landform geography earthquakes and volcanoes july 9, 2013

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Landform Geography Earthquakes and Volcanoes July 9, 2013

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Page 1: Landform Geography Earthquakes and Volcanoes July 9, 2013

Landform Geography

Earthquakes and VolcanoesJuly 9, 2013

Page 2: Landform Geography Earthquakes and Volcanoes July 9, 2013

Earthquakes

• Sudden release of tectonic stress creates movement in Earth’s crust & shockwaves through lithosphere

Page 3: Landform Geography Earthquakes and Volcanoes July 9, 2013

Earthquake Processes

Page 4: Landform Geography Earthquakes and Volcanoes July 9, 2013

Earthquake Energy• Waves released by an earthquake:

– P-waves – primary, compressional waves that travel 1.5-8 km/sec

– S-waves – secondary, vertical waves that travel 60-70% slower than P waves

Page 5: Landform Geography Earthquakes and Volcanoes July 9, 2013

Triangulation to Locate ‘QuakeKnown distance to stations A, B and C shows location of epicenter

Page 6: Landform Geography Earthquakes and Volcanoes July 9, 2013

Measuring Earthquakes• Richter Scale – logarithmic measure where

each whole number represents 10X the shaking of the next smaller number

Page 7: Landform Geography Earthquakes and Volcanoes July 9, 2013

Faulting• Earthquakes occur along faults – cracks in

Earth’s crust where rocks or plates are displaced

• Fault Types:– Normal –

– Reverse –

– Strike-Slip –

– Overthrust –

Page 8: Landform Geography Earthquakes and Volcanoes July 9, 2013

Normal Fault

Page 9: Landform Geography Earthquakes and Volcanoes July 9, 2013

Reverse Fault

Page 10: Landform Geography Earthquakes and Volcanoes July 9, 2013

Strike-slip Fault

Page 11: Landform Geography Earthquakes and Volcanoes July 9, 2013

San Andreas Fault(Transform Fault)

Movement

Movement

Page 12: Landform Geography Earthquakes and Volcanoes July 9, 2013

Overthrust fault

Page 13: Landform Geography Earthquakes and Volcanoes July 9, 2013

1886 Charleston Earthquake

Page 14: Landform Geography Earthquakes and Volcanoes July 9, 2013

Volcanoes

• Mts or hills w/ a conduit down into upper mantle through which magma, ash & gases are ejected

• 3 basic types:– Cinder-cone Volcanoes– Composite (strato) Volcanoes– Shield Volcanoes

Page 15: Landform Geography Earthquakes and Volcanoes July 9, 2013

• Where to find volcanoes– Subduction zones, Sea-floor spreading, and Hot spots

Page 16: Landform Geography Earthquakes and Volcanoes July 9, 2013

Cinder-Cone Volcanoes• Small, steep-sided

volcano made of magma fragments & rock debris from central vent

Page 17: Landform Geography Earthquakes and Volcanoes July 9, 2013

Composite Volcanoes• Large, steep-sided volcano built up by layers of lava &

rock debris – over subduction zones – viscous, silicate magma - explosive eruptions

Cross Section Mt. Fuji

Page 18: Landform Geography Earthquakes and Volcanoes July 9, 2013

Pacific “Ring of Fire”• Concentration of composite volcanoes around the

Pacific Basin over subduction zones

Page 19: Landform Geography Earthquakes and Volcanoes July 9, 2013

Shield and Composite Volcanoes

Mauna Loa, Hawaii

Page 20: Landform Geography Earthquakes and Volcanoes July 9, 2013

Shield Volcanoes• Broad, gentle-sided volcanoes formed from low-

silica, low-viscosity magma – lava flows cool & harden to become basalt

Page 21: Landform Geography Earthquakes and Volcanoes July 9, 2013

Volcanic Output

• Volcanic ash consists of powder-size to sand-size particles of igneous rock material that have been blown into the air by an erupting volcano.

• An ash field is a geographic area where the ground has been blanketed by the fallout of an ash plume.

• Silicosis

• Dry ash weighs about ten times the density of fresh snow

Page 22: Landform Geography Earthquakes and Volcanoes July 9, 2013

Volcanic Ash

Page 23: Landform Geography Earthquakes and Volcanoes July 9, 2013

Volcanic Lightning

• Volcanoes produce 2 kinds of lightning:– First occurs in the smoke– The second is produced by the mouth of the

volcano

• Not all volcanoes produce lightning

Page 24: Landform Geography Earthquakes and Volcanoes July 9, 2013

Hot Spots• Stationary points in asthenosphere from which a

magma plume intermittently pushes through the crust above

• Plates move over hot spots, carrying deposits of basalt with them

• Hawaii (& the Emperor Seamount Chain) & Yellowstone have been shaped by hotspots

Page 25: Landform Geography Earthquakes and Volcanoes July 9, 2013

Formation of HawaiiEmperor Seamount Chain70 M yrs old – Pac. Plate

1st moved North, then NW

HawaiiKauai Oldest – Big Island (Hawaii) still over hot spot

70 mya

Present

Page 26: Landform Geography Earthquakes and Volcanoes July 9, 2013

Hot Spot Tracks

Page 27: Landform Geography Earthquakes and Volcanoes July 9, 2013

Yellowstone Hot SpotNorth American Plate has moved west, then northwest over past

16.5 M yrs

Calderas from eruptionsin past 2 M yrs

Page 28: Landform Geography Earthquakes and Volcanoes July 9, 2013

Supervolcano• A supervolcano is an eruption that rates a magnitude

of 8 on the Volcanic Explosivity Index. • The VEI is a scale that rates eruptions on their ejected

volume, plume height and duration. The scale ranges from 0 through 8.

• Only a few dozen eruptions in all of Earth's history are known to have a VEI of 8.

• Two of those eruptions, the Lava Creek eruption (640,000 years ago) and the Huckleberry Ridge eruption (2.2 million years ago), occurred at Yellowstone.

• These eruptions were given the VEI rating because their ejected volume exceeded 1000 cubic kilometers

Page 29: Landform Geography Earthquakes and Volcanoes July 9, 2013

Geyser Cross Section

Page 30: Landform Geography Earthquakes and Volcanoes July 9, 2013

Calderas• Large depression formed when a volcanic

mountain collapses after erupting

Crater Lake, Oregon