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Keywords:
Planar,
Intersects,
Fault,
Outcrop,
Compass
The horizontal direction of the outcropping edges of tilted rocks; or, the direction of a horizontal line supposed to be drawn on the surface of a tilted stratum. It is at right angles to the dip.
A tunnel bored horizontally into the slate vein
The angle between true north and the horizontal line contained in any planar feature (inclined bed, dike, fault plane, and so forth); also the geographic direction of this horizontal line.
The direction in which a horizontal line can be drawn on a plane.
refers to a horizontal line along on inclined plane.
An angle giving the orientation of a planar feature such as bedding or a fault plane; it is the compass direction of the line of intersection of the planar feature and the horizontal. It is usually given as "N40E" (forty degrees east of north, or "N60W" etc.
Compass direction of the intersection between a structural surface (such as a bedding plane or a fault plane) and the horizontal.
1. ) The horizontal line marking the intersection between the inclined plane of a solid geological structure and the Earth's surface. 2. The compass direction of this line, measured in degrees from true north.
The bearing (compass direction) of a horizontal line on a bedding plane, a fault plane, or some other planar structural feature.
The compass direction of the line of intersection created by a dipping bed or fault and a horizontal surface.
general trend or direction of a geological feature in a horizontal plane
the trend of a linear feature on a map or on a generally flat ground surface. The linear feature usually is the eroded end of a layered rock unit or the inter-section of a fault plane with the land surface.
a bearing (relative to North) of an imaginary horizontal line on the plane
The bearing of a horizontal line in a plane or a joint.
The course or bearing of the outcrop of an inclined bed or structure on a level surface. It is perpendicular to the direction of the dip.
The geographic direction of a line created by the intersection of a plane and the horizontal. Often used to describe the geographic "trend" of a fold or fault.
The direction of a horizontal line on a plane (e.g., bedding, cleavage or fault plane); strike is perpendicular to dip direction (see Dip).
(1) the horizontal course or bearing of an inclined bed, stratum or vein, or the direction of a horizontal line in the plane of an inclined bed, stratum or vein.
The direction, or bearing from true north, of a vein or rock formation measured on a horizontal surface.
The direction or trend of a bedding plane or fault, as it intersects the horizontal.
Trend or bearing, relative to north, of the line defined by the intersection of a planar geologic surface (for example, a fault or a bed) and a horizontal surface such as the ground.
The direction of the line of intersection of a bed or vein with the horizontal plane. The strike of a bed is the direction of a straight line that connects two points of equal elevation on the bed.
The bearing of a horizontal line in the plane of a vein, bed, or fault with respect to the cardinal points of the compass.
The direction taken by a structural surface such as a fault or bedding plane as it intersects the horizontal;
The direction, or trend, of the line marking the intersection of a fault plane (or another planar geologic feature) with the horizontal. Strike is always at a right angle to dip.
The course or bea ri ng of the outcrop of an inclined bed or structure on a level surface.
Direction taken by a structural surface such as an ore body, fault or bedding plane as it intersects a horizontal plane
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