This lease rider form may be used when you are involved in a lease transaction, and have made the decision to utilize the form of Oil and Gas Lease presented to you by the Lessee, and you want to include additional provisions to that Lease form to address specific concerns you may have, or place limitations on the rights granted the Lessee in the “standard” lease form.
Virgin Islands Geophysical and Seismic Operations
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State:
Multi-State
Control #:
US-OG-800
Format:
Word;
Rich Text
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FAQ
Earthquakes occur regularly in the Virgin Islands. The eastward shifting Caribbean plate grinds against the westward moving North American plate, just north of the Virgin Islands along the Puerto Rican Trench. Generally, the quakes are too small for people to notice, and they do not cause tsunamis.
The U.S.Virgin Islands are part of the Greater Antilles that lies parallel to the Puerto Rico Trench; an oblique subduction zone where the North American Plate is underthrusted beneath the Caribbean Plate along the Lesser Antilles subduction zone transits to strike-slip along the Septentrional-Oriente fault zone.
The continental segment of the North American?Caribbean plate boundary is expressed as the Motagua?Polochic fault system (Fig. 3). This sinistral fault system is made up of two dominant faults, the Motagua fault in the southeast and the Polochic fault in the northwest of the fault zone.
Puerto Rico and the Virgin Islands are located at an active plate boundary between the North American plate and the northeast corner of the Caribbean plate. Plate movements have caused large magnitude earthquakes and devastating tsunamis.
Although tsunamis are infrequent in the USVI, several active tectonic sources capable of producing powerful tsunamis lie in close proximity to the Territory. The location of the source relative to the Territory is important for understanding how quickly waves will arrive onshore and the impacts they will have.
A long process of undersea mountain building and uplift brought submarine ridges and peaks to the surface. This was followed by periods of explosive volcanism, alternated with periods of coral reef deposits, changing sea levels and future intrusion, creating the island we call St. John today.
The geology of the U.S. Virgin Islands includes mafic volcanic rocks, with complex mineralogy that first began to erupt in the Mesozoic overlain and interspersed with carbonate and conglomerate units.
Puerto Rico and the Virgin Islands are located at an active plate boundary between the North American plate and the northeast corner of the Caribbean plate. Plate movements have caused large magnitude earthquakes and devastating tsunamis.