Bamba la Antaktiki : Tofauti kati ya masahihisho

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[[Picha:AntarcticPlate.png|300px|thumb|Bamba la Antaktiki]]
'''Bamba la Antaktiki''' ni [[bamba la gandunia]] linalobeba [[bara]] la [[Bara la Antaktiki|Antaktiki]] na sehemu za sakafu ya bahari jirani.
 
Bamba hilo huwa na eneo la km<small><sup>2</sup></small> 60,900,000.
{{Infobox tectonic plate|image=File:AntarcticPlate.png|alt=The Antarctic Plate|type=[[List of tectonic plates#Major plates|Major]]|area={{convert|60,900,000|km2|sqmi|abbr=on}}<ref>{{cite web|url=http://geology.about.com/library/bl/blplate_size_table.htm |title=Sizes of Tectonic or Lithospheric Plates |publisher=Geology.about.com |date=March 5, 2014 |accessdate=January 22, 2016}}</ref>|move_direction=north-west|move_speed={{convert|12|-|14|mm|in|abbr=on}}/year|geo_features=[[Antarctica]], [[Southern Ocean]]}} '''Bamba la Antaktiki''' ni [[bamba la gandunia]] linalobeba [[bara]] la [[Bara la Antaktiki|Antaktiki]] na sehemu za sakafu ya bahari jirani.
 
Mabamba yanayopakana ni [[Bamba la Nazca]], [[Bamba la Amerika ya Kusini]], [[Bamba la Afrika]], [[Bamba la Australia]] na [[Bamba la Pasifiki]].
, Plateau ya Kerguelen na inayoenea nje chini ya [[Bahari kuu|bahari]] zinazozunguka. Baada kuvunjika kutoka Gondwana (sehemu ya kusini ya supercontinent [[Pangaia|Pangaea]] ), sahani Antarctic alianza kusonga bara la Antaktika kusini kwa eneo lake sasa wametengwa na kusababisha bara kuendeleza kiasi baridi ya hali ya hewa. <ref>{{Cite journal|last=Fitzgerald|first=Paul|date=2002|title=Tectonics and landscape evolution of the Antarctic plate since the breakup of Gondwana, with an emphasis on the West Antarctic Rift System and the Transantarctic Mountains|url=http://www.geology.cwu.edu/facstaff/huerta/g501/pdf/Fitzgerald2002.pdf|journal=Royal Society of New Zealand Bulletin|issue=35|pages=453–469|access-date=February 1, 2015}}</ref> Sahani ya Antarctic inafungwa karibu kabisa na mifumo ya upanuzi wa katikati ya bahari . Sahani zinazoambatana ni Bamba la Nazica, Bomba la [[Bamba la Amerika ya Kusini|Amerika Kusini]], [[Bamba la Amerika ya Kusini|Bamba]] la [[Bamba la Afrika|Kiafrika]], [[Bamba la Afrika|Sahara]] ya Kisomali, Bamba la Indo-Australia, Bomba la [[Bamba la Pasifiki|Pacific]], na, kwa mipaka ya kubadilisha, Bamba la Scotia .
 
,Kihistoria Plateaubaada ya Kerguelenkuvunjika na inayoenea nje chini yakwa [[Bahari kuu|bahariGondwana]] zinazozunguka. Baada kuvunjika kutoka Gondwana (sehemu ya kusini ya supercontinentbara kuu la kale [[Pangaia|Pangaea]] ), sahani Antarctic alianza kusonga barabamba la AntaktikaAntaktiki kusinililianza kwakusogea eneopale lakelilipo sasana wametengwa nahivyo kusababisha bara kuendeleza kiasitabianchi baridi yakabisa hali yala hewaAntaktiki. <ref>{{Cite journal|last=Fitzgerald|first=Paul|date=2002|title=Tectonics and landscape evolution of the Antarctic plate since the breakup of Gondwana, with an emphasis on the West Antarctic Rift System and the Transantarctic Mountains|url=http://www.geology.cwu.edu/facstaff/huerta/g501/pdf/Fitzgerald2002.pdf|journal=Royal Society of New Zealand Bulletin|issue=35|pages=453–469|access-date=February 1, 2015}}</ref> Sahani ya Antarctic inafungwa karibu kabisa na mifumo ya upanuzi wa katikati ya bahari . Sahani zinazoambatana ni Bamba la Nazica, Bomba la [[Bamba la Amerika ya Kusini|Amerika Kusini]], [[Bamba la Amerika ya Kusini|Bamba]] la [[Bamba la Afrika|Kiafrika]], [[Bamba la Afrika|Sahara]] ya Kisomali, Bamba la Indo-Australia, Bomba la [[Bamba la Pasifiki|Pacific]], na, kwa mipaka ya kubadilisha, Bamba la Scotia .
 
[[jamii:Gandunia]]