Guam Surface Pits

State:
Multi-State
Control #:
US-OG-827
Format:
Word; 
Rich Text
Instant download

Description

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.

How to fill out Surface Pits?

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FAQ

The Chamorro people settled Guam and the Mariana islands approximately 5,500 years ago. Portuguese explorer Ferdinand Magellan, while in the service of Spain, was the first European to visit and claim the island on March 6, 1521. Guam was fully colonized by Spain in 1668.

Volcanic rocks of southern Guam are locally overlain by limestone. The top of the mountainous ridge and central basin are covered by old limestone units. They are Miocene to Pliocene age and are known as Bonya and Alifan Limestone. Eastern coast and Orote Peninsula comprise of younger limestone.

These places are best for caverns & caves in Guam: Pagat Cave. Talofofo Falls Park. Marbo Cave.

Guam's creation story begins with two powerful gods, a brother and a sister, named Puntan and Fu'una (or Pontan and Fo'na). Long long ago, before anything else existed, Puntan and Fu'una lived. But one day, Puntan felt his spirit dying, and he looked at Fu'una and told her to use his body to create the world.

The geology of Guam formed as a result of mafic, felsic and intermediate composition volcanic rocks erupting below the ocean, building up the base of the island in the Eocene, between 33.9 and 56 million years ago. The island emerged above the water in the Eocene, although the volcanic crater collapsed.

The island is a result of the volcanic activity created by subduction of the Pacific Plate under the Philippine Sea Plate at the nearby Mariana Trench, which runs from the east of Guam to the southwest. Volcanic eruptions established the base of the island in the Eocene, roughly 56 to 33.9 million years ago (mya).

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.

Imagine the areas surrounding Guam without water--all you will see are mountains of volcanoes and a nearby crevice known as the Marianas Trench, the deepest place on earth. Geologists have stated that the island of Guam and the Marianas Islands were created millions of years ago by active volcanoes.

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Guam Surface Pits