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Kontinente Wiki

Sieben Kontinente gliedern die heutige Weltkarte. "Terra X" stellt alle Erdteile und ihre einzigartige Tier- und Pflanzenwelt vor. Wie hat sich das Leben den. 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.

Die 7 Kontinente

Durch Bewegung unseres Planeten begann der Ur-Kontinent vor Millionen Jahren zu zerbrechen. Heute sprechen wir von sieben Kontinenten, die teilweise​. Sieben Kontinente gliedern die heutige Weltkarte. "Terra X" stellt alle Erdteile und ihre einzigartige Tier- und Pflanzenwelt vor. Wie hat sich das Leben den. Diese Statistik zeigt die Flächen der Kontinente. Der größte Kontinent ist Asien mit einer Fläche von rund 44 Millionen Quadratkilometer.

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Kontinent (z latinského contineō, -ēre, což znamená držím pohromadě) je velkou souvislou pevninskou masou. Česká zeměpisná škola odděluje termíny kontinent a světadíl, který jinak bývá často považován za synonymum.. Jelikož neexistuje žádný standard pro definici kontinentu, různé kultury a vědní obory mají odlišné seznamy toho, co považují za kontinent. Br. Kontinent Površina Stanovnika 1 Azija: 44,4 mil. km² mil. 2 Afrika: 30,3 mil. km² mil. 3 Sjeverna Amerika: 24,2 mil. km² mil. 4. 3/7/ · Ang pinakamahigpit na kahulugan ng kontinente ay ang isang magkakarugtong na kalupaan o pangunahing kalupaan (mainland), kung saan binubuo ng mga baybayin at hangganang panlupa (land boundaries) ang mga gilid unequivocalnotion.com pananaw na ito, tinutukoy ng kontinental na Europa ang pangunahing kalupaan ng Europa - di kasama rito ang mga isla ng Gran Britanya, Irlanda, Malta, at Islandiya.

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Dagiti rehion iti Lubong. Kategoria : Dagiti kontinente. Nailemmeng a katkategoria: Amin a pungol nga artikulo Nangruna nga artikulo pungol.

Dagiti nagan ti espasio Artikulo Pagtungtungan. Dagiti pangkitaan Basaen Urnosen Urnosen ti taudan Kitaen ti pakasaritaan.

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.

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.

There are many microcontinents, or continental fragments , that are built of continental crust but do not contain a craton. Some of these are fragments of Gondwana or other ancient cratonic continents: Zealandia , [85] which includes New Zealand and New Caledonia ; Madagascar ; the northern Mascarene Plateau , which includes the Seychelles.

Other islands, such as several in the Caribbean Sea , are composed largely of granitic rock as well, but all continents contain both granitic and basaltic crust, and there is no clear boundary as to which islands would be considered microcontinents under such a definition.

The Kerguelen Plateau , for example, is largely volcanic, but is associated with the break-up of Gondwanaland and is considered a microcontinent, [86] [87] whereas volcanic Iceland and Hawaii are not.

The British Isles , Sri Lanka , Borneo , and Newfoundland are margins of the Laurasian continent—only separated by inland seas flooding its margins.

The movement of plates has caused the formation and break-up of continents over time, including occasional formation of a supercontinent that contains most or all of the continents.

The supercontinent Columbia or Nuna formed during a period of 2. The eight continents later re-assembled into another supercontinent called Pangaea ; Pangaea broke up into Laurasia which became North America and Eurasia and Gondwana which became the remaining continents.

The following table lists the seven continents with their highest and lowest points on land, sorted in decreasing highest points.

Some sources list the Kuma—Manych Depression a remnant of the Paratethys as the geological border between Europe and Asia. North America. South America.

From Wikipedia, the free encyclopedia. Very large landmass identified by convention. For other uses, see Continent disambiguation. Main article: Boundaries between the continents of Earth.

See also: List of transcontinental countries. This section possibly contains synthesis of material which does not verifiably mention or relate to the main topic.

Relevant discussion may be found on the talk page. November Learn how and when to remove this template message.

For a more comprehensive list, see List of continents by population. Main article: Supercontinent. Further information: Indian subcontinent and Arabian Peninsula.

