Mountains
<<%%What do old and young mountain tops look like?%%<<
@@Old mountains have been eroded and weathered over time making them more rounded, whereas young mountains have sharp peaks and steep slopes.@@
Anticline vs. Syncline
- Anticline - a fold in the rock that bends upward into an arch
- Syncline - a fold in the rock that bends downward to form a V shape
- Both are seen in fold mountains
- The upward part of the folded rock is called the
syncline
- The bottom of the fold is called the
anticline
%%Faults%%
%%Faults%%: A large brittle fracture in a rock body
The point of origin for most earthquakes
@@Folds@@
- %%Fold%%: Where two or more of Earth's tectonic plates are pushed together
@@Fold Mountains@@
- Fold Mountains are created when two plates ^^collide^^ with each other.
- When two plates collide together, the heavier plate sinks .
- The lighter plate then buckles upwards creating a fold mountain.
- e.g The Andreas Mountains. The Nazca Plate (heavier) slipped under the South American Plate (lighter).
@@Fault Mountains@@
- Fault mountains are formed when rock layers are pushed together and broken along a fault line
- When two plates collide together, the heavier plate sinks .
- The lighter plate then buckles upwards creating a fold mountain.
- e.g The Andreas Mountains. The Nazca Plate (heavier) slipped under the South American Plate (lighter).
- \
Types of Plate Boundaries:
- ^^Divergent Boundary^^****: plates that move apart.
- Mid-ocean Ridges, Rift Valleys, Fissure Volcanoes
- ^^Convergent Boundary:^^ occurs due to subduction. Plates move towards each other or pushed under another.
- Also called “Destructive Boundaries” because plate materials is subducted.
- Mountains and volcanoes
- %%Three types of Convergent Boundary:%%
- Oceanic–continental: subduction zone, deep ocean trenches. Stratovolcanoes and Volcanic Mts. on Land.
- Oceanic –oceanic: Subduction zone. Deep Ocean Trenches, Island Arcs, Undersea Volcanism
- Continental-continental: mountain ranges
- ^^Transform Boundary:^^ plates slide past each other.
- Creates fault valley or undersea canyon
- Most earthquake occurs in this boundary.