SGT-Xwp1

2. A fold sharing constant orthogonal thickness of rocks.
4. A fold in which the hinge is angular.
6. An erosnal surface separating two unrelated groups of rocks.
7. A fault in which hangingwall block goes up relative to the footwall block.
9. A depression located along the axial trend of an anticline.
11. The elastic behaviour of a material during deformation.
14. Anguler fragments of lava in a tuffaceous matrix.
18. minor normal faults having similar orientation as that of the associated major fault.
19. A seismically active, median mountain range present in Atlantic and Pacific occean.
20. It is a fracture along which the rocks are relatively displaced from one another.

1. The faults which radiate from a central point.
3. A low angle thrust fault showing displacement for several kilometers.
5. A geosyncline in which volcanism is not associated with sedimentation.
8. A tectonically active zone which has not experienced earthquake during a time interval.
10. A structurally high area in the crust, produced by uprising movements as is seen in a dome also.
12. A fault showing horizontal sh'ike separation.
13. It is a rock-fracture produced due to less amount ofdeformation or strain.
15. A regional linear topographic feature reflecting a crusta I structure.
16. A planar surface parallel to axis of a fold.
17. The angle between the horizontal and the lineation, measured in the plane containing the lineation.