Midterm 2- Dynamic Earth Flashcards
Cross section of a stream and velocity
The deepest part of the stream has the highest velocity.
Outer vs inner portion of a meandering stream
Outer parts of meander:
→ velocity is highest
→ erosion
→ cutbank
Inner meander bends :
→ velocity is low
→ deposition
→ point bars
Liquefaction
Loosely packed, water-logged sediments at or near the ground surface lose their strength in response to strong ground shaking. Causes major subsidence, fracturing, and horizontal sliding of the ground surface
Describe the process that causes a nonconformity
Occurs where rocks that formed deep in
Earth are overlain by sedimentary rocks
formed at the Earth’s surface. Indicates that all the rocks overlying the metamorphic or
igneous rocks have been removed by
uplift and erosion.
Hanging valley
formed when the main glaciers cut deeper than side tributaries
Kame
Hills formed by sediment deposition
in/on ice – left after the glacier melts
earthquakes that follow the largest shock of an earthquake sequence
Aftershock
Glacial erosion and deposition
Glaciers move, pick up & transport
rocks and Glaciers transport material and melt
Amplification of seismic waves
Soft sediments amplify seismic vibrations increasing damages
sheets of floating ice attached to land usually occupy coastal embayments
Ice shelves
Surface faulting
Displacement that reaches the Earth’s
surface during slip along a fault.
* Commonly occurs with shallow
earthquakes (epicenter <20 km.)
* May accompany aseismic creep or
natural or man‐induced subsidence
Shallow Earthquakes
Form through tension and normal faulting at divergent boundaries; strike-slip at transform faults
The four wave types
A)Body waves
1)P waves
2)S waves
B)Surface waves
3)Love wave
4)Reighleigh wave
the degree of earthquake shaking at a given locale based on the amount of damage
Intensity
Types of stream deposition features
1)Flood plains
2)Terrances
3)Alluvial fans
4)Deltas
Horizontal fold
is a special type of fold in which both limbs are parallel but offset to each other. The limbs are horizontal, or nearly so.
Ground failure
The term ground failure is a general reference to landslides, liquefaction, lateral spreads, and any other consequence of shaking that affects the stability of the ground.
Graded profile
a smooth concave profile which is steep as the source(high erosion) and gentle at the mouth (high deposition)
Terrances
when streams carve downward into their floodplains, leaving discontinuous remnants of older floodplain surfaces as step-like benches along the sides of the valley
Anatomy of a delta
1)Topset beds- at the very surface of the delta and sit on the foreset beds
2)Foreset beds- sit under the topset bed and form a slope towards the bottomset bed
3)Bottomset beds-lowest bed at the bottom of the body of water, made from the progradation of the foreset bed
Continental glacier
Glaciers much larger than Alpine glaciers that cover entire land masses
Moraine formed as the ridge of till at front of a stable glacier
End moraine
Flashflood
A flood caused by heavy or excessive rainfall in a short period of time
a mountain glacier whose flow is confined by valley walls, forms a U shape
Valley glacier
Plucking
Water seeps into cracks, freezes, and mechanically breaks up the bedrock.
These fragments are plucked out by glacier.Rock fragments dragged
along the base of the glacier.
Fold types
1)Syncline
2)Anitcline
3)Horizontal fold
4)Plunging fold
Describe the process that causes an angular unconformity
1)Sediments are accumulated in a bed
2)Later tectonic forces cause uplifting, folding, and deformation of sedimentary layers during mountain building
3)Erosion strips away the top layers leaving an uneven plain with exposed folded portions
4)Subsidence below the sea allows for new deposits on formerly eroded surface. The surface layer where the new sediments meet preserves an angular unconformity
Two methods to determine age of strata
1)Relative age and dating which places rocks and events in formation sequence
2)Radiometric age specifies the actual number of years that have passed since an event
occurred using radioactive decay
Crevases
Brittle surface fissures that form over lower plastic flow
Strike
measured compass
direction of a line produced
from the intersection of a
horizontal plane with an
inclined rock plane.
Columnar jointing
a geological structure where sets of intersecting closely spaced fractures, referred to as joints, result in the formation of a regular array of polygonal prisms, or columns. often seen in thick lava flows, is a result of cooling and contraction of lava.
