منابع مشابه
Geomorphology of Uluru, Australia
A famous and well known Australian inselberg,1 Uluru,2 is an interesting geological feature in that its geomorphology is still a matter of controversy among conventional geologists. Traditionally, Uluru’s stratigraphical history began hundreds of millions of years ago, being fashioned into its current contour only as recently as between 60 million years ago until the present. The process by whi...
متن کاملGeomorphology of Uluru, Australia: Discussion
ISSN: 1937-9056 Copyright © 2011 Answers in Genesis. All rights reserved. Consent is given to unlimited copying, downloading, quoting from, and distribution of this article for non-commercial, non-sale purposes only, provided the following conditions are met: the author of the article is clearly identified; Answers in Genesis is acknowledged as the copyright owner; Answers Research Journal and ...
متن کاملGeomorphology of Uluru, Australia: Reply
ISSN: 1937-9056 Copyright © 2011 Answers in Genesis. All rights reserved. Consent is given to unlimited copying, downloading, quoting from, and distribution of this article for non-commercial, non-sale purposes only, provided the following conditions are met: the author of the article is clearly identified; Answers in Genesis is acknowledged as the copyright owner; Answers Research Journal and ...
متن کاملTectonic Geomorphology and Volcano-Tectonic Interaction in the Eastern Boundary of the Southern Cascades (Hat Creek Graben Region), California, USA
The eastern boundary of the Southern Cascades (Hat Creek Graben region), California, USA, is an extensively faulted volcanic corridor between the Cascade Range and Modoc Plateau. The morphology of the region is a result of plate motions associated with different tectonic provinces, faulting, and recurring volcanic activity, making it an ideal place to study the interrelationship between tectoni...
متن کاملTectonic geomorphology and hydrocarbon induced topography of the Mid-Channel Anticline, Santa Barbara Basin, California
The geomorphology of the western sector of the Mid-Channel Anticline (MCA), Santa Barbara, southern California suggests the actively growing fold is laterally propagating to the west. The presence of fold scarps and cross faults that segment the structure suggests that buried faults that are producing the folding are present at shallow depths. The summit area of the anticline at the Last Glacia...
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ژورنال
عنوان ژورنال: Geological Society, London, Special Publications
سال: 2010
ISSN: 0305-8719,2041-4927
DOI: 10.1144/sp346.13