They took on new energy; the golds and reds and flesh tones became warmer.
|
|
He became warmer — it was like he would stand in a way with Matilda that you knew they were linked.
|
|
Initially tired from a day of doing press, Madden became warmer and more animated as he spoke, his blue eyes widening often for emphasis.
|
|
As the waters in the sound became warmer and warmer during the summer months, the cooling current couldn't keep up, and cold-water species such as lobsters no longer thrived in southern New England.
|
|
The dominant vegetation was eucalyptus woodlands that were displaced by grassland as the climate of the region became warmer and drier.
|
|
Formation of bogs in Latvia started in the postglacial period, approximately 10,000 years ago as the climate became warmer and more humid. Thus allowing Sapropelic mud formation at the bottom of the lake, consisting of sandy soil and the remains of water plants and animals.
|
|
75, 86. In supplying this demand, the ice trade increasingly shifted north, away from Massachusetts and towards Maine.Weightman, p. 172. Various factors contributed to this. New Englands' winters became warmer during the 19th century, while industrialisation resulted in more of the natural ponds and rivers becoming contaminated.
|
|
After the glacier melted, the area was cold and wet. The area was a Tundra Biome which grasses grew slowly. This is when Paleo Indians came into the area around 11,000 B.C. After several thousand years, the area became warmer. As the climate warmed, vegetation patterns changed.
|
|
She also posed nude for many of his photos and took images of him. Both had separate studios in their home. After Eakins' death in 1916, she returned to painting, adding considerably to her output right up to the 1930s, in a style that became warmer, looser, and brighter in tone. She died in 1938.
|
|
They waited only for opportunities to get away. By 1857 only four of the original residents were left, and the survivors reported more illness as the weather became warmer again. The area remained remote until 1873 with the arrival of the railroad. The town of Chanute, Kansas sprang up four miles (6 km) south of the former commune.
|
|
As the sea became warmer, the ocean floor released a massive amount of methane. As the methane reached the atmosphere, the earth became even warmer, which led to the extinction of even more lifeforms on land. In the program, the extinction is argued to have lasted less than 1 million years.The Day The Earth Nearly Died, www.bbc.co.uk.
|
|
The species is found in the high hills and is part of a complex of several species which are thought to have speciated by being isolated in the cool tops of the higher hills of southern India as the climate became warmer. Earlier included in other genera, they were placed in a newly established genus in 2017.
|
|
Even buffalo were much larger than today. The glaciers continued to retreat and the climate became warmer over the next few millennia; the giant creatures died out about 9,000 years ago.Ojakangas and Matsch, Minnesota’s Geology, pp. 116–18. This glaciation has drastically remodeled most of Minnesota, and all but two of the state's regions are covered with deep layers of glacial till.
|
|
Fitzroya cupressoides and tepú (Tepualia stipularis) grow in the poorly drained soils of the Piuchén and Pirulil ranges. Before the end of the Llanquihue glaciation, the southern parts of Chiloé Island constituted open landscapes. This changed around 12,500 years ago when the climate became warmer and forests colonized the region. The upper portions of Cordillera del Piuchén, locally known as la Campaña, has a Magellanic moorland vegetation.
|
|
Oregon's Jurassic invertebrates, such as the reef-building clam Lithiolus problematicus and the mussel-like Buchia piochii, indicate shallow sea environments similar to those of the state's late Triassic. Among Oregon's Jurassic-aged vertebrate fossils are the remains of marine crocodiles, tentatively identified in the genus Metriorhynchus. These crocodiles likely shared Oregon's Jurassic seaways with ichthyosaurs. Plant fossils from Oregon's Jurassic period show that the terrestrial environment became warmer and wetter, creating swampy conditions.
|
|
The most recent glaciation, the Devensian, ended about 10,000 years ago. The higher parts of the North York Moors were not covered by the ice sheets but glaciers flowed southwards on either side of the higher land mass. As the climate became warmer at the end of the ice age the snowfields on the moors began to melt. The meltwater was unable to escape northwards, westwards or eastwards because it was blocked by ice.
