List of tectonic plate interactions
http://dbpedia.org/resource/List_of_tectonic_plate_interactions an entity of type: Thing
Tectonic plate interactions are classified into three basic types:
* Divergent boundaries are areas where plates move away from each other, forming either mid-ocean ridges or rift valleys. These are also known as constructive boundaries.
* Convergent boundaries are areas where plates move toward each other and collide. These are also known as compressional or destructive boundaries.
* Subduction zones occur where an oceanic plate meets a continental plate and is pushed underneath it. Subduction zones are marked by oceanic trenches. The descending end of the oceanic plate melts and creates pressure in the mantle, causing volcanoes to form.
* Obduction occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates
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Bíonn trí chineál idirghníomhaíocht bainteach le teicteonaic phlátaí
* a tharlaíonn sna háiteanna a scarann plátaí óna chéile, agus le himeacht ama cruthaítear droim sléibhe ar ghrinneall an aigéin. Tugtar teorainneacha cruthaitheacha orthu freisin.
* Teorainneacha coinbhéirseacha a aimsítear sna háiteanna a bhuaileann plátaí isteach ar a chéile. Scriostar carraigeacha anseo agus dá bhrí sin tugtar teorainneacha scriosacha nó comhbhrúiteacha orthu.
* Criosanna fodhuchtaithe (freisin: 'Zóin fhodhuchtaithe') a aimsítear sna háiteanna a mbuaileann pláta aigéanach agus pláta ilchríochach lena chéile. Bíonn baint ag leo. Lúbann pláta amháin agus téann sé síos isteach faoin bpláta eile. Tugtar 'fodhuchtú' ar an phróiseas sin agus 'zón foduchtaithe' ar an áit ina dtarlaonn sé. Leánn an chui
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Liosta idirghníomhaíocht teicteonacha
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List of tectonic plate interactions
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146184
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1105938025
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Tectonic plate interactions are classified into three basic types:
* Divergent boundaries are areas where plates move away from each other, forming either mid-ocean ridges or rift valleys. These are also known as constructive boundaries.
* Convergent boundaries are areas where plates move toward each other and collide. These are also known as compressional or destructive boundaries.
* Subduction zones occur where an oceanic plate meets a continental plate and is pushed underneath it. Subduction zones are marked by oceanic trenches. The descending end of the oceanic plate melts and creates pressure in the mantle, causing volcanoes to form.
* Obduction occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction.
* Orogenic belts occur where two continental plates collide and push upwards to form large mountain ranges. These are also known as collision boundaries.
* Transform boundaries occur when two plates grind past each other with only limited convergent or divergent activity.
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Bíonn trí chineál idirghníomhaíocht bainteach le teicteonaic phlátaí
* a tharlaíonn sna háiteanna a scarann plátaí óna chéile, agus le himeacht ama cruthaítear droim sléibhe ar ghrinneall an aigéin. Tugtar teorainneacha cruthaitheacha orthu freisin.
* Teorainneacha coinbhéirseacha a aimsítear sna háiteanna a bhuaileann plátaí isteach ar a chéile. Scriostar carraigeacha anseo agus dá bhrí sin tugtar teorainneacha scriosacha nó comhbhrúiteacha orthu.
* Criosanna fodhuchtaithe (freisin: 'Zóin fhodhuchtaithe') a aimsítear sna háiteanna a mbuaileann pláta aigéanach agus pláta ilchríochach lena chéile. Bíonn baint ag leo. Lúbann pláta amháin agus téann sé síos isteach faoin bpláta eile. Tugtar 'fodhuchtú' ar an phróiseas sin agus 'zón foduchtaithe' ar an áit ina dtarlaonn sé. Leánn an chuid den phláta aigéanach atá foduchtaithe agus cruthaíonn sé seo brú sa mhaintlín, rud is cúis le bolcáin a fhoirmiú.
* a tharlaíonn nuair a bhrúitear pláta ilchríochach faoi phlátá aigéanach, ach tá sé seo neamhghnách, mar go mbíonn dlúis choibhneasta na bplátaí teicteonacha i bhfabhar fodhuchtaithe an phláta aigéanaigh. Lúbann an pláta aigéanach agus dá bharr, de ghnáth, cruthaítear droim láraigéin nua, agus iompaítear an ródhuchtú go fodhuchtú.
* a tarlaíonn nuair a bhualann dhá phláta ilchríochach lena chéile. Ag éirí as na fórsaí a chruthaítear, déantar sliabhraonta móra. Tugtar teorainneacha imbhuailte orthu freisin.
* a tharlaíonn nuair a mheileann dhá phláta thar a chéile le gníomhaíocht choinbhéirseach nó dhibhéirseach teoranta amháin.
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