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Due to this, the number of continents varies; up to seven or as few as four geographical regions are commonly regarded as continents. Most English-speaking countries recognize seven regions as continents. In order from largest to smallest in area, these seven regions are Asia, Africa, North America, South America, Antarctica, Europe, and Australia.
Transcontinental country in Europe and Asia, classified as an Eastern European country by the United Nations Statistics Division: Russia ( North Asia ). States mostly or entirely in West Asia, but commonly associated with Europe, and a member of the Council of Europe: Armenia, Azerbaijan, Cyprus, Georgia, and Turkey.
The Seven Summits consist of the highest mountain peak on each of the continents. Different lists include slight variations, but generally, the same core is maintained. The seven summits depend on the definition used for a continent – in particular the location of the border of that continent. This results in two major points of variation.
Chronology of continents. A continent is a large geographical region defined by the continental shelves and the cultures on the continent. [1] In the modern day, there are seven continents. However, there have been more continents throughout history. Vaalbara was the first supercontinent. [2] Europe is the newest continent. [3]
Population ranking of the world's continents and continental subregions. This is a list of continents and continental subregions by population . World population by continent, 2021. Asia (59.4%) Africa (17.6%) Europe (9.4%) North America (7.5%) South America (5.5%) Oceania (0.6%)
This 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 ...
Formed from three cratonic fragments - the Baltic Shield, Sarmatia and Volgo–Uralia. Formed part of Columbia, then Rodinia and Pannotia. Collided with Laurentia and Avalonia to form Laurussia. [1] [4] [2] [10] Cathaysia. 1800. Continent. Fused with the Yangtze block to form the South China Craton during the Early Paleozoic.
A supercontinent cycle is the break-up of one supercontinent and the development of another, which takes place on a global scale. [4] Supercontinent cycles are not the same as the Wilson cycle, which is the opening and closing of an individual oceanic basin. The Wilson cycle rarely synchronizes with the timing of a supercontinent cycle. [1]