Download VOLCANOES - Rocky River

Survey
yes no Was this document useful for you?
   Thank you for your participation!

* Your assessment is very important for improving the work of artificial intelligence, which forms the content of this project

Document related concepts
no text concepts found
Transcript
VOLCANOES
21.2
What is a volcano?
• Volcano: opening in the Earth’s crust where
magma erupts onto the surface
• Magma: molten rock underground
• Lava: magma that has reached Earth’s
surface
How Does A Volcano Form?

Under certain conditions, small amounts of
mantle rock can melt, forming liquid
magma. The magma rises upward through
the crust, erupting at the surface as a
volcano.
Structure of a Volcano
3 Factors That Determine the
Viscosity of Magma:
1. Temperature – the higher the
temperature, the lower the viscosity
 2. Water Content – the more water, the
lower the viscosity
 3. Silica Content – the higher the silica
content, the higher the viscosity. Silica acts
like glue.

TYPES OF LAVA


Felsic
- high silica content
- light colored
- slow moving
- explosive eruptions
Mafic
- low silica content
- dark colored
- fast flowing lava
- quiet eruptions
LAVA FRAGMENTS

Tephra: solid fragments of lava
- ash: less than 2mm diameter
- lapilli: 2 – 64mm diameter
- bombs: 64mm or higher diameter
Ash
Lapilli
Bombs
OTHER LAVA FRAGMENTS

aa – broken, sharp
blocks of lava

Pahoehoe – smooth,
wrinkled lava
VOLCANO ZONES
Pacific Ring of Fire
- zone around the Pacific Ocean
- most active area of volcanoes in World
 Mid-Ocean Ridges
- zone along divergent plates
 Eurasian Belt
- zone along south border of Eurasian plate

Hot Spots
A hot spot is a region where hot rock extends
deep within the mantle to the surface.
 Example: Hawaii

3 TYPES OF VOLCANOES
1. CINDER CONE
Steep sides
 Smallest, most abundant
 Active for a short time, then become
dormant

2. COMPOSITE
Consists of alternating layers of ash,
cinders, and lava
 Steep sides
 Thick magma
 Lot of gases

3. SHIELD
Consists of layers of mafic lava
 Gently sloping sides, wide base

FAMOUS ERUPTIONS
Vesuvius, Italy – 79 A.D.
 Krakatau, Indonesia – 1883
 Mount St.Helens, U.S. – 1980
 Mt. Pinatubo, Phillipines – 1992
 Eyjafjallajökull volcano in Iceland – April,
2010

Mt. Vesuvius
Mt. Krakatau
1883
Mt. St.Helens
1980
BEFORE
AFTER
Mt.Pinatubo
1992
Mt.Kilaeau
Present
VOLCANOES IN OUTER
SPACE
The Moon – no volcanoes
 Mars
- Olympus Mons
- 3 times higher than Mt.Everest
 Io
- Moon of Jupiter
- volcanic activity

Related documents