Mrs. Z’s Mountain Building notes ONLY!
Mountain Building
Rock Deformation AKA – Mountain
Building
• Deformation - the bending, breaking, and
tilting of the earth’s crust.
• Three types of Stress:
1. Compressional
 
2. Tensional
 
3. Shear

FOLDING - flat layers of rock are
under severe compression and are
squeezed from the sides. The
layers moved into folded positions
without breaking (although some
cracks may appear).
 Three types of Folds:
1. Anticlines - upward folds
2. Synclines – downward
folds
3. Monoclines – gently
dipping bends in
horizontal rock layershttp://www.cr.nps.gov/history/online_books/geology/publications/bul/1508/images/fig27.jpg
Features formed by tectonic activity
Normal
1. Faults - A break in the
rock layers along
which there is no
movement is called a
fracture.
Once movement
occurs, the fracture is
known as a fault.
Three Main Types of
Faults:
 2. Reverse Fault
• occurs along convergent boundaries (compression force)
• The hanging wall moves up above the foot wall
 Thrust Fault
o reverse fault where the hanging wall is pushed at
such a low angle (not steep) that it moves UP AND
OVER the foot wall
 3. Strike-Slip Fault
• occurs at transform boundaries
(shearing force)
• The rocks along either side of the fault
slide horizontally
 Ex. San Andreas Fault
North Carolina Fault System
Four Types of Mountains
1. Folded Mountains - Found where continents have
collided. Ex. Appalachian Mts., Himalayan Mts.
• Plateaus - areas of flat-topped land high above
sea level. Ex. Colorado Plateau (Grand Canyon)
2. Fault-Block Mountains - Formed by faults, where
part of the earth’s crust have been broken into large
blocks and then were lifted above the surrounding
crust. Ex. Grand Teton, MT
3. Volcanic Mountains - Form when molten rock erupts
onto earth’s surface.
Ex. Cascade Mts. in Pacific NW and
the mid-Ocean ridges
4. Dome Mountains - An unusual type that is formed when
molten rock rises but does not break through the surface.
Ex. Adirondacks, NY

Mountain building ppt nc 13

  • 1.
    Mrs. Z’s MountainBuilding notes ONLY! Mountain Building
  • 2.
    Rock Deformation AKA– Mountain Building • Deformation - the bending, breaking, and tilting of the earth’s crust. • Three types of Stress: 1. Compressional   2. Tensional   3. Shear 
  • 3.
    FOLDING - flatlayers of rock are under severe compression and are squeezed from the sides. The layers moved into folded positions without breaking (although some cracks may appear).
  • 4.
     Three typesof Folds: 1. Anticlines - upward folds 2. Synclines – downward folds 3. Monoclines – gently dipping bends in horizontal rock layershttp://www.cr.nps.gov/history/online_books/geology/publications/bul/1508/images/fig27.jpg
  • 5.
    Features formed bytectonic activity Normal 1. Faults - A break in the rock layers along which there is no movement is called a fracture. Once movement occurs, the fracture is known as a fault. Three Main Types of Faults:
  • 6.
     2. ReverseFault • occurs along convergent boundaries (compression force) • The hanging wall moves up above the foot wall  Thrust Fault o reverse fault where the hanging wall is pushed at such a low angle (not steep) that it moves UP AND OVER the foot wall
  • 7.
     3. Strike-SlipFault • occurs at transform boundaries (shearing force) • The rocks along either side of the fault slide horizontally  Ex. San Andreas Fault
  • 8.
  • 9.
    Four Types ofMountains 1. Folded Mountains - Found where continents have collided. Ex. Appalachian Mts., Himalayan Mts. • Plateaus - areas of flat-topped land high above sea level. Ex. Colorado Plateau (Grand Canyon) 2. Fault-Block Mountains - Formed by faults, where part of the earth’s crust have been broken into large blocks and then were lifted above the surrounding crust. Ex. Grand Teton, MT
  • 10.
    3. Volcanic Mountains- Form when molten rock erupts onto earth’s surface. Ex. Cascade Mts. in Pacific NW and the mid-Ocean ridges 4. Dome Mountains - An unusual type that is formed when molten rock rises but does not break through the surface. Ex. Adirondacks, NY