Main article: Submerged continent. Further information: Zealandia. Further information: Continental fragment. See also: Madagascar. Main article: Geological history of Earth.

This section needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed.

May Learn how and when to remove this template message. Further information: Continental crust and Plate tectonics. Geography portal Environment portal Ecology portal.

National Geographic. Retrieved 6 December Columbia Encyclopedia New York: Columbia University Press. Retrieved 20 February Oxford University Press ; "continent 1 n.

Catherine Soanes and Angus Stevenson. Oxford University Press; "continent 1 n. Erin McKean. ProQuest Information and Learning. Madalas isinasama rin sa mga ito ang mga nabasag na bahagi continental fragment o mikrokontinenteng tulad ng Madagascar na hindi karaniwang itinuturing kontinente.

May ilan ding mga kontinente na nakalubog, tulad ng kontinente ng Selandiya Ingles: Zealandia. Ang Daigdig lamang ang planetang natukoy na may kabalatang kontinental.

Madalas pinapangkat ang mga isla sa karagatan sa karatig-kontinente nito upang mahati ang buong mundo sa pitong rehiyon. Sa ilalim ng sistemang ito, ginugrupo kasama ng Awstralya ang karamihan sa mga kapuluan at isla sa Karagatang Pasipiko sa isang rehiyong tinatawag na Osiyanya Oceania.

Ayon sa madalas napagkakasunduan, "nauunawaan na ang kontinente ay isang malaki, tuloy-tuloy, at magkakahiwalay na masa ng kalupaan, madalas hinihiwalay ng mga malalawak na katubigan.

Nauwi sa isang di makatwirang pag-uuri ang pamantayan sa ano ba ang "malaki" sa hindi. Halimbawa, itinuturing na ang isla ng Greenland , na may lawak na 2,, kilometro kwadrado o , milya kwadrado ay ang pinakamalaking isla sa mundo, samantalang pinakamaliit naman na kontinente ang Awstralya , na may lawak na 7,, kilometro kwadrado o 2,, milya kwadrado.

May mga baybayin ang lahat ng mga pangunahing masa ng kalupaan ng Daigdig sa iisa't magkakakonektang Karagatan ng Mundo, na nahahati naman sa mga pangunahing bahagi ng katubigan depende sa kontinente at samu't saring mga pamantayang heograpikal.

Ang pinakamahigpit na kahulugan ng kontinente ay ang isang magkakarugtong [6] na kalupaan o pangunahing kalupaan mainland , kung saan binubuo ng mga baybayin at hangganang panlupa land boundaries ang mga gilid nito.

Sa pananaw na ito, tinutukoy ng kontinental na Europa ang pangunahing kalupaan ng Europa - di kasama rito ang mga isla ng Gran Britanya , Irlanda , Malta , at Islandiya.

Sa ganon ring pananaw, tinutukoy rin ng kontinente ng Awstralya ang pangunahing kalupaan ng Awstralya - di kasama naman rito ang isla ng Tasmanya at Bagong Ginea.

Tinutukoy naman ng kontinental na Estados Unidos ang magkakasamang 48 estado nito maliban sa Hawaii sa Karagatang Pasipiko at Alaska sa hilagang-kanluran ng Hilagang Amerika, na minsan ding sinasama sa naturang pangkat.

Sa usapan naman ng heolohiya o heograpiyang pisikal, maaaring lumagpas sa isang tuyong lupa dry land ang isang kontinente at isama ang mababaw at nakalubog na lapag kalapagang kontinental , o continental shelf [7] gayundin sa mga islang nakalitaw sa kalapagang iyon mga islang kontinental, o continental islands , sa kadahilanang kasama rin sila sa naturang kontinente.

Bilang pambuo ng kultura, lumalagpas sa kalapagang kontinental ang saklaw ng isang kontinente at sinasama ang mga mga nabasag na bahagi nito mikrokontinente at isla sa karagatan.

