cratons of the world - EAS
Vaalbara - Wikipedia
https://en.wikipedia.org/wiki/VaalbaraWebVaalbara was an Archean supercontinent consisting of the Kaapvaal Craton (now in eastern South Africa) and the Pilbara Craton (now in north-western Western Australia).E. S. Cheney derived the name from the last four letters of each craton's name. The two cratons consist of crust dating from 2.7 to 3.6 Gya, which would make Vaalbara one of Earth's earliest …
Continent | National Geographic Society
https://www.nationalgeographic.org/encyclopedia/ContinentWebJul 27, 2022 · Even older than these ancient, eroded mountain ranges are flatter, more stable areas of the continents called cratons. A craton is an area of ancient crust that formed during Earth’s early history. Every continent has a craton. Microcontinents, like New Zealand, lack cratons. Cratons have two forms: shields and platforms.
Diamond - Wikipedia
https://en.wikipedia.org/wiki/DiamondWebDiamond is a solid form of pure carbon with its atoms arranged in a crystal. Solid carbon comes in different forms known as allotropes depending on the type of chemical bond. The two most common allotropes of pure carbon are diamond and graphite.In graphite the bonds are sp 2 orbital hybrids and the atoms form in planes, with each bound to three …
Crust | National Geographic Society
https://www.nationalgeographic.org/encyclopedia/crustWebJul 15, 2022 · “Crust ” describes the outermost shell of a terrestrial planet. Our planet ’s thin, 40-kilometer (25-mile) deep crust—just 1% of Earth ’s mass—contains all known life in the universe. Earth has three layers: the crust, the mantle, and the core.The crust is made of solid rocks and minerals.Beneath the crust is the mantle, which is also mostly solid rocks …
List of tectonic plates - Wikipedia
https://en.wikipedia.org/wiki/List_of_tectonic_platesWebThis is a list of tectonic plates on Earth's surface. Tectonic plates are pieces of Earth's crust and uppermost mantle, together referred to as the lithosphere.The plates are around 100 km (62 mi) thick and consist of two principal types of material: oceanic crust (also called sima from silicon and magnesium) and continental crust (sial from silicon and aluminium).
Craton - Wikipedia
https://en.wikipedia.org/wiki/CratonWebA craton (/ ˈ k r eɪ t ɒ n /, / ˈ k r æ t ɒ n /, or / ˈ k r eɪ t ən /; from Greek: κράτος kratos "strength") is an old and stable part of the continental lithosphere, which consists of Earth's two topmost layers, the crust and the uppermost mantle.Having often survived cycles of merging and rifting of continents, cratons are generally found in the interiors of tectonic …
Geography of India - Wikipedia
https://en.wikipedia.org/wiki/Geography_of_IndiaWebIndia is situated north of the equator between 8°4' north (the mainland) to 37°6' north latitude and 68°7' east to 97°25' east longitude. It is the seventh-largest country in the world, with a total area of 3,287,263 square kilometres (1,269,219 sq mi).. On the south, India projects into and is bounded by the Indian Ocean—in particular, by the Arabian Sea on the west, …
Asia - West Asia | Britannica
https://www.britannica.com/place/Asia/West-AsiaWebAsia’s indigenous vegetation has provided many of the world’s food crops—including most of the cereal grains, oilseeds, fruits, and vegetables—and its lands provided one of the great cradles of agriculture. Three primary centres for the domestication of those plants have been postulated. One was in the southwest, consisting of sites in the Levant and northern …
Craton — Wikipédia
https://fr.wikipedia.org/wiki/CratonWebUn craton (du grec κράτος, kratos : force), appelé aussi aire continentale, est une vaste portion stable du domaine continental par opposition aux zones instables déformées (les orogènes).Il forme un élément de lithosphère continentale possédant une identité géologique, notamment en termes de nature des roches et de structuration des unités …
Hoggar Mountains - Wikipedia
https://en.wikipedia.org/wiki/Hoggar_MountainsWebThis mountainous region is located about 1,500 km (930 mi) south of the capital, Algiers.The area is largely rocky desert with an average elevation of more than 900 m (3,000 ft) above sea level. The highest peak, Mount Tahat, is at 2,908 m (9,541 ft). The mountains are primarily composed of metamorphic rock approximately 2 billion years old, although there …

