This form provides that any Party may propose that geoscience operations be conducted on the Contract Area lands. The Party wishing to conduct geoscience operations shall furnish the other Parties with an information notice which generally describes the proposed geoscience operation.
Guam Geoscience Operations on the Contract Area
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Multi-State
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US-OG-705
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FAQ
Guam is a large volcanic base which has been repeatedly elevated, on which coral limestone has repeatedly formed. The entire northern half is a shelving, more or less flat, plateau of metamorphosed coral limestone, a terrace atop a submerged volcanic base.
The central and northern parts of the island are composed of limestone with Mount Santa Rosa and Mount Mataguac having several volcanic formations. The southern part is volcanic with elongated mountain ridges, which divide the inland valleys and coastlines.
The island is sharply divided into a northern limestone plateau with a general elevation of about 500 feet (150 metres) and a higher area of volcanic hills to the south. The plateau is covered with a thick growth of jungle, while the volcanic hills support mainly sword grass.
The foundation of the island of Guam is volcanic rock that is covered in limestone over approximately 60% of its surface. The volcanic rock has low permeability due to its texture and poor sorting, while the limestone tends to be highly permeable due to its high porosity (Gingerich 2003).
Guam is the largest island in Micronesia and is the southernmost of the Mariana Islands. The northern half of Guam is composed of a relatively flat coralline limestone plateau about 260 m above sea level, whereas the southern part is mountainous volcanic terrain with elevations up to 406 m (Mount Lamlam).
The southern lava volcano merged with the older northern one, leaving only their twin peaks above sea level forming the island we now know as Guam. The island is 212 square miles--30 miles in length and 8.5 miles width in the northern tip and 11.5 miles in the south.