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Faịlụ:Debris flow channel, Ladakh, NW Indian Himalaya.JPG

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English: Debris flow channel in Ladakh, NW Indian Himalaya, produced in the storms of August 2010. Morphology is characteristic of debris flow deposits. Note coarse bouldery levees on both sides of the channel, mud drape on the insides of these levees, and poorly sorted rocks on floor of channel. The banding on the sides of the channel are evidence of pulsing in the flow during its waning stage. "Drip" structure on left side of the channel demonstrates the non-newtonian rheology of the debris flow material, which has failed and flowed down the rock below after deposition of the levee.
Ǹgụ́ụ̀bọ̀chị̀
Mkpọlọ́gwụ̀ Orü ọnwé
Odé ákwụ́kwọ́ DanHobley

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depicts Bekee

Oge/afọ mmalite

2 Jụn 2011

exposure time Bekee

0.008 second

f-number Bekee

4.5

focal length Bekee

6.3 millimetre

ISO speed Bekee

50

MIME ụdị

image/jpeg

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Bìri èhì/ogè k'ị hụ òtù ụ̀fa dị̀ m̀gbè ahụ̀.

Èhì/OgèMbọ-akaÓgólógó na asaáÒjìèmeNkwute
dị ùgbu â01:57, 2 Mee 2012NvóÁká màkà otù ȯ dị nà 01:57, 2 Mee 20123,072 × 2,304 (1.47 MB)DanHobley

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