Thermochemistry Heats of Formation and Calculating Heats of Reaction.
Chapter 7 Sections 3 & 4 Volcanic Eruptions As magma heats up it becomes LESS dense and flows...
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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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/1.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/2.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/3.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/4.jpg)
![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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/5.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/6.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/7.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/8.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/9.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/10.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/11.jpg)
Edge of a pyroclastic flow
![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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/13.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/14.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/15.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/16.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/17.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/18.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/19.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/20.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/21.jpg)
![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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/22.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/23.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/24.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/25.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/26.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/27.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/28.jpg)
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.](https://reader036.fdocuments.in/reader036/viewer/2022062407/56649d9e5503460f94a89219/html5/thumbnails/29.jpg)
GEYSERS (New Zealand)