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To incline downward from the plane of the horizon; as, strata of rock dip.
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Inclination downward; direction below a horizontal line; slope; pitch.
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The angle of inclination of a mineral deposit. The true dip is always measured in a vertical plane perpendicular to the strike.
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An angle giving the orientatio n of a planar feature such as bedding or a fault plane; it is the acute angle measured between the planar feature and the horizontal. It is measure perpendicular to the strike direction.
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The steepest line of fall on a horizontal measured plane. It is the path a marble would follow as it rolled down the plane's surface. It is unidirectional and always perpendicular to strike.
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(4) the angle at which a structure or rock bed is inclined from the horizontal as measured at right angles to the strike and in the vertical plane.
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the amount and direction of tilt of a geologic surface from horizontal, measured in degrees. The geologic surface usually is a layered rock unit or a fault plane.
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The angle that a rock unit, fault or other rock structure makes with a horizontal plane. Expressed as the angular difference between the horizontal plane and the structure. The angle is measured in a plane perpendicular to the strike of the rock structure.
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The angle formed by the inclined plane of a geological structure and the horizontal plane of the Earth's surface.
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The angle between the horizontal plane and a structural surface (such as a bedding plane, a joint, a fault, foliation, or other planar features).
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The inclination to the horizontal of any stratum of earth or rock.
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(physics) the angle that a magnetic needle makes with the plane of the horizon
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appear to move downward; "The sun dipped below the horizon"; "The setting sun sank below the tree line"
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slope downwards; "Our property dips towards the river"
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(D). The angular difference between the geometrically true and the apparent or visual horizon.
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the angle a rock bed makes with the horizon; water dropped on a bed will run in the direction of the dip
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A measure of the angle between the flat horizon and the slope of a sedimentary layer, fault plane, metamorphic foliation, or other geologic structure.
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Angle of inclination a fault stratum makes with the horizontal plane. See Strike.
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The angle between the horizontal and a sloping surface such as a bedding plane; dip is measured perpendicular to strike direction.
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The angle that rock strata make with a horizontal surface, measured at right angles to the strike.
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the angle of incline from horizontal of a planar feature, such as an orebody
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an undesirable downward movement of the spine and head during the swing. Example: He had a pronounced dip in his downswing and as a result frequently shanked the ball.
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Refers to the angle at which the bedrock strata are inclined from the horizontal. Dip on bedrock surfaces may be caused by forces that bend the rock mass or by a variety of mechanisms active when sediments that make up the rock were accumulating.
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the angle that a refractor or reflector makes with the horizontal. Also, the angle of inclination of a geologic layer or sedimentary bed.
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the inclination of a geologic structure (bed, vein, fault, etc.) from the horizontal; dip is always measured downwards at right angles to the strike.
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The angle at which a vein, structure or rock bed is inclined from the horizontal as measured at right angles to the strike, also, the angle at which a drill hole is inclined, measured from the horizontal.
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The inclination from the horizontal of the to surface of a geological structure. A Dip Meter indicates dip relative to a well bore.
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The maximum angle that a structural surface, such as layering in a rock or a fault makes with the horizontal, measured in the vertical plane perpendicular to the strike.
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angle made to the horizontal by a bedding plane
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The angle that a planar geologic surface (for example, a fault) is inclined from the horizontal.
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The maximum angle of inclination downward that a vein or bed makes with a horizontal plane.
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the angle that a bedding plane or fault makes with the horizontal when measured perpendicular to the strike of the bedding plane or fault.
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the angle of the plan of a bed relative to the horizontal.
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The angle that a structural surface (e.g., a bedding or fault plane) makes with the horizontal, measured perpendicular to the strike of the structure.
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The angle by which a rock layer or fault plane deviates from the horizontal. The angle is measured in a plane perpendicular to the strike.
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Inclination of a geological feature/rock from the horizontal (perpendicular to strike);
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The angle between a geologic surface -- for example, a fault plane -- and the horizontal. The direction of dip can be thought of as the direction a ball, if placed upon the tilted surface, would roll. Thus, a ball placed on a north-dipping fault plane would roll northward. The dip of a surface is always perpendicular to the strike of that surface.
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a downward slope of a stratum or vein. [AHDOS
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The maximum angle by which a stratum or other planar feature deviates from the horizontal. The angle is measured in a plane perpendicular to the strike.
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Same as inclination.
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