|
|
The raven diverged into the ancestor of the forest and little ravens in the east and Australian raven in the west. As the climate was cooler and drier, the aridity of central Australia split them entirely. Furthermore, the eastern diverged into nomadic little ravens as the climate became dryer and, in forested refuges, forest ravens. As the climate eventually became warmer, the western ravens spread eastwards and outcompeted forest ravens on mainland Australia but coexisted with little ravens.
|
|
As the climate was cooler and drier, the aridity of central Australia split them entirely as the habitat between became inhospitable. Furthermore, the eastern diverged into nomadic little ravens and, in forested refuges, forest ravens. As the climate eventually became warmer, the western ravens spread eastwards and outcompeted forest ravens on mainland Australia, as evidenced by the forest ravens' being found only in closed forest refuges on the mainland but in a wider variety of habitats in Tasmania.
|
|
The Earth was generally cold during the early Cambrian, probably due to the ancient continent of Gondwana covering the South Pole and cutting off polar ocean currents. However, average temperatures were 7 degrees Celsius higher than today. There were likely polar ice caps and a series of glaciations, as the planet was still recovering from an earlier Snowball Earth. It became warmer towards the end of the period; the glaciers receded and eventually disappeared, and sea levels rose dramatically.
|
|
Brachiopods lost much of their former diversity as well. On land, most families of amphibians and reptiles became extinct. alt= The eastern coast of the US became warmer and wetter during the Early Jurassic because the newly formed Atlantic Ocean brought it into contact with more humid air. Fossils from spanning from the Late Triassic to Early Jurassic were preserved in the Newark Supergroup, which is found between the Canadian province Nova Scotia and South Carolina.
|
|
The gradual transition period is sometimes termed Mesolithic (northern and western Europe) or Epipalaeolithic (Levant and Near East). The glaciers retreated as the world climate became warmer and that inspired an agricultural revolution, though at first the dog was probably the only domesticated animal. This was accompanied by a social revolution in that humans gained from agriculture the impetus to settle. Settlement is the key precursor to civilisation, which cannot be achieved by a nomadic lifestyle.
|
|
The habitat is mostly barren and exposed to full sun and harsh winter weather. This is one of several goldenrods that are relict species, plants that were more common when conditions were colder and wetter. As glaciers receded, the area became warmer and drier, and plants such as this goldenrod were left in areas that most resemble the alpine climate to which it was adapted. It now persists in the high mountain peaks that have the harshest winter conditions.
|
|
Colonel Wilma Deering was portrayed by actress/model Erin Gray in the 1979 movie and subsequent NBC television series Buck Rogers in the 25th Century. Initially, Wilma was depicted as a cold, aloof military officer and starfighter pilot, with little interest in Captain Rogers. However, she quickly warmed to him and, throughout the weekly series, Wilma Deering's character became warmer, sexier, and more humorous. Often, it was Wilma who came to the rescue of Buck, as opposed to the other way round.
|
|
On each occasion ice fields formed on the higher land and sent glaciers down the main valleys. There was scouring of material from the valley sides by the glaciers and this was deposited on lower ground as the ice retreated when the climate became warmer. In Yorkshire the higher land of the North York Moors stood proud of the glaciers, the Pennine valleys show classic glacial features and there was abundant deposition in the Vale of York and Holderness as the ice melted.
|
|
As the climate became warmer, the late Magdalenian peoples of Iberia modified their technology and culture. The main techno-cultural change is the process of microlithization: the reduction of size of stone and bone tools, also found in other parts of the World. Also the cave sanctuaries seem to be abandoned and art becomes rarer and mostly done on portable objects, such as pebbles or tools. It also implies changes in diet, as the megafauna virtually disappears when the steppe becomes woodlands.
|
|
At the peak of this high-water phase, most of Finland was under water, including present-day Helsinki at a depth of ; only southern Sweden was both free of ice and above the waterline. The Danish Islands were all connected west of the Strait of Oresund. Around 10,500 BP the climate became warmer, the ice retreated to the north of Mount Billingen, and the waters broke through central Sweden again, providing a second egress. Water level dropped to the sea level of that time.
|
|
During the reign of Augustus the climate became warmer and the aridity in North Africa persisted. The biotopes of Heterogaster urticae, which in Roman times occurred farther north than in the 1950s, suggest that in the early Empire mean July temperatures were at least 1 °C above those of the mid-20th-century. Pliny the Younger wrote that wine and olives were cultivated in more northerly parts of Italy than in the previous centuries, as did Saserna in the last century BC (both father and son).
