Chapter 7 - Sediment and Sedimentary Rocks Flashcards
Name the types of Physical erosion accompanying or following weathering, and what they create
Rill erosion - shallow rivulets
Incision - ravines, gullies
Washout - spires, pillars, arches, hoodoos
Mass Wasting - slumps, falls, slides
What is rill erosion, and what does it create?
Type of physical erosion.
- erosion by a heavy rainfall, and then water draining off. Creating a narrow rivulet (narrow little stream)
- creates shallow rivulets
What is an incision and what does it create?
Type of physical erosion
- a cut into a surface
- creates ravines, gullies
Incisions + washouts create canyons
What is a washout and what does it create?
Type of physical erosion
- creates spires (individual column of rocks that are separated from other rocks)
- rainfall that is more or less vertical washes it out, and then the big boulders act as roofs and prevent further erosion, leaving only a column there
- east of drumhellar and yoho national park you find these
- washouts also create hoodoos pillars and arches
Difference beteen hoodoos and spires?
Spires are a column of rock with constant thickness separated from other rock due to washout, and hoodies are the same but have variable thickness
What happens when incisions combine with washouts?
- you get canyons
- ex) grand canyon
1) What is shear strength:
With respect to rocks;
2) What does shear strength depend on?
1) You must overcome shear strength cause slope failure
2) Shear strength depends on
- slope
- friction/cohesion
- external support
With respect to rocks;
What are the most common causes of slope failure in
a) poorly consilidated material
b)hard bedrock
Most common causes of slope failure are:
- in poorply consolidated material: rain
- in hard rock: bedding relative to slope, fractures (more parallel bedding to slope = more chance of slope failure)
- insufficient external support
Explain the slumping in the Pacific Palisades in southern california
-Undercutting of steep sea cliffs by wave action resulted in massive slumping in the pacific palisades area of souther california
What is the most common cause of slope failure in unconsolidated material?
Most common causes of slope failure is rainfall on a poorly consolidated material (not hard rock)
- rain comes in and lubricates the grains between them
- common when slope of underlying material is parallel to the entire landscape
- so if bedding is not parallel to slope, its harder to cause this kind of slope failure
4 types of soil creep are:
- Land slides (mudslide / earthflow)
- Slump
- Rock slides
- Steep cliff
Describe land slides
MASS WASTING
land slides / mud slide / earth flow
-after heavy rain, a chunk of soil just moves uniformly and slides down the slope
Describe slumping
MASS WASTING
In a slump, material moves downward along the cuved surface of a rupture(concave), causing the slump block to rotate backward.
-Most slumps involve unconsolidated or weakly consolidated material and are typically caused by erosion along the slope’s base
-When there is a pre-existing slope that is very steep, a homogeneous material detachees along one or more CONCAVE
-figure 11.9 is very helpful
Describe rock slides, and explain the difference between rock slide and a land slide
MASS WASTING
- rock slide: large rocks are parallel to bedding planes, and an entire chunk/slab just slides down parallel to slope
- land slide occurs after a heavy rain, and a chunk of soil just moves uniformly down the slope
Describe a Rock-fall.
MASS WASTING
Rockfalls result from failure along cracks, fractures, or bedding planes in the bedrock and are common features in the areas of steep cliffs
-occured in frank slide
-rock fall and roll, big boulders kinda just rolled off the hill
