Guam 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

In addition, there are thousands of fault lines that zigzag across the island, resulting from the collision (and subduction) of the Pacific plate and the Marianas plate. A major fault line divides the island geologically between the limestone plateau of the north, and the mountainous volcanic region in the south.

Seismicity in the region is primarily controlled by active convergence between two purely oceanic tectonic plates: the Pacific plate subducts northwestward beneath the Philippine Sea plate at the Mariana trench (Karig, 1971; Karig and others, 1978; Hussong and Uyeda, 1981; Ranken and others, 1984).

The 1991 Uniform Building Code currently places Guam in seismic Zone 3.

Because it is a high island, Guam has extensive freshwater resources, and is not threatened by sea-level rise like the low atoll nations in the region. However, Guam lies directly within the typhoon belt, and is regularly hit by major storms and typhoons [9].

With the exception of the Cabras and Tamuning-Yigo faults, all the faults strike northwest. The Tamuning-Yigo fault strikes east-northeast, and the Cabras fault strikes north-northeast.

Earthquakes in Guam are infrequent but are often accompanied by tsunami. The small island, which is an unincorporated and organized territory of the United States, lies at the extreme southern end of the Mariana Islands and at the eastern margin of the Philippine Sea Plate.

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Guam Seismic Data and Operations