|
|
Utah Lake is a remnant of a much larger pleistocene lake called Lake Bonneville, which existed from 75,000 to 8,000 years ago. At its peak 30,000 years ago, Lake Bonneville reached an elevation of above sea level and had a surface area of , which was nearly as large as Lake Michigan. The weight of the lake depressed sections of the lake bottom by as much as before the surface rebounded when the lake dried up. About 12,000 years ago, the climate of the region became warmer and drier.
|
|
This early phase came to an end with the onset of the Ice Age during which there is no evidence of a human presence in Warwickshire.Archaeology in Warwickshire, The Old Stone Age Human groups returned to the area around 10,500 years ago at the beginning of the Mesolithic period or Middle Stone Age. As the climate became warmer and the ice sheets retreated, the habitat changed and the forest was re-established. These people were hunter-gatherers who used bows and arrows and had domesticated dogs to help them in the chase.
|
|
During the transition from the last glacial to the Holocene, the Huelmo–Mascardi Cold Reversal in the Southern Hemisphere began before the Younger Dryas, and the maximum warmth flowed south to north from 11,000 to 7,000 years ago. It appears that this was influenced by the residual glacial ice remaining in the Northern Hemisphere until the later date. The Holocene climatic optimum (HCO) was a period of warming in which the global climate became warmer. However, the warming was probably not uniform across the world. This period of warmth ended about 5,500 years ago with the descent into the Neoglacial and concomitant Neopluvial.
|
|
The potential for mining fluorine-containing minerals to obtain the raw material necessary for the production of CFCs and PFCs is supported by mineralogical surveys of Mars that estimate the elemental presence of fluorine in the bulk composition of Mars at 32 ppm by mass (as compared to 19.4 ppm for the Earth). Alternatively, CFCs might be introduced by sending rockets with payloads of compressed CFCs on collision courses with Mars. When the rockets crashed into the surface they would release their payloads into the atmosphere. A steady barrage of these "CFC rockets" would need to be sustained for a little over a decade while Mars changed chemically and became warmer.
|
|
From ancient times, people suspected that the climate of a region could change over the course of centuries. For example, Theophrastus, a pupil of Aristotle, told how the draining of marshes had made a particular locality more susceptible to freezing, and speculated that lands became warmer when the clearing of forests exposed them to sunlight. Renaissance and later scholars saw that deforestation, irrigation, and grazing had altered the lands around the Mediterranean since ancient times; they thought it plausible that these human interventions had affected the local weather. Vitruvius, in the first century BC, wrote about climate in relation to housing architecture and how to choose locations for cities.
|
|
Around the IJsselmeer is an arc of boulder clay high areas of land, which formed during the Ice Age glaciations of the Pleistocene epoch: Texel, Wieringen, Urk, de Voorst, and Gaasterland. To south of that arc, as a result of meltwater, a lake formed, which became known as Almere. North of the boulder clay highland of Urk, the Vecht river flowed into the Almere, while the river IJssel with tributaries flowed into the south of Urk. As the climate became warmer during the Middle Ages, the sea level rose; and since the Ice Age ended the Netherlands and around have been slowly steadily sinking because of forebulge effect.
|
|
São Joaquim, Brazil Cfb climates are predominant in most of Europe except the northeast, as global temperature became warmer towards late 20th and early 21st century. However, just few decades ago, oceanic climate was only present in parts of Western Europe, including northern Spain, Northwestern Portugal (mountains), Belgium, Britain, France, Ireland and the Netherlands. They are the main climate type in New Zealand and the Australian states of Tasmania, Victoria and southeastern New South Wales (starting from the Illawarra region). In North America, they are found mainly in Washington, Oregon, Vancouver Island and neighbouring parts of British Columbia, as well as many coastal areas of southwest Alaska.
|
|
Hanna initially spent much of his time in New York, where many financiers were based. He faced resistance at first, both because he was not yet widely known on the national scene, and because some moneymen, although appalled at the Democratic position on the currency issue, felt Bryan was so extreme that McKinley was sure to win. Others were disappointed New York Governor Morton was not the presidential nominee, but their support became warmer as they came to know McKinley and Hanna. Reports of Bryan support in the crucial Midwest, and intervention by Hanna's old schoolmate, John D. Rockefeller (his Standard Oil gave $250,000), made executives more willing to listen.
