mictite (mic'-tite). Coarsely composite rock formed as the result of contamination of a magma, by the incorporation and partial or complete assimilation of country-rock fragments, under conditions of relatively low temperature and probably at relatively high levels in the crust (Dietrich and Mehnert, 1961). Rarely used.
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median lamina . In many stenolaemate bryozoans, the erect median colony wall from which zooids grow in two back-to-back layers to form bifoliate colonies. Syn: mesotheca.
frost creep . Soil creep resulting from frost action (Kerr, 1881).
saltierra (sal-ti-er'-ra). A deposit of salt left by evaporation of a shallow, inland lake. Archaic. Etymol: Spanish, "salt earth".
hydrogenesis (hy-dro-gen'-e-sis). The natural condensation of moisture in the air spaces of surficial soil or rock material.
chute [hydraul] . An inclined water course, either natural or artificial.
filter feeder . An animal that obtains its food by removing particulate organic matter from water that passes through a part of its body used as a filter; e.g., bryozoans, barnacles, bivalves. Cf: suspension feeder.
boralsilite . A colorless or white monoclinic mineral: Al16B6O30(Si2O7).
natural remanent magnetization . The entire remanent magnetization of a rock as measured in the absence of an inducing magnetic field. Abbrev: NRM. Syn: natural remanence; natural remanent magnetism.
mesogenetic (mes''-o-ge-net'-ic). A term for the period between the time when newly buried deposits are affected mainly by processes related to the depositional interface ( eogenetic stage) and the time when long-buried deposits are affected by processes related to the erosional interface ( telogenetic stage). Also applied to the porosity that develops during the mesogenetic stage (Choquette and Pray, 1970, p.220).