Folding

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Folding occurs when layers of rock in the crust buckle due to collisions between tectonic plates. There are two main types of folds: anticlines, where the rock layers buckle upwards in an inverted U-shape, and synclines, where layers buckle downwards in a U-shape. Different kinds of folds form depending on the direction and amount of compressional forces, including symmetrical, asymmetrical, overfolded, recumbent, and overthrust folds. Folding of layers can result in the formation of fold mountains over geologic timescales.

What is folding? ,[object Object],[object Object],[object Object],[object Object]

Types of folds ,[object Object],[object Object],[object Object],[object Object],[object Object]

Overfold / Overturned Fold ,[object Object],[object Object]

Recumbent Fold ,[object Object],[object Object]

Overthrust Fold ,[object Object],[object Object]

Different folds Symmetrical fold Asymmetrical fold Overfold Recumbent fold

Resultant landforms ,[object Object],[object Object]

What is fault? Fault terminology Fault plane: Hanging wall Foot wall Slip and separation: Separation Classification of faults Apparent movement as basis Normal faults Graben Reverse faults: Strike – slip faults On the basis of altitude (dip and strike) Mode of occurrences as basis Parallel faults Enechelon faults Peripheral faults Radial faults On the basis of slip Engineering consideration of faults

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Folding

1. Landscape Folding

8. Anticline and Syncline

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14. Different folds Symmetrical fold Asymmetrical fold Overfold Recumbent fold

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Folding

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