|
|
Ancient cross close to Crazywell Pool The climate became wetter and cooler over the course of a thousand years from around 1000 BC, resulting in much of high Dartmoor being largely abandoned by its early inhabitants. It was not until the early Mediaeval period that the weather again became warmer, and settlers moved back onto the moors. Like their ancient forebears, they also used the natural granite to build their homes, preferring a style known as the longhouse — some of which are still inhabited today, although they have been clearly adapted over the centuries. Many are now being used as farm buildings, while others were abandoned and fell into ruin.
|
|
Populations of Desmognathus organi can be found in high elevation spruce-fir and hardwood forest habitats in the Blue Ridge Mountains. It is rare to find this species below 1500m. It is thought that historically the distribution of spruce-fir forests and subsequent populations of pygmy salamanders may have been continuous at one point, but as the climate became warmer and drier populations became isolated on the high elevation "islands" that we see today. This species occurs north and east of the French Broad river, ranging from the southwesternmost part of Virginia, particularly Mount Rogers and Whitetop Mountain, to the ridges of western North Carolina and eastern Tennessee.
|
|
His teammate Barrichello, Felipe Massa and Nick Heidfeld of Sauber, Jordan drivers Giancarlo Fisichella and Takuma Sato, Coulthard, Arrows' Heinz-Harald Frentzen, and the British American Racing (BAR) duo of Jacques Villeneuve and Olivier Panis, were second through tenth. Some drivers—including Barrichello, Massa and Fisichella—ran off the dusty, slippery track into a gravel trap during the session because of a low amount of grip; none sustained damage to their vehicles. Conditions became warmer and sunnier for the second practice session though rainfall threatened towards the end. The fastest times to be recorded within the first 20 minutes since the track temperature was at its warmest.
|
|
The early Cambrian climate was probably moderate at first, becoming warmer over the course of the Cambrian, as the second-greatest sustained sea level rise in the Phanerozoic got underway. However, as if to offset this trend, Gondwana moved south, so that, in Ordovician time, most of West Gondwana (Africa and South America) lay directly over the South Pole. The early Paleozoic climate was also strongly zonal, with the result that the "climate", in an abstract sense, became warmer, but the living space of most organisms of the time—the continental shelf marine environment—became steadily colder. However, Baltica (Northern Europe and Russia) and Laurentia (eastern North America and Greenland) remained in the tropical zone, while China and Australia lay in waters which were at least temperate.
|
|
Political relations between the Soviet Union and Zambia were challenged by Chinese presence in Zambia, and the cordial attitude of the Kaunda government towards the West, however, Kaunda visited the Soviet Union on state visits in 1974 and 1987. The Soviet embassy in Lusaka (now the Russian embassy) was the largest embassy in Southern Africa. Relations between the two countries soured in 1976, when Kaunda said on the Soviet and Cuban presence in Angola, "(t)hey drove colonialism and fascism out the front door, only to let a plundering tiger and its cubs in the back door." Soviet support for the Zimbabwe African People's Union, which operated primarily out of Zambia, helped to stop relations from detiorating further, and ties became warmer after Abel Muzorewa, the Prime Minister of Zimbabwe Rhodesia launched airstrikes inside Zambia in 1979.
|
|
The East Riding has two quite distinctive and contrasting archaeological areas, the Yorkshire Wolds and the Humber Wetlands. The Yorkshire Wolds form an upland arc of chalk hills stretching from Flamborough head on the coast to the Humber Estuary at its southern end. The Humber Wetlands consist of all the land in the Humber basin that lies below 10 metres above sea level which encompasses a large part of Holderness and the valleys of the Rivers Hull and Derwent and the lower part of the River Ouse valley. The Arctic conditions associated with the last Ice Age started to improve and the climate gradually became warmer about 10,000 BC. This warming-up process suffered several temporary setbacks as short, cool spells occurred which disrupted the overall momentum. By about 9,000 BC the vegetation had changed from tundra to a closed woodland, of pine and birch.
|
|