- Toreva block
A Toreva block landslide is a distinctive
landslide type which may occur when a stronger material such as sandstone or limestone overlies a weaker material such asshale and an eroding agent undercuts the weaker lower layer. The type was first recognized by "Parry Reiche" in 1937, and takes its name fromToreva, Arizona . Toreva blocks exhibit a characteristic backward rotation toward the parent cliff.The existence of Toreva blocks may be used to infer a warmer or wetter earlier climate, e.g. toreva blocks in the
Transantarctic Mountains .References
cite journal
last = Reiche
first = Parry
authorlink =
coauthors =
title = The Toreva block, a distinctive landslide type
journal = Journal of Geology
volume = 45
issue = 5
pages = 538–548
publisher =
date =
url =
doi =
id =
accessdate =External links
* [http://web.umr.edu/~rogersda/cp_megalandslides/toreva,_az.htm Toreva, AZ Landsliding]
* [http://gsa.confex.com/gsa/2002AM/finalprogram/abstract_38572.htm TOREVA BLOCKS IN THE TRANSANTARCTIC MOUNTAINS: IMPLICATIONS FOR CENOZOIC PALEOCLIMATE]
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