The Humboldt orogeny was a widespread mountain building event, preserved in rocks throughout much of East Antarctica including Mac. Robertson Land and the Humboldt Mountains of Queen Maud Land. The event deformed miogeoclinal deposits.[1]
See also edit
References edit
- ^ Anderson, John B. (1999). "Antarctic Marine Geology". Cambridge University Press. p. 30-32. ISBN 9780521593175.
 | This article about a regional geological feature is a stub. You can help Wikipedia by expanding it. |
.svg){kind=small} | This Antarctica-related article is a stub. You can help Wikipedia by expanding it. |