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Outcrop

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369: 470: 354: 448: 429: 406: 391: 598: 335: 122: 25: 586: 292:, cliffs are distinguished from outcrops: cliffs have a continuous line along the top edge with lines protruding down; outcrops have a continuous line around each area of bare rock. An outcrop example in 556: 260:
Accurate description, mapping, and sampling for laboratory analysis of outcrops made possible all of the geologic sciences and the development of fundamental geologic laws such as the
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orientations. Outcrops are also very important for understanding fossil assemblages, and paleo-environment, and evolution as they provide a record of relative changes within geologic
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of earth history. Some of the types of information that cannot be obtained except from bedrock outcrops or by precise drilling and coring operations, are
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Bedrock and superficial deposits may also be exposed at the Earth's surface due to human excavations such as quarrying and building of transport routes.
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Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by
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and vegetation and cannot be seen or examined closely. However, in places where the overlying cover is removed through
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erosion during the last glacial maximum (ca. 11000 BC), followed by scouring by sea waves, followed by
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Visible exposure of bedrock or ancient superficial deposits on the surface of the Earth
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rate such as on steep hillsides, mountain ridges and tops, river banks, and
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and outcrops are therefore extremely important for understanding the
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has produced many smooth coastal and littoral outcrops.
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Outcrops allow direct observation and sampling of the
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"Outcrop"
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bedrock
superficial deposits
terrestrial planets
soil
erosion
tectonic uplift
erosion
weathering
tectonically active
Finland
glacial
isostatic uplift
bedrock
in situ
geologic
geologic maps
geological history
geologic time scale

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