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Cocos Island (Chamorro: Islan Dåno) is an island 1 mile (1.6 km) off the southern tip of the United States territory of Guam, located within the Merizo Barrier Reef, part of the municipality of Malesso'.
A map showing the Neolithic Austronesian migrations into the islands of the Indo-Pacific. Guam, along with the other Mariana Islands, were the first islands settled by humans in Remote Oceania.
A population density map of Guam, 2000. A 1668 description reported that there were approximately 180 Chamoru villages on Guam with a total island population between 35,000 and 50,000. [12] The Spanish strategy of villagization, called reducción, which began in the Spanish-Chamorro Wars, transferred the population to seven towns.
Map showing the four municipalities of the Northern Mariana Islands, with Guam shown for context and indicating which islands have airports. Administratively, the CNMI is divided into four municipalities: The Northern Islands (north of Saipan) form the Northern Islands Municipality.
The islands are part of a geologic structure known as the Izu–Bonin–Mariana Arc system, and range in age from 5 million years old in the north to 30 million years old in the south (Guam). The island chain arose as a result of the western edge of the Pacific Plate moving westward and plunging downward below the Mariana plate, a region which ...
Many villages have rich histories reaching back thousands of years. Artifacts from ancient Chamorro settlements can be found in every village of Guam. When the Spanish Empire colonized the Marianas Islands as part of its Pacific possessions in the 16th and 17th centuries, the island was divided into separate districts with each district consisting of a parish with a village center governed by ...
Malesso' (formerly Merizo) is the southernmost village in the United States territory of Guam. Cocos Island (Chamorro: Islan Dåno) is a part of the municipality. The village's population has decreased since the island's 2010 census. [1] Malesso' is the closest populated place in the United States to the equator.
Geologic map of Guam. 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.