Evidence for Continental drift
1)Geographic fit of continents
2)Fossil evidence range overlap
3)Fold belts
4)Glaciations & Palaeoclimates
Phanerozoic Eon
last 570 million years,Pangea fully assembled and results in the Permian
Mass Extinction Event
Turbulent flow
Molecules travel in complex paths
leading to mixing! Can keep
sediment in suspension and Helps erosion
The P-wave shadow
because of the existence of the liquid outer core. When the P-waves enter the liquid core, they are refracted, or bent, away from their original path. This leaves a region where the P-waves do not travel
factors that determine laminar or turbulent flow
1)velocity (rate of movement)
2)geometry (primarily its depth)
3)viscosity (higher viscosity → greater tendency for laminar flow)
the blocks of continental fragments and oceanic islands that have collided with a continent and are now permanently attached
Accreted Terrane margins
Lehmann Discontinuity
The Lehmann discontinuity is an abrupt increase of P-wave and S-wave velocities at the depth of 220 km in Earth’s mantle. P waves slow and S waves dissapear in the liquid outer core. P waves speed up when hitting the solid inner core
relatively smaller earthquakes that precede the largest earthquake in a series
Foreshock
Moraine formed from tributary
glaciers joining
Medial moraine
For each increase in magnitude, the energy released increases ~ 31.6 times
Frequency and magnitude scale
made of sediment that slowly builds up directly underneath a glacier by tiny streams, or as the result of a glacier meeting hills and valleys in the natural landscape, left as a remnant of a retreating glacier
Ground moraine
Stratigraphic Superposition
In any undisturbed stratigraphic sequence, the oldest layers are at the bottom of the sequence, and the youngest units are at the top
a glacier, a thick layer of ice and snow, that covers fewer than 50,000 square kilometers
Ice caps
Horn
Peak that forms when 3 or more cirques meet, forms a distinct triangular shape
Epicenter
point on Earth’s surface directly above the focus
Developed using California buildings as its standard Rates from I (not felt) to XII (total damage)
Modified Mercalli Intensity Scale
a planar zone of seismicity corresponding with the down-going slab in a subduction zone
Wadati-Benioff Zone
Braided stream
Highly variable discharge and flow
volume. Lots of sediment in stream,
Flows around islands & bars
formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock forming
steep-sided inlets to sea
Fjord glacier
Till
unsorted random mix of rocks deposited by glaciers that are
10-100’s m thick – “rock flour”
Structure of geologic time from largest to smallest
1)Eon→ large period of time
2)Era
3)Period
4)Epoch → small period of time
Sea floor spreading evidence
1) Symmetrical Magnetic field reversals
2)New sea floor rock being formed at the ridges
Earliest evidence of life:
stromatolite mounds
3.8 billion years ago
What does this symbol mean
Represents and inclined bed
Original Horizontality
Sedimentary rock layers, or strata were originally deposited as relatively horizontal sheets of sediment. This means that strata that do not retain their original horizontality have
been displaced by movements of the Earth’s crust.
Moraines
material left behind by a moving glacier
-Based on the amplitude of the ground
movement caused by seismic wave
– Accounts for the decrease in wave
amplitude with increased distance
– Mainly for local/nearby earthquakes
Richter scale
Elastic rebound
When a fault is stuck during a movement an excess of energy is stored in the rock, when the force is great enough to break elastic energy is released
Massive erosive force transporting high volumes of sediment downwards and is a major source of water on earth
Streams
Cretaceous Mass Extinction Event
Around 65 million years ago, asteroid impact and resulting climate change caused a mass extinction
Budget
Balance between accumulation
at upper end & ablation at lower end
Hanging wall vs Foot
Hanging wall is the one in movement
Plate boundary types
1)Divergent boundary
2)Convergent boundary
3)Transform fault plane
Location of mid ocean ridges
Mid-Atlantic
East Pacific
Mid-Indian
Iceland Ridge
How did we determine the age of the earth?
Assuming that the earth formed around the same time as the universe we can use meteorite samples to estimate the creation of earth. Since the earth is continuously moving it can be assumed that most of the original rock has been eroded or recycled.
Dating with carbon-14
Half-life of only 5730 years so used to date
very recent events. C-14 is produced in
the upper atmosphere but must be done on organic material
Continental drift
Theory proposed by Alfred Wegener which proposed the super continent Pangea
To better estimate the size of very large earthquakes uses a scale Derived from the amount of displacement along a fault
Moment magnitude scale
Erratics
chunks of rocks transported over long distances by glaciers. When they drop these rocks, they are often far from their origin painting a story of the glaciers path
Anticline
a structural trap formed by the folding of rock strata into an arch-like shape. The rock layers in an anticlinal trap were originally laid down horizontally and then earth movement caused it to fold into an upward arch-like shape
Hydrologic Cycle
the continuous circulation of water in the Earth-Atmosphere system between the ocean,atmosphere, and crust.
highly concentrated combined flow of fluid and sediments under high shear stress in the swash zone, forms small channels
Sheet flow
Fold geometries
1)Symetrical fold
2)Asymetrical fold
3)Overturned fold
4)Recumbant fold