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calcareous Formed from or containing a high proportion of calcium carbonate in the form of calcite or aragonite, used of a sediment, sedimentary rock, or soil type. calcite A mineral that is the crystalline form of calcium carbonate (CaCO 3), showing trigonal symmetry and a great variety of mineral habits.
The following is a list of rock types recognized by geologists.There is no agreed number of specific types of rock. Any unique combination of chemical composition, mineralogy, grain size, texture, or other distinguishing characteristics can describe a rock type.
Tor – Large, free-standing rock outcrop on a gentle hill summit; Tower karst – Tall structures of soluble rock; Tuya – Flat-topped, steep-sided volcano formed when lava erupts through a thick glacier or ice sheet; Volcanic cone – Landform of ejecta from a volcanic vent piled up in a conical shape; Volcanic island – Island of volcanic ...
A rock formation is an isolated, scenic, or spectacular surface rock outcrop. Rock formations are usually the result of weathering and erosion sculpting the existing rock. The term rock formation can also refer to specific sedimentary strata or other rock unit in stratigraphic and petrologic studies.
Perianth or other segments free, not united. Compare symphyllous, gamophyllous, and polyphyllous. apophysis 1. The external part of a cone scale. 2. An outgrowth of an organ or an enlargement of a stem. appendage A secondary part attached to a main structure; an external growth that seldom has any obvious function, hence appendiculate ...
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For a more diffuse surface, a continuous growth mechanism may require changes over several successive layers simultaneously. Non-uniform lateral growth is a geometrical motion of steps—as opposed to motion of the entire surface normal to itself. Alternatively, uniform normal growth is based on the time sequence of an element of surface.
Planes of weakness are developed in metamorphic rocks by the recrystallization and growth of micaceous minerals. [4] A rock's fissility can be degraded in numerous ways during the geologic process, including clay particles flocculating into a random fabric before compaction, bioturbation during compaction, and weathering during and after uplift.