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| A | B | C | D |
| (1) Oxidation | (1) Solution | (1) Fall | (1) Pressure |
| (2) Carbonation | (2) Salt weathering | (2) Creep | (2) Temperature |
| (3) Freeze thaw weathering | (3) Oxidation | (3) Slide | (3) Slope |
| (4) Shattering | (4) Carbonation | (4) Flow | (4) Rainfall |
| A | B | C | D |
| (1) Algae | (1) Rock fall | (1) Relief and slope | (1) Shattering |
| (2) Roots and plants | (2) Landslide | (2) Gravity | (2) Block disintegration |
| (3) Lichens | (3) Earth flow | (3) Water | (3) Exfoliation |
| (4) Moss | (4) Exfoliation | (4) Vegetation | (4) Burrowing |
| A | B | C | D |
| (1) Symmetrical Fold | (1) Black Forest | (1) Narmada Valley | (1) Caldera |
| (2) Isoclinal Fold | (2) Vosges | (2) African Valley | (2) Crater Lake |
| (3) Overturned Fold | (3) Himalayas | (3) Tapi Valley | (3) Cinder Cone |
| (4) Recumbent Fault | (4) Satpuras | (4) Rhine Valley | (4) Lava Plateau |
| A | B | C | D |
| (1) Mt. Fujiyama | (1) Normal Fault | (1) Rock Fragments | (1) Crater Lake |
| (2) Mt. St. Helens | (2) Reverse Fault | (2) Volcanic Dust | (2) Caldera |
| (3) Pinatubo | (3) Tear Fault | (3) Inflammable gases | (3) Volcanic Plug |
| (4) Mayon | (4) Overturned fold | (4) Biotic Material | (4) Volcanic Plateau |
| A | B | C | D |
| (1) Asymmetrical Fold | (1) Normal Fault | (1) Zone I – Very high intensity | (1) Limb |
| (2) Overturned Fold | (2) Thrust Fault | (2) Zone II – High intensity | (2) Anticline |
| (3) Isoseismal Lines | (3) Reverse Fault | (3) Zone III – Moderate intensity | (3) Syncline |
| (4) Symmetrical Folds | (4) Tear Fault | (4) Zone IV – Low intensity | (4) Trough |