Ice-sheets sentence example
- Some of the stiff boulder clays or " till " so prevalent over parts of the north of England appear to have been deposited from ice sheets during the glacial period.
- The great ice sheets formed terminal moraines around their border at various halting stages; but the morainic belts are of small relief in comparison to the great area of the ice; they rise gently from the till plains to a height of 50, 100 or more feet; they may be one, two or three miles wide; and their hilly surface, dotted over with boulders, contains many small lakes in basins or hollows, instead of streams in valleys.
- The morainic belts are arranged in groups of concentric loops, convex southward, because the ice sheets advanced in lobes along the lowlands of the Great Lakes; neighboring morainic loops join each other in re-entrants (north-pointing cusps), where two adjacent glacial lobes came together and formed their moraines in largest volume.
- When the ice sheets fronted on land sloping southward to the Ohio, Mississippi and Missouri rivers, the drift-laden streams flowed freely away from the ice border; and as the streams, escaping from their subglacial channels, spread in broader channels, they ordinarily could not carry forward all their load; hence they acted not as destructive but as constructive agents, and aggraded their courses.
- It must therefore have been a sort of oasis, when the ice sheets from the north advanced past it on the east and west and joined around its southern border.Advertisement
- There are no permanent ice sheets known on the mainland of north-eastern Canada, but some of the larger islands to the north of Hudson Bay and Straits are partially covered with glaciers on their higher points.
- The glacial deposits profoundly modified the surface of the country, whether they resulted from the melting of the ice-sheets of the time of maximum glaciation, or from the movements of local glaciers.
- anthropogenic climate warming will accelerate the natural process toward reduction in polar ice sheets.
- calveving of icebergs from these ice streams is the main way in which ice is lost from the Antarctic ice sheets.
- Recent discoveries show a major hidden source of water comes from polar ice sheets.Advertisement
- During the colder phases, large ice sheets formed over the northern hemisphere land masses.
- terminal moraines, the deposits dropped at the front of a glacier, mark stages in the retreat of the ice sheets.
- Drive slowly and be prepared for invisible ice sheets on the road.