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Massachusetts
Seismic Data and Operations

Massachusetts Seismic Data and Operations

Category:

Oil Gas and Minerals - Agreements

State:

Multi-State

Control #:

US-OG-720

Format:

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

The Northern Appalachians Seismic Zone is an active seismic zone in the Appalachian Mountains of eastern North America, extending from New Brunswick southwards into New England and Boston.

Massachusetts is composed largely of large terranes, but is also grouped into various belts and fault zones by structural geologists. Other major faults and features from west to east: Eastern Border Fault, an inactive Mesozoic rift, formed the Connecticut River Valley and runs along the eastern side of it.

The Massachusetts State Building Code consists of a series of international model codes and any state-specific amendments adopted by the Board of Building Regulations and Standards (BBRS).

Rhode Island and Southeastern Massachusetts fall nearly in the center of the North American Plate, one of 15 (seven primary, eight secondary) that cover the Earth.

New England sits on a spiderweb of faults, ing to the USGS. But faults in Massachusetts are small compared to those in western states like California, meaning the likelihood of a devastating quake is slim. The state's biggest recorded earthquake happened more than 250 years ago, off the coast of Cape Ann in 1755.

In Central Massachusetts, the most pronounced fault is the Clinton-Newbury fault, created 250 million to 450 million years ago. It runs 97 miles from Worcester to Newbury through Lake Quinsigamond and the Acre section of Clinton.

For example, the City of Boston is situated on both bedrock and filled land, so an earthquake would affect these areas differently. The areas of filled land would be expected to experience stronger ground shaking and the potential for damage.

Ing to Mass.gov, "Massachusetts is located in a moderate earthquake zone." The site says, "Although these quakes typically cause only insignificant or mild damage, larger earthquakes are possible and could cause serious damage to buildings and infrastructure."

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