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  2. Cleavage (crystal) - Wikipedia

    en.wikipedia.org/wiki/Cleavage_(crystal)

    Miller index {h k ℓ}. Cleavage forms parallel to crystallographic planes: [1] Basal, pinacoidal, or planar cleavage occurs when there is only one cleavage plane.Talc has basal cleavage.

  3. File:Olivine nodule in basalt from Smrčí, Czech Republic.jpg

    en.wikipedia.org/wiki/File:Olivine_nodule_in...

    English: Green olivine nodule (mantle xenolith) in basalt from Smrčí, Czech Republic. The dominant olivine component is forsterite over minor fayalite, the rest of nodule is made of smaller amount of pyroxene and spinel. Size of the specimen 9x7.5 cm.

  4. Olivine - Wikipedia

    en.wikipedia.org/wiki/Olivine

    The mineral olivine (/ ˈ ɒ l. ɪ ˌ v iː n /) is a magnesium iron silicate with the chemical formula (Mg,Fe) 2 Si O 4.It is a type of nesosilicate or orthosilicate.The primary component of the Earth's upper mantle, [9] it is a common mineral in Earth's subsurface, but weathers quickly on the surface.

  5. Fracture (mineralogy) - Wikipedia

    en.wikipedia.org/wiki/Fracture_(mineralogy)

    Fracture differs from cleavage in that the latter involves clean splitting along the cleavage planes of the mineral's crystal structure, as opposed to more general breakage. All minerals exhibit fracture, but when very strong cleavage is present, it can be difficult to see.

  6. Cleavage (geology) - Wikipedia

    en.wikipedia.org/wiki/Cleavage_(geology)

    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.

  7. Kimberlite - Wikipedia

    en.wikipedia.org/wiki/Kimberlite

    The distinctive characteristic of olivine lamproites is phlogopite macrocrysts and microphenocrysts, together with groundmass micas that vary in composition from phlogopite to "tetraferriphlogopite" (anomalously Al-poor phlogopite requiring Fe to enter the tetrahedral site). Resorbed olivine macrocrysts and euhedral primary crystals of ...

  8. Cumulate rock - Wikipedia

    en.wikipedia.org/wiki/Cumulate_rock

    A rock consisting of 80% olivine, 5% magnetite and 15% groundmass is an olivine mesocumulate, (in essence a peridotite). Cumulate terminology is appropriate for use when describing cumulate rocks. In intrusions which have a uniform composition and minimal textural and mineralogical layering or visible crystal accumulations it is inappropriate ...

  9. Conchoidal fracture - Wikipedia

    en.wikipedia.org/wiki/Conchoidal_fracture

    A conchoidal fracture is a break or fracture of a brittle material that does not follow any natural planes of separation. Mindat.org defines conchoidal fracture as follows: "a fracture with smooth, curved surfaces, typically slightly concave, showing concentric undulations resembling the lines of growth of a shell". [ 1 ]