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Moho
en
(geology) The Mohorovičić discontinuity.
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Moho
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moho
en
The North Island takahē, an extinct rail of New Zealand.
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This species comprises several subspecies found throughout much of Australasia and the south-west Pacific region, including the Philippines (where it is known as tikling), New Guinea, Australia, New Zealand (where it is known as the banded rail or moho-pereru in Māori), and numerous smaller islands, covering a range of latitudes from the tropics to the Subantarctic.
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The Mohorovičić discontinuity (Croatian pronunciation: ), usually referred to as the Moho, is the boundary between the Earth's crust and the mantle.
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At significantly shallower depths, above the Moho, calcic plagioclase is the more stable aluminous mineral in peridotite while garnet is the stable phase deeper in the mantle below the spinel stability region.
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"Moho House" on IMDb "Moho House" at TV.com
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4 sinne gevind in 1 ms. Hulle kom uit baie bronne en word nie nagegaan nie.