Ohio Seismic Data and Operations

State:
Multi-State
Control #:
US-OG-720
Format:
Word; 
Rich Text
Instant download

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

Geologists have identified a couple fault lines that run across our southern viewing area, including the Anna-Champaign fault, and the Auglaize fault that does run into southern Allen county. These faults are associated with an ancient 500 foot deep rift zone that runs through this area.

The easiest way is to find out?? if a property is located in a Seismic Hazard Zone is to use the California Earthquake Hazards Zone Application?? or search our collection of online maps. You can also visit one of the California Geological Survey offices? (call ahead), or your city or county office.

The ODNR Division of Geological Survey coordinates a 21-station network (see attached map) of seismograph stations throughout the state in order to continuously record earthquake activity.

The largest historic earthquake in the state occurred in 1937. This event had an estimated magnitude of 5.4 and caused considerable damage in the town of Anna and in several other western Ohio communities. The large map shows all historical and instrumentally located earthquakes from 1776 through 2007.

Seismometers allow us to detect and measure earthquakes by converting vibrations due to seismic waves into electrical signals, which we can then display as seismograms on a computer screen. Seismologists study earthquakes and can use this data to determine where and how big a particular earthquake is.

Ohio is on the periphery of the New Madrid Seismic Zone, an area in Missouri and adjacent states that was the site of the largest earthquake sequence to occur in historical times in the continental United States. Four great earthquakes were part of a series at New Madrid in 1811 and 1812.

There are four zones, with Zone 1 being the least threatened by seismic activity, and Zone 4 being the most threatened (ie. areas near an active fault line).

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Ohio Seismic Data and Operations