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Crevasse [geomorphology]
| Глоссарий геологических терминов |
(a) a wide breach or crack in the bank of a river or canal; especially one in a natural levee or an artificial bank of the lower mississippi river. compare - flood-plain splay, avulsion. (b) part 629 - glossary 629-20 (430-vi-nssh, 2008) a wide, deep break or fissure in the earth after an earthquake. [glaciology] a deep, nearly vertical fissure, crack, or rift in a glacier or other mass of land ice. gg
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Crevasse, английский
Crevasse filling, английский
A short, straight ridge of stratified sand and gravel believed to have been deposited in a crevasse of a wasting glacier and left standing after the ice melted; a variety of kame. may also occur as long, sinuous ridges and linear complexes of till or drift. gg
Crevasse splay, английский
(not recommended) use flood-plain splay. compare - crevasse.
Crevassed, английский
Especially, английский
Artificial, английский
- Искусственный
- Made to resemble a natural material or object, for example, faux marbre.
- A искусственный intelligence, language
- Bait made of some type of metal, plastic or rubber. comes in many colors, may be scented or unscented.
Mississippi, английский
- Шт. миссисипи (сша)
- Р. миссисипи (сша)
Earthquake, английский
- Землетрясение о ~ measured 7.0 on the richter scale землетрясение 209 earthquake-resistant интенсивностью 7 баллов по шкале рихтера
- Sudden fracturing and release of energy from stresses built up over a
Glaciology, английский
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Crevasse filling, английский
A short, straight ridge of stratified sand and gravel believed to have been deposited in a crevasse of a wasting glacier and left standing after the ice melted; a variety of kame. may also occur as long, sinuous ridges and linear complexes of till or drift. gg
Crest [geomorphology], английский
A geomorphic component of hills consisting of the convex slopes (perpendicular to the contour) that form the narrow, roughly linear top area of a hill, ridge, or other upland where shoulders have converged to the extent that little or no summit remains; dominated by erosion, slope wash and mass movement processes and sediments (e.g., slope alluvium, creep). commonly, soils on crests are more similar to those on side slopes than to soils on adjacent interfluves. compare - interfluve, head slope, side slope, nose slope. sw
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