Trisha Shetty (Editor)

Solifluction lobes and sheets

Updated on
Share on FacebookTweet on TwitterShare on LinkedInShare on Reddit
Covid-19
Solifluction lobes and sheets

Solifluction lobes and sheets are types of slope failure and landforms. In solifluction lobes sediments form a tongue-shaped feature due to differential downhill flow rates. In contrasts solifluction sheets sediment moves more-less uniformily downslope, being thus a less selective form of erosion than solifluction lobes.

References

Solifluction lobes and sheets Wikipedia


B
i
Link
H2
L