Diese Statistik zeigt die Flächen der Kontinente. Der größte Kontinent ist Asien mit einer Fläche von rund 44 Millionen Quadratkilometer. Durch Bewegung unseres Planeten begann der Ur-Kontinent vor Millionen Jahren zu zerbrechen. Heute sprechen wir von sieben Kontinenten, die teilweise. Category:DE:Kontinente auf der Erde. Language; Watch · Edit · Purge · Help. Category:Continents on Earth - Other languages. Afrikaans.
Die 7 KontinenteSieben Kontinente gliedern die heutige Weltkarte. "Terra X" stellt alle Erdteile und ihre einzigartige Tier- und Pflanzenwelt vor. Wie hat sich das Leben den. Kontinente werden per Definition als durch Ozeane getrennte Festlandmasse bezeichnet. Parallel dazu wird die bevölkerte Welt in meist fünf Erdteile eingeteilt:. Modelle von Definition der Kontinente belegen, denn die die Mikrokontinente – vier bis sieben Kontinente gezählt.
Kontinente Wiki Navigační menu VideoMga Kontinente sa Daigdig Modelle von Definition der Kontinente belegen, denn die die Mikrokontinente – vier bis sieben Kontinente gezählt. kontinente ist eine Zeitschrift, die von 24 weltweit tätigen katholischen Ordensgemeinschaften, dem Internationalen Katholischen Missionswerk missio Aachen. Die meisten Kontinente sind durch Ozeane klar voneinander getrennt. Das Klexikon ist wie eine Wikipedia für Kinder und Schüler. Kontinente sind oftmals von Ozeanen getrennt, können aber auch durch größere Gebirgszüge getrennt sein. Die Erde besitzt sieben Kontinente, welche vom.
Other islands such as Great Britain were joined to the mainlands of their continents. There are several ways of distinguishing the continents:.
As previously mentioned, some geographers use the name Oceania for a region including most of the island countries and territories in the Pacific Ocean as well as the continent of Australia.
The following table summarizes the area and population of the continental regions used by the United Nations.
Apart from the current continents, the scope and meaning of the term continent includes past geological ones.
Supercontinents , largely in evidence earlier in the geological record, are landmasses that comprise more than one craton or continental core.
Over time, these supercontinents broke apart into large land masses which formed the present continents. Certain parts of continents are recognized as subcontinents, especially the large peninsulas separated from the main continental landmass by geographical features.
The most notable examples are the Indian subcontinent and the Arabian Peninsula. In many of these cases, the "subcontinents" concerned are on different tectonic plates from the rest of the continent, providing a geological justification for the terminology.
Where the Americas are viewed as a single continent America , it is divided into two subcontinents North America and South America    or three with Central America being the third.
Some areas of continental crust are largely covered by the sea and may be considered submerged continents. Notable examples are Zealandia , emerging from the sea primarily in New Zealand and New Caledonia , and the almost completely submerged Kerguelen Plateau in the southern Indian Ocean.
Some islands lie on sections of continental crust that have rifted and drifted apart from a main continental landmass.
While not considered continents because of their relatively small size, they may be considered microcontinents. Madagascar , the largest example, is usually considered an island of Africa, but its divergent evolution has caused it to be referred to as "the eighth continent" from a biological perspective.
The Biodiversity Information Standards organization has developed the World Geographical Scheme for Recording Plant Distributions , used in many international plant databases.
This scheme divides the world into nine "botanical continents", some match the traditional geographical continents, but some differ significantly.
Asia Minor ,  The first distinction between continents was made by ancient Greek mariners who gave the names Europe and Asia to the lands on either side of the waterways of the Aegean Sea , the Dardanelles strait, the Sea of Marmara , the Bosporus strait and the Black Sea.
Ancient Greek thinkers subsequently debated whether Africa then called Libya should be considered part of Asia or a third part of the world.
Division into three parts eventually came to predominate. Herodotus  in the 5th century BC objected to the whole of Egypt being split between Asia and Africa "Libya" and took the boundary to lie along the western border of Egypt, regarding Egypt as part of Asia.
He also questioned the division into three of what is really a single landmass,  a debate that continues nearly two and a half millennia later.
Eratosthenes , in the 3rd century BC, noted that some geographers divided the continents by rivers the Nile and the Don , thus considering them "islands".
Others divided the continents by isthmuses , calling the continents "peninsulas". These latter geographers set the border between Europe and Asia at the isthmus between the Black Sea and the Caspian Sea , and the border between Asia and Africa at the isthmus between the Red Sea and the mouth of Lake Bardawil on the Mediterranean Sea.
