Chapter 7 Sections 3 & 4 Volcanic Eruptions As magma heats up it becomes LESS dense and flows...

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VOLCANOES Chapter 7 Sections 3 & 4

Transcript of Chapter 7 Sections 3 & 4 Volcanic Eruptions As magma heats up it becomes LESS dense and flows...

Page 1: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

VOLCANOES

Chapter 7

Sections 3 & 4

Page 2: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Volcanic Eruptions As magma heats up it

becomes LESS dense and flows upwards.

If there is an opening in the crust, it will reach the earth’s surface – a volcano is born!

Page 3: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Inside a volcano

Page 4: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.
Page 5: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

ERUPTIONS As magma rises the pressure surrounding

it decreases. (It is not as deep anymore) This allows gases in and around the magma to expand. These expanding gases push the magma out of the volcano.

Eruptions can spew out

Ash – fine dust specks

Cinders – pebble-sized particles

Bombs – baseball to car sized

pieces!

Page 6: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

ASH CINDERS

BOMBS!

Page 7: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

2 types of eruptions

1) QUIET: magma low in silica; magma flows easily, gases bubble out slowly and gently.

2) EXPLOSIVE: magma high in silica; thick/sticky; doesn’t always flow out of the crater; can plug it like a cork; gases get trapped and build up pressure until they “explode”.

PYROCLASTIC FLOW: when the volcano hurls out a mixture of hot gases, ash, cinders, and bombs.

Page 8: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

QUIET EXPLOSIVE

Page 9: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

SCARY PYROCLASTIC FLOW!

Mt. PinatuboPhilippines

1991 eruption

Page 10: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

More pyroclastic flows

Page 11: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Edge of a pyroclastic flow

Page 12: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Pyroclastic flows cause tremendous damage!

Page 13: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Volcano Hazards Fire Ash can bury towns Landslides Mudslides Flooding (melted

snow)

Page 14: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Stages of Volcanic ActivityVolcanoes are classified

as:

1) ACTIVE – a live volcano that is erupting or will in the near future

2) DORMANT – “sleeping” may erupt again

3) EXTINCT – a dead volcano; unlikely to ever erupt again.

Page 15: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

TYPES OF VOLCANOES

Wide, gently sloping,

usually form at a hot spot,

lava pours out gently

Lava has high

viscosity, steep, cone shaped hill,

more explosive eruptions

Combination of both; sometimes

gently flowing lava, sometimes

explosive, alternating layers of ash/cinders &

lava

Page 16: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Click for the video clip!

Page 17: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Other volcanic landforms

Lava plateau – lava flows out of several long cracks in an area and eventually over hundreds of years build up to form a plateau

Page 18: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Calderas Caldera – huge hole left by the

collapse of volcano

Page 19: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Soils from Lava & AshWhen hardened lava erodes and forms soil,

phosphorous, potassium and other important minerals are released. These make the soil very fertile.

Page 20: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Dikes and SillsWhen magma forces itself across rock

layers it hardens into a DIKE.

When magma squeezes between horizontal layers of rock it forms a SILL.

Page 21: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.
Page 22: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Dikes & Sills in New Zealand

Page 23: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Volcanic NecksForms when magma hardens in the

volcano’s pipe and the softer rock surrounding it erodes away.

Page 24: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Batholiths & Dome Mountains

Batholith: large rock masses form the core of many mtn ranges; formed when a large body of magma cools inside the crust.

Dome Mountain: smaller bodies of hardened magma

Page 25: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Batholiths

Sierra Batholith (Yosemite Nat’l Park)

Page 26: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Dome Mountains

Page 27: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Geothermal Activity Geo – means “earth” Therme – means “heat” Geothermal is heat produced

by the Earth (actually magma!) Hot springs & Geysers are

types of geothermal activity found in volcanic areas.

Page 28: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

Hot Springs

In IDAHO

In ARKANSAS

Page 29: Chapter 7 Sections 3 & 4 Volcanic Eruptions  As magma heats up it becomes LESS dense and flows upwards.  If there is an opening in the crust, it will.

GEYSERS (New Zealand)