Maryland 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

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.

A seismometer is the internal part of the seismograph, which may be a pendulum or a mass mounted on a spring; however, it is often used synonymously with "seismograph". Seismographs are instruments used to record the motion of the ground during an earthquake.

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.

A seismogram is a record of the ground motions caused by seismic waves from an earthquake. A seismograph or seismometer is the measuring instrument that creates the seismogram.

Unusual animal behavior: Animals may act strangely or become agitated before an earthquake. Small tremors or foreshocks: These are smaller earthquakes that can occur before a larger earthquake. Ground uplift or subsidence: Changes in the ground level can be a sign of stress building up along fault lines.

The mid-Atlantic and central Appalachian region, including Maryland, is characterized by a moderate amount of low-level earthquake activity, but their cause or causes are largely a matter of speculation. In Maryland, for example, there are numerous faults, but none is known or suspected to be active.

The 2011 earthquake was one of the strongest earthquakes to be felt in Maryland. At p.m. on Aug. 23, 2011, a 5.8 magnitude earthquake hit about 38 miles northwest of Richmond, Virginia, and was felt across more than a dozen states.

Seismic waves lose much of their energy in traveling over great distances. But sensitive detectors (seismometers) can record theses waves emitted by even the smallest earthquakes. When these detectors are connected to a system that produces a permanent recording, they are called seismographs.

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Maryland Seismic Data and Operations