Aritz Hodei Itsaso
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Transcript of Aritz Hodei Itsaso
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GEOLOGIA LANA
ARITZ LASARTE, HODEI HERNANDEZ ETA ITSASO IDOATE
DBH 2.B
2008-ko Apirila
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HORN (higadura egitura)
ZIRKUA
MIHIA
MORRENA (sedimentazio
egitura)
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U itxurako harana.
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ILDOA
KARKABAK
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MAITAGARRIEN TXIMINIA (HIGADURA
EGITURA)
Maitagarrien tximiniak karkaben antzera sortzen dira, baino material heterogeneoaren gainean. Harri gogorrek, higaduraren aurkako erresistentzia haundia dutenez, azpiko harriak babesten dituzte.
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HARRERA ARROA: Urak metatzen diren tokia.
(higadura egitura)
HUSTUBIDE KANALA: Urak egiten duen ebakidura.
(garraio egitura)
ALUBIOI KONOA: Garraiatutako materialak
metatzen diren tokia. (sedimentazio egitura)
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SEDIMENTAZIOA
Ibaiek eragile geologiko bezala ura dute, solido nahiz likido izan. Gainera hiru prozesu geologiko betetzen dituzte: Higadura, garraioa eta sedimentazioa.
HIGADURA
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UR JAUZIAK
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UR-LASTERRAK
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ARROILA
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IBAIAREN MEANDROA
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IBAI BARRAK IBAIAREN METAKETAK
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IBAI-TERRAZA
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DELTAESTUARIOA
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DOLINA
HAITZULOA
ESTALAGMITAK ETA
ESTALAKTITAK
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ESTALAGMITAK ETA ESTALAKTITAK
LEIZEA
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ERG
Haizeak harriak higatzeko gaitasuna du eta hau korrosioa deitzen da. Haizeak basamortuko harea mugitzen du baino ez harriak. Horrela REG-ak (harri basamortuak) eta ERG-ak (harea basamortuak) sortzen dira.
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REG edo basamortu harritsua
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DUNAK
Dunak basamortuetan haizeak sortzen dituen harea multzoak dira. Haizeak jotzean dunek C forma hartzen dute eta aurrera mugitzen dira. Duna txikiak azkarrago mugitzen dira eta haundiekin elkartzen dira tamainu handiago izateko.
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HONDARTZA
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ITSASLABARRAK
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ITSASLABARRAK
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BADIAK
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TONBOLOA