Kung susundin naman ito, mapapabilang din ang islang bansa ng Islandiya sa Europa at ang Madagascar naman sa Aprika. Kung ipipilit ang pinakatugatog ng konseptong ito, mapapabilang ang mga isla at kapuluang bansa sa platong kontinental ng Awstralya sa isang malakontinenteng quasi-continent tinatawag na Osiyanya Oceania.

Den Rest nehmen Meere und Inseln ein. Der einzige Unterschied betrifft die Bezeichnung der kleinsten Erdregion. Die US-amerikanische Quelle bezeichnet sie, jeweils ins Deutsche übertragen, als Australien und die britische als Ozeanien.

An dieser Feinheit ist abzulesen, wie vielseitig die Problematik sein kann, eine Definition für den Begriff Kontinent zu finden. Inselgruppe gehört zum Kontinent Asien, obwohl sie nicht aus kontinentaler Kruste besteht.

Nur ein kleiner Teil der Erdoberfläche gehört nicht dazu. Getrennt würden alle Kontinente letztlich durch die Ozeane. 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.

Help Learn to edit Community portal Recent changes Upload file. Retrieved 27 November In geology, a continent is defined by continental crust, which is a platform of metamorphic and igneous rocklargely of granitic composition. Gayunpaman, madalas itinuturing na kontinente ang Europa dahil sa kabuuang lawak ng lupang maikukumpara sa ibang kontinente: 10,, kilometro kuwadrado (3,, milya kuwadrado). Kalahati lang sa sukat na iyon ang kabuuang lawak ng Timog Asya, kaya madalas itong itinuturing na subkontinente. Sebaka sa linaha ke mobu o moholo oa metsi o pota-potiloeng ke metsi. Ka bongata bo boholo ba metsi a letsoai (a thehiloeng haholo ke maoatle) ao ho oona ho koahetsoeng ka karolo ea 75 lekholong ea lefatše, ho bonolo haholo ho bona mona le moo ho hlaha libaka tse ngata tse tsoelang pele, e leng ho etsang hore ho se ke ha e-ba bonolo hore li-geographer li fe mabitso ana mabitso a lihlekehleke. Br. Kontinent Površina Stanovnika 1 Azija: 44,4 mil. km² mil. 2 Afrika: 30,3 mil. km² mil. 3 Sjeverna Amerika: 24,2 mil. km² mil. 4. Mapa ku animashon ku ta mustra e diferente kontinentenan i regionan. Depende di e konvenio i modèl, algun kontinente ta konsolidá i subdividí: por ehempel, Eurasia ta keda subdividí den Eropa i Asia (koló kòrá), mientras Nort i Sur Amérika algun bes ta rekonosé komo ún kontinente Merikano (koló bèrdè). Derived terms []. superkontinent; Usage notes []. Depending on how one makes the divisions, one may count between 4 and 7 kontinenter on Earth, maybe most often 5 or 6 (Antarctic, Eurasia, Africa, Australia, and finally the Americas as either one or two).
Kontinente Wiki Ti maysa a kontinente ket maysa kadagiti kadakkelan a bagbagi ti kadagaan iti Lubong. Relevant discussion may be found on Nations League Termine talk page. Wigen Letzteres spiegelt auch die zunehmende Erforschung der Tektonik von Mikroplatten wider. Kontinente Wiki English Dictionary sa wikang Ingles ika-2 na edisyon. European Environmental Agency. Unsourced material may be Kostenlose Online Spielen and removed. Some areas of continental crust are largely covered by the sea and may be considered submerged continents. Extrapolating the concept to its extreme, some geographers group the Australian continental plate with other islands in the Pacific into one "quasi-continent" called Oceania. Psc Mit Paypal Kaufen latter geographers set the border between Europe and Asia at the isthmus between the Black Sea and the Caspian Seaand the border between Asia and Africa at the isthmus between the Red Sea and the mouth of Lake Bardawil on the Mediterranean Sea. Views Read Edit View history. Retrieved 19 November Some geological continents are largely covered with watersuch as Zealandia see submerged continents below. For other uses, see Continent disambiguation. 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. Deine Registrierung ist leider fehlgeschlagen. Australien ist der kleinste und flachste Kontinent der Erde und liegt wie eine riesige Insel im Meer. Bis im

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