Re: Earthquakes
From University of Oklahoma
Oklahoma Geology: Why Do We Have Earthquakes?
Background: Oklahoma Geology
Although much of Oklahoma belongs to the stable central plains province of the United States, it has been involved in major mounting building and basin forming processes in the past few hundred years. This may help to explain why Oklahoma, although not experiencing major earthquakes activity, nevertheless has a sustained level of seismicity.
Major geological provinces in Oklahoma include 4 mountain ranges or uplifts (Ozark Uplift, Wichita Uplift, Arbuckle Uplift and Ouachita Mountains), 5 basins (Anadarko Basin, Arkoma Basin, Ardmore Basin, Marietta Basin and Hollis Basin), and the Northern Shelf Area. In the far western panhandle is Black Mesa. The Nemaha Ridge runs approximately north-south through north central and central Oklahoma. The Gulf Coastal Plain, consisting of young sedimentary rocks, covers the most southeasterly part of the state.
" You've Been Thunder Struck ! "
Bookmarks