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Mica is crystalline and forms layers.
Foliated metamorphic rocks exhibit a layering affect with parallel layers of mineral crystals one on top of the other. A good example of this is gneiss, which has alternating layers of light and dark minerals. Foliation takes place when pressure is applied to crystals and they recrystallize or align themselves at right angles to the direction of the applied directional stress.
Flint is a chemical sedimentary rock formed from the precipitation of silica rich solutions in layers of marine sediments.
Yes
Visible layers or bands in metamorphic rock is designated as 'foliation' and the rock is said to be 'foliated'.
Probably not. While layered lava flows are not uncommon, most layered rocks formed from the accumulation and lithification of sediment.
Some minerals in sedimentary rocks include halite mineral crystals which are in rock salt and gypsum mineral crystals which are in rock gypsum. Also, calcite crystals are found in oolitic limestone and travertine.
Mica is crystalline and forms layers.
deep under the earth
A mineral alignment is a layered arrangement of firmly joined crystals of minerals; the minerals are aligned in layers or bands.
Maybe Sedimentary Rocks?
yes
The definition of hue is color. Appearance could also relate to color, or if the mineral has cleavage or is fractured. Cleavage refers to the formation of a mineral in layers, and fracture is when a mineral has no specific formation pattern. These characteristics are visible. How a mineral appears is what it looks like.
They are called foliated metamorphic rocks.
The texture of a rock consists of it's grain or mineral crystal size, the arrangement of the grains or crystals, and the degree of uniformity of the grains or crystals. Examples of rock texture would be: * Coarse grained--visible crystals or grains as in granite. * Fine grained--small grains, invisible to the unaided eye as in shale. * Porphyritic--large visible crystals in a fine grained matrix as in granite porphyry. * Schistose--layers of flattened micaceous minerals such as in mica schist. * Foliated--a metamorphic rock texture of parallel mineral banding as in gneiss. * Homogenous--same grain apperance in all directions as in basalt.
Foliated metamorphic rocks exhibit a layering affect with parallel layers of mineral crystals one on top of the other. A good example of this is gneiss, which has alternating layers of light and dark minerals. Foliation takes place when pressure is applied to crystals and they recrystallize or align themselves at right angles to the direction of the applied directional stress.
rock formed of small rocks that are cemented together by dissolved mineral material?