crevasse

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crevasse的示例

  • Since rock walls do not contain any cementing material, the runoff water is retained, filtered, and slowly released through the existing crevasses.

  • Transported logs and wood fragments occur in siltstone and sandstone units variously interpreted as river channel deposits, flood deposits and crevasse splay deposits.

  • In clear weather they got across the final crevasses and moved down just ahead of a descending cloud base.

  • They found that a crevasse 15 km in height in an ice shell 75 km thick would trap y4.9r109 m3 of ammonia- water.

  • Each time you move from one gallery to another you cross the line of a crevasse and glimpse the horizon.

  • These sheer crevasses provide a strongly contained view of the horizon.

  • Sheeted sandstone deposits represent crevasse splays, which deposited sand more uniformly in overbank areas.

  • They are assigned to a crevasse splay origin.

  • A mental module probably looks more like a roadkill, sprawling messily over the bulges and crevasses of the brain (1998, 30).

  • The active flood plains of major rivers are only 1-2 km wide and produce 3-5 m thick natural levees, crevasse channels and flood-plain deposits.

  • The festival brochure claimed that the film reinvented 'folklore and fairytales', whilst being 'an uncompromising cinematic look at the darker crevasses of society and human nature'.

  • The overbank areas received influxes of coarse and fine sediment as sheet flows and crevasse splays, but were sufficiently stable to allow the formation of soils.

  • These typically low-lying areas with respect to the river channels are characterized by the facies architecture that indicates crevasse splay and suspended fall-out of fine-grained sedimentation.

  • A team of 30 specialists flew in, but not before radar and satellite images had been used to plot the position of every crevasse in the vicinity.

  • Mitri et al. (in review) have shown that ammonia-water mixtures can erupt from such an ocean by bottom crevasse formation and subsequent transport by convective motions in the ice shell.

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