geog 3251: mountain geog, summer 2010 adina racoviteanu

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GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

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Page 1: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

GEOG 3251: Mountain Geog, summer 2010Adina Racoviteanu

Page 2: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Objectives

• Describe types of mountain hazards

• Relate earthquake activity to plate tectonics Define earthquake, focus and epicenter, types of waves

• Define landslides, lahars, mudslides

Page 3: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

1.What is an earthquake?

• Earthquake = Vibration of the Earth produced by the rapid release of energy

• Seismic waves = Energy moving outward from the focus of an earthquake

Page 4: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Why do earthquakes occur?

• Fractures, faults

• Energy released

and propagates in all directions as seismic waves causing

earthquakes

Focus = location of initial slip on the fault; where the earthquake originates

Epicenter = spot on Earth’s surface directly

above the focus

Page 5: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Where do earthquakes occur?

1) Most earthquakes (90%) occur along the edge of oceanic and continental plates

2) Some along faults:

normal, reverse, transform

Page 6: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Seismic waves: forms• P-waves:

– compressional, or push-pull waves– Propagate parralel to the direction in which the wave is moving– Move through solids, liquids

• S-waves:– Called shear waves– Propagate the movement perpendicular to the direction in which the wave ismoving

• Surface waves (L-waves or long waves).– Complex motion– Up-and-down and side-to-side– Slowest– Most damage to structures, buildings

Page 7: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Earthquake size: two ways to measure

1) Magnitude: Richter Scale

2) Intensity: Mercalli Scale

Page 8: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

1) Richter Scale

• Measures the energy released by fault movement

• related to the maximum amplitude of the S wave measured from the seismogram

• Logarithmic-scale

56

31.5 times energy

7

992 times more energy!!

Page 9: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Frequency of Occurrence of Earthquakes

Descriptor Magnitude Average Annually

Great 8 and higher 1 ¹

Major 7 - 7.9 17 ²

Strong 6 - 6.9 134 ²

Moderate 5 - 5.9 1319 ²

Light 4 - 4.9 13,000

(estimated)

Minor 3 - 3.9 130,000

(estimated)

Very Minor 2 - 2.9 1,300,000

(estimated)

¹ Based on observations since 1900. ² Based on observations since 1990.

Page 10: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Recent Earthquake Activity around the World

Page 11: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Largest earthquake in the world

Chile : May 22, 1960 Magnitude 9.5

•More than 2,000 killed, 3,000 injured, 2,000,000 homeless, and $550 million damage in southern Chile• tsunami caused 61 deaths•$75 million damage in Hawaii;• 138 deaths and $50 million damage in Japan; •32 dead and missing in the Philippines; and $500,000 damage to the west coast of the United States.

Page 12: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Most Destructive Known Earthquakes on Record in the World

Date Location Deaths Magnitude Comments

May 31, 1970 Peru 66,000 7.9 $530,000,000damage, great rockslide, floods.

July 27, 1976 China, Tangshan

255,000(official)

7.5 Estimated death toll as high as 655,000.

Sept 19, 1985 MexicoMichoacan

9500(official)

8.0   Estimated death toll as high as 30,000Old lake bed magnified shock waves by 500%

2001 Jan 26 India 20,023 7.7 166,836 injured,

600,000 homeless

.

2004 Dec 26 Sumatra 283,106 9.0 Deaths from earthquake and tsunami

Page 13: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

India, Gujarat earthquakeJan 26, 2001

Page 14: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Same year…Arequipa. S.PeruJune 2001

Page 15: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Jun 23, 2001 Magnitude 8.1 earthquake strikes

Arequipa

Page 16: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Earthquake damage

• Ground Failure - constructions collapse

• Fires - from broken gas and electrical lines

• Landslides - EQ's triggered; occur in hilly/mountainous areas.

• Liquefaction - water-saturated, unconsolidated materials flow

• Tsunami (seismic sea waves; "tidal" waves) - can grow up to 65 m

Page 17: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Landslides

Source: National Geophysical Data Center

Turnnagin Heights,Alaska,1964

Page 18: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Natural disasters in the Cordillera Blanca, Peru:

Huascaran avalanche

Page 19: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Favoring conditions

• Major tectonic faults that are active

• Marked glacierization

• Geologically young, steep mountains

• Pro-glacial lakes

• Immediate vicinity of human settlements

Page 20: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Mass wasting: types

• Creep

• Landslides: rock slides

• Flows: avalanches, debris flow, mud flow

• Rock falls

Page 21: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Common mountain hazards

Page 22: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu
Page 23: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Pokhara, Nepal(base of the Annapurnas)

Page 24: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Lahars= debris flows associated with volcanic eruptions

Page 25: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Landslide and Debris Flow (Mudslides):

• masses of rock, earth, or debris saturated with water and moving down a slope

• They are activated by:

storms,

earthquakes,

volcanic eruptions,

fires,

alternate freezing or thawing,

steepening of slopes by erosion or human modification.

Page 26: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Avalanche:

– similar in mechanism to landslide

– it involves a large amount of ice, snow and rock falling quickly down the side of a mountain

– ice builds in cornices or forms over a weaker layer of snow, creating the danger of an avalanche.

Page 27: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

ALPAMAYO

Nev. Chacraraju

Page 28: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Mt. HUASCARAN, PERU

Page 29: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

1962 HUASCARAN AVY

• Large snow year

• 50 degree F increase in temp over a few minutes

• Caused avalanche

• 4,000 fatalities

Page 30: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

1970 Avalanche

• Triggered by 7.7 magnitude earthquake

• Rock face failure

• Incorporated 30 meters of snow and ice!

• Moraines confined flow initially

• Accelerated over a distance of 2.4 km

• Became airborne at change of slope

Page 31: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu
Page 32: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Landslides: May 30, 1970 Peru disaster

Magnitude: 7.9

•A large mass of ice and rock slid from a vertical face on Nevado Huascaran, the highest peak in Peru

•Debris reached a velocity of 280 km/hr

•traveled 11 km horizontally in about 4 minutes at a mean velocity of 165 km/hr.

•Buried the towns of Yungay and Ranrahirca, The death toll in both villages was 20,000.

Page 33: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

1970 Earthquake that caused the Huascaran disaster killed about 40,000 people in Huaraz.

Streets of Huaraz after the1970 Earthquake.

Adobe houses collapsed, killing people inside.

Page 34: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

The town of Huaraz flattened

Page 35: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Huaraz today: a growing tourist town

Page 36: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu
Page 37: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Rock avalanche deposit

Debris flowdeposit

Page 38: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu
Page 39: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu
Page 40: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Yungay is now completely abandoned. Cemetery has a monument to the dead.

Page 41: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu
Page 42: GEOG 3251: Mountain Geog, summer 2010 Adina Racoviteanu

Tomorrow’s lecture: Human sacrifice

•Highly worshipped mountain;

•stratovolcano

•Coropuna is believed to contain Inca ruins and human sacrifices offered to the mountain deity.