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Distal [sedimentology]
| Глоссарий геологических терминов |
(adjective) said of a sedimentary deposit consisting of fine clastics and deposited farthest from the source area. compare - proximal. gg
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Distal, английский
- In a manipulative or interrogating system, of or pertaining to the end opposite from the eyepiece and farthest from the person using the system. objective; tip.
- In a manipulative or interrogating system, of or pertaining to the end opposite from the eyepiece and farthest from the person using the system. objective; tip. e
- In a manipulative or interrogating system, of or pertaining to the end opposite from the eyepiece and farthest from the person using the system. objective; tip.1 e effective emissivity (?*): measured emissivity value of a particular surface under existing measurement conditions (rather than the generic tabulated value for the surface material) that can be used to correct a specific measuring instrument to provide a correct temperature measurement.3 effusivity, thermal: ability of heat to escape from a body, expressed as a characteristic of that body.3 square root of the product of thermal conductivity, mass density and specific heat.
Distal convoluted tubule, английский
A part of the kidney filtering system before the collecting ducts
Distal interphalangeal joint, английский
A joint nearest the end of the finger or toe. abbr dip
Distal phalanges, английский
Bones nearest the ends of the fingers and toes
Distal phalanx, английский
Distal surface, английский
Sedimentary, английский
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Distributary [streams], английский
(a) a divergent stream flowing away from the main stream and not returning to it, as in a delta or on a flood plain. it may be produced by stream deposition choking the original channel. (b) one of the channels of a braided stream; a channel carrying the water of a stream distributary. gg
Disintegration moraine, английский
A drift topography characterized by chaotic mounds and pits, generally randomly oriented, developed in supraglacial drift by collapse and flow as the underlying stagnant ice melted. slopes may be steep and unstable and there will be used and unused stream courses and lake depressions interspersed with the morainic ridges. characteristically, there are numerous abrupt, lateral and vertical changes between unconsolidated materials of differing lithology. sj & sw
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