Through the Roman period and the Middle Ages , a few writers took the Isthmus of Suez as the boundary between Asia and Africa, but most writers continued to consider it the Nile or the western border of Egypt Gibbon [ citation needed ].
In the Middle Ages, the world was usually portrayed on T and O maps , with the T representing the waters dividing the three continents.
By the middle of the 18th century, "the fashion of dividing Asia and Africa at the Nile, or at the Great Catabathmus [the boundary between Egypt and Libya ] farther west, had even then scarcely passed away".
Christopher Columbus sailed across the Atlantic Ocean to the West Indies in , sparking a period of European exploration of the Americas.
But despite four voyages to the Americas, Columbus never believed he had reached a new continent—he always thought it was part of Asia.
After reaching the coast of Brazil , they sailed a long way farther south along the coast of South America , confirming that this was a land of continental proportions and that it also extended much farther south than Asia was known to.
Within a few years, the name "New World" began appearing as a name for South America on world maps, such as the Oliveriana Pesaro map of around — Maps of this time though, still showed North America connected to Asia and showed South America as a separate land.
In Martin Waldseemüller published a world map, Universalis Cosmographia , which was the first to show North and South America as separate from Asia and surrounded by water.
A small inset map above the main map explicitly showed for the first time the Americas being east of Asia and separated from Asia by an ocean, as opposed to just placing the Americas on the left end of the map and Asia on the right end.
In the accompanying book Cosmographiae Introductio , Waldseemüller noted that the earth is divided into four parts, Europe, Asia, Africa and the fourth part, which he named "America" after Amerigo Vespucci's first name.
From the 16th century the English noun continent was derived from the term continent land , meaning continuous or connected land  and translated from the Latin terra continens.
While continent was used on the one hand for relatively small areas of continuous land, on the other hand geographers again raised Herodotus's query about why a single large landmass should be divided into separate continents.
Thus Europe, Asia, and Africa is one great continent, as America is another. From the late 18th century, some geographers started to regard North America and South America as two parts of the world, making five parts in total.
Overall though, the fourfold division prevailed well into the 19th century. Europeans discovered Australia in , but for some time it was taken as part of Asia.
By the late 18th century, some geographers considered it a continent in its own right, making it the sixth or fifth for those still taking America as a single continent.
Antarctica was sighted in during the First Russian Antarctic Expedition and described as a continent by Charles Wilkes on the United States Exploring Expedition in , the last continent identified, although a great "Antarctic" antipodean landmass had been anticipated for millennia.
From the midth century, atlases published in the United States more commonly treated North and South America as separate continents, while atlases published in Europe usually considered them one continent.
However, it was still not uncommon for American atlases to treat them as one continent up until World War II.
Some geographers regard Europe and Asia together as a single continent, dubbed Eurasia. Geologists use the term continent in a different manner from geographers.
In geology, a continent is defined by continental crust, which is a platform of metamorphic and igneous rock , largely of granitic composition.
Continental crust is less dense and much thicker than oceanic crust, which causes it to "float" higher than oceanic crust on the dense underlying mantle.
This explains why the continents form high platforms surrounded by deep ocean basins. Some geologists restrict the term 'continent' to portions of the crust built around stable regions called cratons.
Cratons have largely been unaffected by mountain-building events orogenies since the Precambrian. A craton typically consists of a continental shield surrounded by a continental platform.
The shield is a region where ancient crystalline basement rock typically 1. The platform surrounding the shield is also composed of ancient basement rock, but with a cover of younger sedimentary rock.
This accounts for the great age of the rocks comprising the continental cratons. The margins of geologic continents are characterized by currently active or relatively recently active mobile belts and deep troughs of accumulated marine or deltaic sediments.
Beyond the margin, there is either a continental shelf and drop off to the basaltic ocean basin or the margin of another continent, depending on the current plate-tectonic setting of the continent.
A continental boundary does not have to be a body of water. By this definition, Eastern Europe, India and some other regions could be regarded as continental masses distinct from the rest of Eurasia because they have separate ancient shield areas i.
East European craton and Indian craton. Younger mobile belts such as the Ural Mountains and Himalayas mark the boundaries between these regions and the rest of Eurasia.
Plate tectonics provides yet another way of defining continents. Today, Europe and most of Asia constitute the unified Eurasian Plate , which is approximately coincident with the geographic Eurasian continent excluding India, Arabia, and far eastern Russia.
