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

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Mmẹkụwátá

Nkówá
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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I, the copyright holder of this work, hereby publish it under the following license:
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í-kpó-áhà gbásàa kà
Edebere faịlụ a n'okpuru ikikeree Creative Commons Attribution-Share Alike 3.0 Unported license.
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Nkowapụta

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Ihe ndị egosiri na faịlụ a

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

Ịta nke usòrò

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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