation has largely recolonized the areas devastated by the volcano's eruption. On the northwest side, the rivers are more gently sloped and the land is boggy with lush vegetation. The southeast coastal region is deeply indented, with coastal cliffs, headlands and islands. Three large bays are the remnants of earlier volcanic craters.
Scree slopes fall away below to the headwaters of the River Liza, which flows down Ennerdale. There are few crags on the eastern slopes, although these fall steeply to Styhead Tarn, a feeder of the Borrowdale system. About deep, this tarn occupies a scooped hollow, dammed by boulders fallen from the slopes above. It is reputed to contain trout and is a popular location for wild camping.
Mat river flowing through the gorge. The Skanderbeg Mountains () forms the border between the Central Mountain Range and Western Lowlands in the west. Although the range curves a lot, its main direction is from the north to south, extending about in north- south direction from Vau i Dejës in the north to the city of Elbasan in the south. In the west, the mountains fall steeply into the coastal plain, running along the Adriatic Sea.
The bowl-shaped Rehburg Hills were formed by relief inversion. They fall steeply away to the north, but its southern slopes are more gently. The ridge is, from a geological viewpoint, a saddle (the Rehburg Saddle or Rehburger Sattel), which consists of solid rock. The bulging of the saddle occurred as a result of the movement of Malm Salt (not Zechstein Salt) deep underground that forced the overlying, younger layers of solid rock upwards.
Topography of Africa The high southern and eastern plateaus, rarely falling below , have a mean elevation of about . The South African Plateau, as far as about 12° S, is bounded east, west and south by bands of high ground which fall steeply to the coasts. On this account South Africa has a general resemblance to an inverted saucer. Due south, the plateau rim is formed by three parallel steps with level ground between them.
The Hochkönig is the southernmost and highest mountain block in the Berchtesgaden Alps. Unlike the Watzmann massif about 20 kilometres to the north, it has a plateau that tilts gently towards the north and covers about 15 km². Only in the south does it fall steeply away in rock faces up to 1,000 metres high (the Mandlwände). The edge of the plateau is formed by several high two-thousanders in the shape of a giant oval.
The edges of this plateau then fall steeply to the east and west sides. The mountain vegetation is largely composed of heath around the summit plateau with evergreen forest along the wetter eastern slopes and grassland to the western side. Annual rainfall totals are high (around 2200 mm) but long spells of dry weather occur during the winter period of May to August. Due to its relatively low altitude and tropical location, snow falls very rarely, last recorded in August 1935.
For the most part these flanks fall steeply to the shore, with several areas of woodland on the lower slopes. The exception is Silver Point, the promontory separating the upper and middle reaches of the lake. This is formed by Silver Crag (890 ft), an outlier standing apart from the mass of the fell. The lakeshore path from Sandwick in the north to Patterdale in the south was described by Wainwright as the most beautiful and rewarding walk in Lakeland.
The river itself does not enter on the main line of the Harbour but curves northwards and then runs south into the inlet. The northern shore rises sharply to a much greater extent than the southern, which is in places merely hilly. On that northern shore lies the mountain Mweelrea, Connacht's highest, rising to , and the sides of which fall steeply into the inlet, with Uggool Beach at its western edge. To the south rise the Maumturk Mountains and the Twelve Bens.
The reconstituted Protestant Hussite Church and the Czech Brethren were major beneficiaries of this defection from Catholicism until after World War II, when the overall belief in organized religion started to fall steeply. In addition, the Sudeten Germans, who were those Austrians who ended up within Czech borders after World War I, were mostly Catholics, and their expulsion after World War II also reduced the Church's presence. Over 90% Catholic in 1910, the Czech Republic is now reduced to some 10%.
Several shareholder lawsuits revolved around questionable accounting practices during 2012. In May 2013 the NASDAQ gave OCZ until September 16, 2013 to file its delayed earnings. The company was several quarters late in filing and restated earnings all the way back to 2008. On September 12, 2013, the company disclosed it would not meet the deadline, which was then extended to October 7. 2013 saw OCZ's revenue fall steeply from $88.6 million in the second fiscal quarter of 2012 to $33.5 million in the second fiscal quarter of 2013, while financial losses increased.