India contains a central shield, and the geologically recent Himalaya mobile belt forms its northern margin. North America and South America are separate continents, the connecting isthmus being largely the result of volcanism from relatively recent subduction tectonics.
North American continental rocks extend to Greenland a portion of the Canadian Shield , and in terms of plate boundaries, the North American plate includes the easternmost portion of the Asian landmass.
Geologists do not use these facts to suggest that eastern Asia is part of the North American continent, even though the plate boundary extends there; the word continent is usually used in its geographic sense and additional definitions "continental rocks," "plate boundaries" are used as appropriate.
Over geologic time, continents are periodically submerged under large epicontinental seas, and continental collisions result in a continent becoming attached to another continent.
The current geologic era is relatively anomalous in that so much of the continental areas are "high and dry"; that is, many parts of the continents that were once below sea level are now elevated well above it due to changes in sea levels and the subsequent uplifting of those continental areas from tectonic activity.
Das bedeutet eine Unterteilung in die sieben genannten Kontinente, erweitert um sieben Mikrokontinente. Letzteres spiegelt auch die zunehmende Erforschung der Tektonik von Mikroplatten wider.
Superkontinent mit Subkontinenten handelt. Geologisch umfasst ein Kontinent auch das ihm zugehörige Schelfgebiet , also den Festlandssockel im Flachmeer.
Neben diesen beiden gibt es auch eine historisch-politische Dimension. Beleg hierfür ist die Tatsache, dass Europa als eigener Erdteil gilt, obwohl dies keiner der genannten geografischen oder technischen Definitionen entspricht.
So stabil uns die heutige Verteilung der Landmassen auf der Erde auch erscheinen mag, so stellt sie erdgeschichtlich nur eine Momentaufnahme dar.
Anhand der o. Einige wenige Quellen   sind der Meinung wie bereits in der Unterrichtshilfe der Royal Geographic beschrieben , dass Ozeanien anstelle von Australien der korrekte Name dieses pazifischen Erdteils ist.
Zudem wurde der Begriff Doppelkontinent seit dem ausgehenden Jahrhundert für verschiedene geologische Landmassen genutzt — darunter Eurasien Europa und Asien  und Amerika Nord- und Südamerika  — und wird auch heute teilweise noch in primär geographischen und historischen Publikationen verwendet.
Magkakonekta rin ang mga kontinente ng Apro-Eurasya at Kaamerikahan sa tulong ng tulay na lupa ng Bering. Konektado rin ang iba pang mga isla noong panahon na iyon tulad ng Pilipinas at Gran Britanya sa pangunahing kalupaan ng mga kontinente.
Noon din panahong iyon, may tatlo lamang na kontinenteng magkakahiwalay at magkakaiba: ang kontinente ng Apro-Eurasya-Amerika, Antartika, at Awstralya-Bagong Ginea.
Ang lathalaing ito na tungkol sa Heograpiya ay isang usbong. Makatutulong ka sa Wikipedia sa pagpapalawig nito. Mula sa Wikipedia, ang malayang ensiklopedya.
Mga nilalaman. Nakuha noong Oktubre 16, National Geographic. Tinago mula sa orihinal noong Hunyo 29, Most people recognize seven continents—Asia, Africa, North America, South America, Antarctica, Europe, and Australia, from largest to smallest—although sometimes Asia and Europe are considered a single continent, Eurasia.
Kilala ng karamihan ang pitong kontinente— Asya, Aprika, Hilagang Amerika, Timog Amerika, Antartika, Europa, at Awstralya, pinakamalaki papaliit— kahit na paminsan-minsan, tinuturing bilang iisang kontinente ang Asya at Europa, ang Eurasya.
Nakuha noong Oktubre 7, UN Oceans Atlas sa wikang Ingles. Tinago mula sa orihinal noong Mayo 31, Oxford English Dictionary sa wikang Ingles ika-2 na edisyon.
Oxford University Press. Dagiti nakasilpo ditoy Mainaig a sinuksukatan Agikarga iti papeles Espesial a pampanid Agnanayon a silpo Pakaammo ti panid Dakamaten daytoy a panid Datos ti Wikidata.
Wikimedia Commons. Daytoy nga artikulo dagiti nangruna nga artikulo ket pungol. Makatulongka iti Wikipedia babaen ti panagnayon iti daytoy. Dagiti Heolohiko a nalatak a kontinente.
Dagiti naipakasaritaan a kontinente. Dagiti Limned a kontinente. Mabalina a masakbayan nalatak a kontinente. Dagiti Mitiko ken teoretikal a kontinente.