|
Raven Ridge is a starkly visible sedimentary rock exposure located in Rio Blanco County, Colorado and Uintah County, Utah, USA. It is managed by the Bureau of Land Management. The ridge contains a diverse selection of rare plants unique to the state of Colorado. ==Geology== The Raven Ridge rock exposures provide an opportunity to understand this part of Earth’s history. This section through a sequence of rock layers that were deposited between ~53-49 million years ago, has become exposed because of its later tectonic history. The outcrops span the geological time interval that includes the early and middle portions of the Eocene epoch. During this time, ancestral horses, primates, and rodents, among many other mammal groups, were common at Raven Ridge. At the southern edge of Raven Ridge are found the only available surface coal beds in the area.〔 〕 The rocks of Raven Ridge were originally deposited on or near a shore line as horizontal sedimentary layers within the Uinta Basin. Uplift and folding associated with the later stages of the Laramide Orogeny subsequently tilted them into a nearly vertical position.〔〔 〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Raven Ridge」の詳細全文を読む スポンサード リンク
|