Hand Specimen Description Flashcards
Melanocratic
Mostly dark grains
Leucocratic
Mostly light grained
Mesocratic
Mostly intermediate lightness grains
Mafic
MAgnesium, FerrIC
Dark minerals
Felsic
FELdspar, SIliCates
Light minerals
3 properties for colour
1) Lightness (Melanocratic, Mesocratic, Leucocratic)
2) Index (Mafic/Felsic)
3) Hue
Phaneritic
Can see individual minerals
Aphaneritic
Can’t distinguish individual minerals
Crystals over 5mm
Coarse-grained
Crystals 2-5mm
Medium-sized
Crystals less than 2mm
Fine-grained
Cryptocrystalline
If you can’t see individual crystals with a hand lens
Cryptocrystalline is a rock texture made up of such minute crystals that its crystalline nature is only vaguely revealed even microscopically
Equigranular
Equal sized grains
Interlocking crystals indicate
Igneous (or metamorphic)
Interlocking crystals indicate
Igneous (or metamorphic)
Granular rocks indicate
Sedimentary
Groundmass
Finer minerals around phenocrysts
Foliation
Foliation in geology refers to repetitive layering in metamorphic rocks.
Schistosity
The foliation in schist or other coarse-grained, crystalline rock due to the parallel, planar arrangement of mineral grains of the platy, prismatic, or ellipsoidal types, usually mica. It is considered by some to be a type of cleavage.
Bedding
Beds are the layers of sedimentary rocks that are distinctly different from overlying and underlying subsequent beds of different sedimentary rocks.
Strata or Stratum
In geology and related fields, a stratum is a layer of sedimentary rock or soil, or igneous rock that was formed at the Earth’s surface
Lamination
lamination is a small-scale sequence of fine layers (laminae; singular: lamina) that occurs in sedimentary rocks. Laminae are normally smaller and less pronounced than bedding
Friable
rock or mineral that crumbles naturally or is easily broken, pulverized, or reduced to powder, such as a soft and poorly cemented sandstone.
Vesiculation and Vesicles
Vesicles are the small holes left behind after lava cools and turns into volcanic rock. Vesicles help geologists understand the cooling history of extrusive (volcanic rocks) because lava contains large amounts of dissolved gases that are released as the lava hardens.