- Vulkanologi : kebumian's knowledge that memplajari gunungapi
- Magma : silicate material moltens comprise of incandescence
solid material,molten,and gas that exists at lithosphere coat earths.
Magmas normal temperature bersikar
900 c 1200 C.
- Erupsi : its issue process magma of lithosphere coat gets to
permukan earth. Erupsi one gunungapi dapdt as discharge (efusif) via crack
on stone facings. And sumburan's explosion (ekaplosif) via crater or
volcano funnel.
- I ntrusi is magma : magma
squandering process via rocks streaked cracks, but doesn't get to earth
surface. If intrusi magma ices therefore will form intrusiva's rock.
- Lava : secretory magama gets to earth surface.
- Lava : lava already gets dash with materials at surface
bumu.
- Eflata / is piroklastik's
material : untrammeled material from
gunungapi while happens explosive eruptions.
- Crater : hole on gunungapi's body as place of its issue
magma. Sizable crater so-called caldera. If caldera was filled by water
that quite a lot mak will form vulkanik's crater or lake lake. Crater and
caldera that at Indonesia, for example Crater Takubanperahu (West java),
Tengger's crater (Intermediate java), and Batur's Mountain Caldera (Bali).
Jumat, 30 November 2012
Vulkanisme 's terminologies:
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