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Stones Tell the Story: The geologic history of Shenandoah National Park

  Рет қаралды 1,192

Shenandoah National Park Trust

Shenandoah National Park Trust

Күн бұрын

The Appalachians are one of the oldest mountain ranges in the world, and they hold hints of history far beyond written records and traditional storytelling. This foundational knowledge of the Blue Ridge Mountains sets the scene for all of the unique stories, incredible flora and fauna, breathtaking vistas, and stunning natural features that make up Shenandoah National Park today.
Professor Christopher 'Chuck' M. Bailey, Chair of the Department of Geology at William & Mary and President of the Geological Society of Americatakes us on a storied tour of the awe-inspiring history of the land we now know as Shenandoah National Park, told by its geological features. Learn about the stones that you pass on your favorite hike in the park, and what they reveal about the history and landscape!

Пікірлер: 3
@valoriel4464
@valoriel4464 24 күн бұрын
Excellent talk. Learned so much. The green rocks fascinated me. Lovely to hear their history. Thx from Blue Ridge near Asheville NC. ✌🏻
@SNPTrust
@SNPTrust 21 күн бұрын
So glad you found the video! Dr. Bailey is certainly an expert in the field :)
@AvanaVana
@AvanaVana 3 ай бұрын
Great talk, particularly because in this talk the speaker combats the long-standing fiction promulgated by countless GEO101 and K-12 earth science textbooks that the Appalachian Mountains are “the oldest mountains in the world”. This fiction is has been widely disseminated across a huge section of the general population. Very few people understand that, while the rocks that form the mountains are rather old, the mountains themselves-the relief/landforms/geomorphic surface-is Miocene age and younger, and the original mountains formed during the Paleozoic continental collision-the series of orogenies that culminated in the formation of Pangaea-would have been peneplained down to hydrological equilibrium level just tens of millions of years after they were first uplifted. It’s also probable that some form of “Appalachian” mountains appeared concomitant with the formation of the Atlantic Ocean, as “Rift Shoulders”, or tilted block uplifts associated with the formation of the Triassic to Jurassic extensional basins that developed during early rifting of the Atlantic margin, but these, too, would have been eroded down to nothing for most of remaining Mesozoic and Cenozoic time. It is, however, unknown if during this time, some sort of long-lived “high-relief” geomorphic surface like that which we see today in the Appalachians-primarily caused by differential erosion, as the speaker points out-could have existed, making the mountain range a very long-lived erosional feature. My understanding, however, is that the Atlantic margin was more or less a region of low relief until Miocene time, and the appearance of high relief occurs with a global change in climatic patterns (cooling and development of the Jet Stream), and that most of the relief we observe occurred in focused pulses, first in Miocene time, and then in Pleistocene time, with the glaciation of the Northern Hemisphere. The late great Peter Molnar talked about this-the occurrence of young (
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