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Hematite (/ ˈ h iː m ə ˌ t aɪ t, ˈ h ɛ m ə-/), also spelled as haematite, is a common iron oxide compound with the formula, Fe 2 O 3 and is widely found in rocks and soils. [6] Hematite crystals belong to the rhombohedral lattice system which is designated the alpha polymorph of Fe
Green fluorite with prominent cleavage Biotite with basal cleavage. Cleavage, in mineralogy and materials science, is the tendency of crystalline materials to split along definite crystallographic structural planes.
In chemistry, bond cleavage, or bond fission, is the splitting of chemical bonds.This can be generally referred to as dissociation when a molecule is cleaved into two or more fragments.
Cleavage (breasts), the partial exposure of breasts or their intervening gap. Buttock cleavage, the minor exposure of the buttocks and the gluteal cleft between them; Toe cleavage, the partial exposure of toes in shoes
Since the nature of cleavage is dependent on scale, slaty cleavage is defined as having 0.01 mm or less of space occurring between layers. [1] Slaty cleavage often occurs after diagenesis and is the first cleavage feature to form after deformation begins.
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Hematites is a genus of belemnite from the Mississippian Epoch. See also. Paleontology portal; Belemnite; List of belemnites; References This page was last edited on ...
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