New Jersey 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

Earthquakes felt in New Jersey are generally few and small. However, some earthquakes have produced damage in New Jersey. New Jersey's seismic hazard is lower than many earthquake-prone parts of the United States. Across the state, seismic hazards are highest in northeastern New Jersey.

A view of the city of Yonkers, in New York state, where residents felt an earthquake early morning on . A magnitude 2.2 earthquake was felt in parts of New York and New Jersey early Friday morning, the U.S. Geological Survey told CNN.

Since historic times New Jersey had occasional small earthquake, most of which have been located in the northern part of the state.

New Jersey is in an area where the rarer plate interior-related earthquakes occur. As plates continue to move and plate boundaries change geologically over time, weakened boundary regions become part of the interiors of the plates.

The most recent quake occurred just before a.m. on December 3, 2020 ? a 2.51-magnitude event centered in Milford.

The time?spans between the intensity VII earthquakes were 46 and 101 years. This, and data for the smaller?intensity quakes, imply a return period of 100 years or less, and suggests that New Jersey is overdue for a moderate earthquake like the one of 1884.

Earthquake epicenters in eastern North America and the New Jersey area, however, do not typically occur on known faults. The faults in these areas are the result of tectonic activity from over 200 million years ago. Many faults can be located in New Jersey and in parts of Sussex County.

Although there are many faults in New Jersey, the Ramapo Fault, which separates the Piedmont and Highlands Physiographic Provinces, is the best known (see last figure).

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New Jersey Seismic Data and Operations