North Carolina Seismic Data and Operations

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Multi-State
Control #:
US-OG-720
Format:
Word; 
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Description

This form is used when the Parties agree and shall contribute all proprietary seismic data and all non-proprietary seismic data affecting the Contract Area in its possession as of the effective date of this Agreement, to the extent the data is not restricted by confidentiality or licensing agreements with third parties. It is specifically understood and agreed that each Party has the right to sell, trade, and/or otherwise market seismic data involving the Contract Area which was in its possession prior to the effective date of this Agreement, and the benefits and advantages, including monetary consideration, which it receives as a result of those activities shall be the sole property of the party who owns the data.

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FAQ

The most significant fault in the region is the Brevard fault zone, which extends from Alabama to Virginia across North Carolina, where it coincides with a long, linear topographic low.

Permanent Networks Global Seismographic Network. ... FDSN. ... Regional Networks. ... Virtual Networks at the IRIS DMC. ... PASSCAL. ... Other Sources. ... National Earthquake Information Center, World Data Center for Seismology, Denver, Colorado. ... International Seismological Centre, United Kingdom.

Ing to the United States Geological Survey (USGS), the 1960 Valdivia Earthquake, also known as the Great Chilean Earthquake, is the strongest earthquake ever recorded. It hit the Valdivia town in southern Chile on , and its magnitude was measured at 9.5.

Skyland earthquake of 1916 - the largest earthquake centered in NC.

The Brevard Fault Zone is a 700-km long and several km-wide thrust fault that extends from the North Carolina-Virginia border, runs through the north metro Atlanta area, and ends near Montgomery, Alabama. It is an important Paleozoic era feature in the uplift of the Appalachian Mountains.

The Appalachian Mountains are not on an active tectonic plate boundary?where earthquakes are common?but the region has sporadic minor quakes linked to old fault lines, geologists say.

In terms of the intensity of ground motion, four earthquakes have caused structural damage as measured on the Modified Mercalli Intensity at level VII [level 7]) -- August 31, 1861 Wilkesboro, N.C. (magnitude 5.1); August 31, 1886 Charleston, S.C. (magnitude 7.3); February 21, 1916 Asheville, NC (magnitude 5.5) and ...

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North Carolina Seismic Data and Operations