1. EARTH MOVEMENT AND MAJOR LANDFORMS
FOLDING

2. FOLDING
Folding is the wave-like upliftment of sedimentary rocks due to horizontal forces from two opposite -side.
Folding happen when a part of the crust is pushed against another.

3. Syncline– down fold Anticlines – up fold

5. YOUNG or NEW FOLD MOUNTAINS
Young less than 65 million years old.
Includes today’s major mountain ranges: Andes, Himalayas, Rockies & the Alps.
Not ‘old’ fold mountain such as the lakes.

6. OLD FOLD MOUNTAINS
Old fold mountains were formed in a similar manner but more than 200 million years .
These have been eroded and worn down and have rounded packs.

7. summary Folding is the upliftment of sedimentary rocks.
There are old fold mountains and young fold mountains.
Syncline-down fold
Anticline –up fold

8. From Yogithaa Sreemathi Pranesh Harshit
Thank you
From Yogithaa
Sreemathi
Pranesh
Harshit