Much of the mountain range's area is protected within the King Range National Conservation Area, a National Conservation Area unit of the National Landscape Conservation System, and in the King Range Wilderness Area, both managed by the Bureau of Land Management (BLM). As part of the Northern Coast Ranges, the King Range runs parallel to the coast, and its western slopes fall steeply to the Pacific Ocean. The King Range is adjacent to the Mendocino Triple Junction, where three tectonic plates — the Pacific Plate, the North American Plate, and the Juan de Fuca Plate — meet. The area experiences frequent earthquakes.
Another minor summit, Rudha na Spreidhe, lies at the end of the mountain's northern spur and gives good views of Loch Monar; this was also formerly classed as a top, but has now been deleted from Munro's Tables. Deep, glacial corries surround the mountain on several sides. To the south-east of the summit the slopes fall steeply into a large corrie containing Loch Tuill Bhearnach, the largest of Sgurr na Lapaich's lochans at around 500 metres wide; further south is a smaller corrie surrounding Loch a' Choire Bhig. Both of these lochans drain into Loch Mullardoch.
The mountain's name translates from the Gaelic language as "Mountain of the Castle", a name which reflects the fortress like nature of its western flanks which fall steeply and rockily to the Auch Glen. The former spelling of Ben Achastle confirms that it is a name which goes well back into history."The Call Of The Corbetts", Irvine Butterfield, Page 157 Gives etymology details. However the hills name may not just come from its physical appearance as W.J. Watson in his book "Circular Forts of North Perthshire" (1913) reveals that a circular fortification stood on one of the spurs of Beinn a' Chaisteil and the name may come from that.
The catchment of this system is on the Lévézou plateau- which is at the western end of the Grandes Causses. The plateau lies between 700 m and 900 m and consist of granite rocks. It is a landscape of gentle valleys, drained to the north by the Ceor, Viaur, Bage and Violou which flow towards Rodez, and to the south by the Alrance and the Ruisseau de Asseynes which fall steeply into the Tarn. To the south, exploiting a geological fault is the River Tarn which is at 265 m altitude, and to the south of the river the land rises again to over 600 m.
After the Leine trough has been blocked and flows around the Hube, it runs through the Alfeld Uplands (Alfelder Bergland), also called the Ith-Hils Upland (Ith- Hils-Bergland), which is characterised by a succession of closely spaced ridges and finger valleys running in a northwest-southeast direction. East of the massifs that give the region its alternative name, the Ith and the Hils, which are up to 480 m high, the ridges fall steeply on both sides of the Leine into the valley and are dissected by various tributaries. Beech woods dominate the heights whilst the valleys are used for arable farming. Large areas of the countryside are protected.
The next stop was Hartington, where after about a couple of miles the line began to fall steeply again at 1 in 60 through Alsop en le Dale, Tissington, Fenny Bentley, where there was a goods depot, and Thorpe Cloud, and finally through Church St tunnel to Ashbourne. It can be seen that the gradients and curves meant that it was always a difficult line to work, particularly during winter when it was exposed to the elements on the high moors. By contrast, the line from Ashbourne southwards was relatively easy, following river valleys as it did, first the Henmore Brook and then the River Dove.
Aside from a few ex-council estates which retain significant proportions of social housing in parts of Mottingham and Bromley Common, this constituency is relatively prosperous in terms of income, has low unemployment and is largely suburban with significant parkland and sports areas. The 2011 census shows that the borough is 84.3% White European/British, lower than the national average (86%) and higher than then London average (59%). Until 2006 it was one of the Conservative Party's safest seats but the by-election of that year saw the party's electoral majority fall steeply from over 13,000 (in the 2005 election) to just over 600 votes (see below - "Election results"). They have since rebuilt this majority, which currently stands at just under 11,000.
Tor Ghar is bounded on the south by Tanawal; on the east by Agror, Pariari, Tikari, Nandihar and Deshi; on the northern extremity lies the River Indus and Thakot; and on the west, between the crest and the River Indus. These slopes fall steeply from the crest for some 2000 feet; then follows a zone of gentle, well-cultivated slopes; and then from 4000–5000 feet altitude the hill drops precipitously to the Indus. The actual Indus Valley here varies in width from a few hundred yards to nearly two miles, being narrowest at Kotkai and at its broadest at Palosi. It is crossed at about eleven different points by ferries, the boats holding from twenty to thirty passengers, but the inhabitants pass over the river almost everywhere on inflated skins.

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