63
Igneous Structures: Volcanic

Igneous Structures: Volcanic

  • Upload
    sofia

  • View
    24

  • Download
    0

Embed Size (px)

DESCRIPTION

Igneous Structures: Volcanic. Viscosity. Units: pascal-seconds (kg/m-sec) How many pascals pressure x how many seconds to squash fluid flat? Viscous: Material flows as long as pressure is applied, however small Pseudoviscous: Material flows after some threshold stress. - PowerPoint PPT Presentation

Citation preview

Page 1: Igneous Structures: Volcanic

Igneous Structures: Volcanic

Page 2: Igneous Structures: Volcanic

Viscosity

• Units: pascal-seconds (kg/m-sec)• How many pascals pressure x how many

seconds to squash fluid flat?• Viscous: Material flows as long as pressure is

applied, however small• Pseudoviscous: Material flows after some

threshold stress

Page 3: Igneous Structures: Volcanic

Viscosity of Common Materials

Material Viscosity Pa-Sec

Hydrogen gas, 15 degrees K 0.0000006 (6 x 10-7)

Air, 0 degrees C 0.000017 (1.7 x 10-5)

Liquid Hydrogen 0.00001 (10-5)

Water 0 degrees C 0.0018 (1.8 x 10-3)

Water 100 degrees C 0.0003 (3 x 10-4)

Heavy Machine Oil 15 C 0.66

Glycerin, 20 degrees C 1.5

Honey 20 degrees C 1.6

Page 4: Igneous Structures: Volcanic

Geologic Viscosities

Material Viscosity Pa-Sec

Basalt Lava 1000

Rhyolite Lava 1,000,000

Rock Salt 1014 (Pseudoviscous)

Marble 1016

Granite, Quartzite 1018 - 1020

Asthenosphere 1019 - 1020

Deep Mantle 1021 - 1022

Shallow Mantle 1023 - 1024

Page 5: Igneous Structures: Volcanic

What Drives Magma?

• Magma is typically 10% lighter than equivalent solid rock– Why pressure inhibits melting

• Buoyancy drives magma upward– Weight of rock around volcanic conduit > weight

of magma• Gas pressure powers volcanic eruptions• Mafic (dense) rocks can sink in crust by

viscous flow

Page 6: Igneous Structures: Volcanic

Plate Tectonics and Volcanoes

Page 7: Igneous Structures: Volcanic

A Cinder Cone:Wizard Island, Crater Lake, Oregon

Page 8: Igneous Structures: Volcanic

Paricutin, Mexico

1943-1952

Page 9: Igneous Structures: Volcanic

Anatomy of a Cinder Cone, Hawaii

Page 10: Igneous Structures: Volcanic

Tuff Ring: Diamond Head, Hawaii

Page 11: Igneous Structures: Volcanic

Tuff Ring: Diamond Head, Hawaii

Page 12: Igneous Structures: Volcanic

Shield Volcano: Haleakala, Hawaii

Page 13: Igneous Structures: Volcanic

Stromboli

Page 14: Igneous Structures: Volcanic

Mount Lassen and Mount Tehama

Page 15: Igneous Structures: Volcanic

Mount Shasta, California

Page 16: Igneous Structures: Volcanic

Shasta and Shastina

Page 17: Igneous Structures: Volcanic

Shastina and Landslide Deposit

Page 18: Igneous Structures: Volcanic

Mount Shasta and Landslide Deposit

Page 19: Igneous Structures: Volcanic

Mount Saint Helens and Spirit Lake

Page 20: Igneous Structures: Volcanic

May 18, 1980

Page 21: Igneous Structures: Volcanic

The Mountain Collapses

Page 22: Igneous Structures: Volcanic

Mount St. Helens

Page 23: Igneous Structures: Volcanic

Mt. St. Helens

Page 24: Igneous Structures: Volcanic

Bezymianny, Russia

Page 25: Igneous Structures: Volcanic

Lava Dome, California

Page 26: Igneous Structures: Volcanic

Rhyolite Plugs and Pumice Rings

Page 27: Igneous Structures: Volcanic

Rhyolite Plugs and Pumice Ring

Page 28: Igneous Structures: Volcanic

Obsidian Dome, California

Page 29: Igneous Structures: Volcanic

Obsidian

Page 30: Igneous Structures: Volcanic

Rhyolite Plugs and Pumice Rings

Page 31: Igneous Structures: Volcanic

Maar, Nevada

Page 32: Igneous Structures: Volcanic

Volcanic Neck, New Mexico

Page 33: Igneous Structures: Volcanic

Topographic Inversion, Nevada

Page 34: Igneous Structures: Volcanic

How Calderas Form

Page 35: Igneous Structures: Volcanic

Crater Lake, Oregon

Page 36: Igneous Structures: Volcanic

Mount Mazama: After

Page 37: Igneous Structures: Volcanic

Mount Mazama: Before

Page 38: Igneous Structures: Volcanic

Jemez Caldera, New Mexico

Page 39: Igneous Structures: Volcanic

Valles Caldera, New Mexico

Page 40: Igneous Structures: Volcanic

Tuff, Valles Caldera, New Mexico

Page 41: Igneous Structures: Volcanic

Welded Tuff, California

Page 43: Igneous Structures: Volcanic

Santorini (Thera), Greece

Page 44: Igneous Structures: Volcanic

Santorini, Greece

Page 45: Igneous Structures: Volcanic

Santorini, Greece

Page 46: Igneous Structures: Volcanic

Ash Layer, Santorini

Page 47: Igneous Structures: Volcanic

Ash Layers, Santorini

Page 48: Igneous Structures: Volcanic

What Really Destroyed the Minoan Civilization

Page 49: Igneous Structures: Volcanic
Page 50: Igneous Structures: Volcanic

Collapsing Volcanoes - Hawaii

Page 51: Igneous Structures: Volcanic

Molokai Scarp

Page 52: Igneous Structures: Volcanic

Nuuanu Pali, Oahu

Page 53: Igneous Structures: Volcanic

Tambora 1815

1816: “Year Without A Summer”• 100 cubic km of ash erupted• Global sunset color effects for months• New England– Snow in June and August, Frost in July– Exodus to Midwest

• Europe: High prices, food riots

Page 54: Igneous Structures: Volcanic

Tambora

Page 55: Igneous Structures: Volcanic

Long Valley Caldera

Page 56: Igneous Structures: Volcanic

Long Valley Caldera

Page 57: Igneous Structures: Volcanic

Bishop Tuff

Page 58: Igneous Structures: Volcanic

Compaction of Bishop Tuff

Page 59: Igneous Structures: Volcanic

Toba, Sumatra

Page 60: Igneous Structures: Volcanic

Eyjafjallajokull, Iceland

Page 61: Igneous Structures: Volcanic

Flood Basalts, Washington

Page 62: Igneous Structures: Volcanic

Lava “Delta,” Washington

Page 63: Igneous Structures: Volcanic

Columnar Jointing, Washington