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Recommended for: Grades 6-12

Resource: Plate Tectonics: Lake Mead, Nevada

Plate Tectonics: Lake Mead, Nevada Save to a folder

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Media Type:
QuickTime Video

Length: 2m 13s
Size: 3.1 MB

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Contrary to what most geologists thought less than 100 years ago, we live on a dynamic planet. Earth's surface has changed in countless ways during the 4.6 billion years since it formed, and it continues to change today. This video segment adapted from Discovering Women looks at some of the geologic processes that have shaped the landscape near Lake Mead, Nevada, and suggests that these processes may be causing North America to slowly break apart.

 

Teachers' Domain, Plate Tectonics: Lake Mead, Nevada, published October 21, 2005, retrieved on ,
http://www.teachersdomain.org/resource/ess05.sci.ess.earthsys.meadnv/

 

Features on the surface of Earth provide evidence of past events as well as ongoing processes in our planet's geologic history. Sometimes the ongoing processes uncover evidence of events in the more distant past. For example, as the Colorado River carved out the Grand Canyon, it uncovered 400-million-year-old rocks and exposed evidence of ocean advances and retreats, as well as the history of plant and animal evolution during that time. However, ongoing processes may also destroy evidence of past events, eroding or otherwise transforming geological features and making the task of unraveling geologic history a difficult one.

Like countless regions of the world, the area surrounding Lake Mead, Nevada, has been the scene of a multitude of geologic events. For example, there is evidence that about 2 billion years ago this area formed the western coast of North America. Subsequently, the continent collided with and connected to a volcanic island chain, was flooded several times by inland seas, experienced numerous periods of uplift and erosion, and joined with other continents to form Pangaea, before breaking apart again.

Despite all these events, the geological events of the past 18 million years are the ones that have most clearly defined the region. During this time, movement of Earth's tectonic plates caused explosive volcanic eruptions. At times, this activity blanketed the area with ash, debris, and lava flows. The movement of tectonic plates also stretched the continental crust, causing fault lines to open and the land to break into tipped block formations with high peaks and low valleys. What's more, scientific evidence suggests that this area of stretched crust, called a rift zone, continues to pull apart today. If so, the area around Lake Mead, a human-made reservoir, may one day be the site of a natural inland sea and the boundary between two diverging continents.

To learn more about how the movement of tectonic plates creates rift valleys, check out Plate Tectonics: An Introduction.

To learn more about the rich geologic history of America's Southwest, check out The Grand Canyon: How It Formed.

To see where Earth's many tectonic plates are diverging and converging, check out Tectonic Plates and Plate Boundaries.

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Source: Discovering Women: "Earth Explorer"

Resource Produced by:

WGBH Educational Foundation

Collection Developed by:

WGBH Educational Foundation

Collection Credits

Collection Funded by:

National Science Foundation