• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/77

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

77 Cards in this Set

  • Front
  • Back
  • 3rd side (hint)

fragmented volcanic rocks ejected upwards explosively

Pyroclasts

Molten rock inside earth

Magma

magma that teaches the surface

Lava/pyroclasts

Minerals with Si and O

Silica

50% silica -> low silica

Mafic

Ex. Basalts (dark, dense rocks)

70% silica -> high silica, high amounts of gases

Felsic

Ex. Quartz, feldspar, Rhyolites (light less dense rocks)

60% silica

Intermediate

Ex. Andesites -> most abundant

- Resistance to flow


- controlled by silica content and temperature

Viscosity

Silica - poor, hot, low viscosity

Mafic magmas

Silica rich, cooler, high viscosity

Felsic and Intermediate magmas

H2o , Co2, So2, N2, CI2, CH4

Volcanic Gases (volatiles)

Driving force of eruptions

Exsolve

“River” of Co2 about 50 M thick

Lake Nyos

Low silica, hot, therefore low viscosity, gases escape

Mafic Magmas

fluid lava flows

High Silica, cooler, therefore high viscosity, gases trapped

Felsic/Intermediate Magmas

explosive, eruptions -> pyroclastics

pressure decreases

Mid-ocean ridges

water added

subduction zones

heat added

hot spots

- broad dome, gentle slope, largest


- comp->basaltic lava flows

Shield volcano

Ex. hawaii iceland

- Steep, tall; layered


- pyroclastic flow


- comp -> mostly andesite

Composite/ Strato Volcano

Ex. Mt saint helens

- Steep, small, short-lived


- comp -> andesitic basaltic pyroclasts

Cinder Cone

Powerful, Vertical ejection of pyroclasts, gas, most explosive


VEI = 3-8

Plinian

Fluid basaltic lava flows, least explosive


VEI = 0-1

Hawaiian

Small eruption of pyroclasts


VEI = 1-3

Strombolian

Giant collapse caldera: hot spot

Yellowstone

Shield volcanoes active in hawaii

kilauea


mauna loa

2 deadliest volcanic hazards

Pyroclastic flows and Volcanjc Mudflows

follows explosive eruption

column collapse

follows collapse of dome

dome collapse

rapid flood of pyroclasts and water

Volcanic Mudflow

causes of volcanic mudflow

- rainfall on loose ash


- melting of snow and ice


-breakout of a crater lake, rivers, and lakes

Juan de fuca plate is a ______ boundary

cascadia subduction zone

Atlantic sea floor under Caribbean

Mt Pelee 1902 caribbean

precursors: earthquakes, ash eruptions


St. Pierre - elections


3 days before - invasion of red ants, snakes, and centipedes

Mt Pelee caribbean

precursors: earthquakes, ash eruptions


St. Pierre - elections


3 days before - invasion of red ants, snakes, and centipedes

Mt Pelee caribbean

what kind of eruption was mt pelee how many deaths

pyroclastic flows, death toll: 30,000 2 survivors

One of the survivors from mt pelee due to being in jail cell

Louis-Auguste Cyparis

Nevado del Ruiz 1985 colombia under what plates

Nazca under South American plate

Precursors: steam eruptions, earthquakes, no evacuations, Lahars

Nevado del Ruiz, Colombia

Nevado del Ruiz, Colombia death toll

25,000

Nevado del Ruiz, Colombia death toll

25,000

what plates is Vesuvius 79 CE Italy

Mediterranian seafloor under Europe

Nevado del Ruiz, Colombia death toll

25,000

what plates is Vesuvius 79 CE Italy

Mediterranian seafloor under Europe

what the cities of pompeii and herculaneum buried

pumice and ash fall


pyroclastic flows - most deaths

the main cause of landslides

gravity and friction

the main cause of landslides

gravity and friction

downslope movement under the influence of gravity of rock/soil/sed

Mass wasting

factors in mass wasting

1. water content


2. slope angle


3. geological


4. human


5. vegetation

factors in mass wasting

1. water content


2. slope angle


3. geological


4. human


5. vegetation

excess water increases slope failures

water content

factors in mass wasting

1. water content


2. slope angle


3. geological


4. human


5. vegetation

excess water increases slope failures

water content

steep slopes increase slope failures

slope angle

factors in mass wasting

1. water content


2. slope angle


3. geological


4. human


5. vegetation

excess water increases slope failures

water content

steep slopes increase slope failures

slope angle

tilt rock layers, types of rocks, clay

geological

overloading of slopes, artificial fill, excavation of highways, deforestation

Human

overloading of slopes, artificial fill, excavation of highways, deforestation

Human

DECREASES slope failures, reduce the amount of water in the soil

vegetation

types of mass wasting

Rockfall, Rockslide, flows

types of mass wasting

Rockfall, Rockslide, flows

free fall of rocks - very rapid common in mountainous areas

Rockfall

movement of rock layers down a failure surface


typically with sedimentary rock


everything slides down at the same time

rockslide

movement as a viscous fluid

flows

movement as a viscous fluid

flows

rockslide type- curved surface, weak sediments, small

slump rotational slide

Rockslide- planar surface, more coherent, deadlier

transitional slide

Rockslide- planar surface, more coherent, deadlier

transitional slide

Type of flow - most fluid; heavy rainstorms

Mudflow

Type of flow- largest, fastest, very deadly, rare

Debris flow- avalanche

Type of flows- volcanic mud/debris flow

Lahar

Type of flows- volcanic mud/debris flow

Lahar

type of flow- slowest most widespread

Creep

Triggering events

Rainstorms, earthquakes, volcanoes

when wave energy undercuts the cliffs and makes the recede backwards

coastal erosion and collapse