Continental-continental convergence occurs when two continental plates collide and push against each other, forming large mountain ranges such as the Himalayas. When sedimentary layers between the plates are crumpled and folded, fold mountains are created, with anticlines where the rocks fold upward and synclines where they fold downward. Folds can be symmetrical, asymmetrical, isoclinal, overturned, or recumbent, depending on the orientation and steepness of the axial plane and limbs. Examples of fold mountain ranges include the Himalayas, Alps, Andes, Rockies, and Urals.
10. When an area of sea separates two plates, sediments will settle onto the sea floor and become sedimentary rocks. When the plates move towards each other, the layers of sedimentary rock become crumpled and folded, which makes them fold mountains.
11. syncline anticline Where the rocks are folded upwards, they are called anticlines. Where the rocks are folded downwards, they are called synclines.
18. Folds may be symmetrical or asymmetrical. In a symmetrical fold , the axial plane is vertical and the sides dip symmetrically from the axis. A symmetrical fold is one in which the axial plane is vertical.
26. A fold that’s axial plane’s tilted and beds may dip in same direction of both sides of the axial plane, resulting in one of limbs being rotated through an angle of at least 90 degrees.
29. A plate's axial plate is horizontal, so one of the limbs is completely covered. it is the extreme version of the over turned fold but rotated more then 90 degrees.
39. Notes Axial Plane: an imaginary plane surface that divides a fold symmetrically Fold Axis: a line drawn along the points of maximum curvature of a layer of a fold Plunge: the angle between the horizontal plane and the fold axis
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42. The End Done by Li Wang, Jasmine Lin, Park Byeong Joo, Clara Che Wei Peh