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The islands were also previously known as the Enchanted Isles or Islands (Islas Encantadas) from sailors' difficulty with the winds and currents around them; [7] as the Ecuador Archipelago (Archipiélago de Ecuador) or Archipelago of the Equator (Archipiélago del Ecuador) following their settlement by Ecuador in 1832; [8] and as the Colon or ...
The Philippines is an archipelago that comprises 7,641 islands, [8] and with a total land area of 300,000 square kilometers (115,831 sq mi), it is the world's fifth largest island country. [ 2 ] [ 3 ] [ 9 ] The eleven largest islands contain 95% of the total land area.
Daphne Major is a volcanic island just north of Santa Cruz Island and just west of the Baltra Airport in the Archipelago of Colón, commonly known as the Galápagos Islands. [1] [2] It consists of a tuff crater, devoid of trees, whose rim rises 120 m (394 ft) above the sea.
Download QR code; Print/export ... Major geographic features of the Philippines. 1. Batanes group of islands: 2. Babuyan group of islands: 3.
Rising from the sea floor, the volcanic islands of the Galapagos are set on top of a large submarine platform. The main portion of the Galapagos platform is relatively flat and less than 1000 meters in depth. The steepest slopes are found along the western and southern flanks of the platform with a gradual slope towards the east.
Santiago Island is one of the islands in the Galapagos Archipelago. [5] It was formed from a shield volcano eponymously named Santiago. [6] The oldest lava flows on the island date back to 750,000 years ago. [7] The low, flat summits of the volcano allowed the low-viscosity lava to flow for large distances from the source vents. [8]
Isabela Island (Spanish: Isla Isabela) is the largest of the Galápagos Islands, with an area of 4,586 km 2 (1,771 sq mi) and a length of 100 km (62 mi). By itself, it is larger than all the other islands in the chain combined, and it has a little under 2,000 permanent inhabitants. The island straddles the equator.
The Galápagos triple junction (GTJ) is a geological area in the eastern Pacific Ocean several hundred miles west of the Galápagos Islands where three tectonic plates – the Cocos plate, the Nazca plate, and the Pacific plate – meet. It is an unusual type of triple junction in which the three plates do not meet at a simple intersection.