Title: VOLCANOES
1VOLCANOES
2What is a Volcano?
- A volcano is an opening, or rupture, in a
planet's surface or crust, which allows hot,
molten rock, ash, and gases to escape from below
the surface. Volcanic activity involving the
extrusion of rock tends to form mountains or
features like mountains over a period of time.
The 25th Anniversary of Mt. St. Helens Eruption.
http//en.wikipedia.org/wiki/Volcano
pun.org/.../2005/05/25th-anniversar.html
3What are the Types?
- 4 Main Types
- 1. A shield volcano has shallow-sloping sides.
Shield volcanoes are formed by lava flows of low
viscosity lava that flows easily. Consequently,
a volcanic mountain having a broad profile is
built up over time by a flow after flow of
relatively fluid basaltic lava issuing from vents
or fissures on the surface of the volcano. - Many of the largest volcanoes on Earth are
shield volcanoes (All of the volcanoes in
Hawaii). - 2. A cinder cone is a steep conical hill
of volcanic fragments that accumulate around and
downhill from a and is usually active in eruption
and is usually termed hot spot. The rock
fragments, often called cinders or scoria, are
glassy and contain numerous gas bubbles "frozen"
into place as magma exploded into the air and
then cooled quickly. Cinder cones range in size
from tens to hundreds of meters tall.
Mt. Presley located in New Avalon library.marist.e
du/.../Mt.20Presley.htm
www.worldbook.com/.../studying_eruptions
www.Wikipedia.com
Kilauea volcano in Hawaii.
4Types Continued
- 3. Composite volcanoes or stratovolcanoes are
typically steep-sided, symmetrical cones of large
dimension built of alternating layers of lava
flows, volcanic ash, cinders, blocks, and bombs
and may rise as much as 8,000 feet above their
bases. Some of the most conspicuous and beautiful
mountains in the world are composite volcanoes,
including Mount Fuji in Japan, Mount Cotopaxi in
Ecuador, Mount Shasta in California, Mount Hood
in Oregon, and Mount St. Helens and Mount Rainier
in Washington. - 4. A lava dome or volcanic dome are formed by
relatively small, bulbous masses of lava too
viscous to flow any great distance consequently,
on extrusion, the lava piles over and around its
vent. A dome grows largely by expansion from
within. As it grows its outer surface cools and
hardens, then shatters, spilling loose fragments
down its sides.
St. Augustine volcano, Alaska.
The Novarupta Dome formed during the 1912
eruption of Katma Volcano, Alaska.
www.educ.uvic.ca/.../438/VOLCANO/COMPOSITE.html
http//pubs.usgs.gov/gip/volc/types.html
5How do they Work?
- Volcanoes form when chambers of magma, or
hot molten rock, boil to the surface. These magma
chambers often remain sealed for hundreds of
years between eruptions, until the pressure
builds sufficiently to break through a vent,
which is a crack or weak spot in the rock above. - The blast creates a crater, where lava and
ash spill out, forming the cone. On some
volcanoes, the magma chamber collapses after a
violent eruption and a caldera forms, which is
just a large, bowl-shaped crater. Sometimes these
calderas fill with water, as happened at Crater
Lake in Oregon.
http//www.livescience.com/environment/volcano_ove
rview.html http//www.pacificislandtravel.com/nat
ure_gallery/volcanoes1.gif http//youtube.com/wat
ch?vWv-LxFeQwPIfeaturerelated
6Where and How do they form?
- Most volcanoes are found along a belt,
called the Ring of Fire, that encircles the
Pacific Ocean. Volcanic activity also occurs in
such places as Hawaii, Iceland, southern Europe,
and at the bottom of the sea. - Plate tectonics is the main reason for the
formation of volcanoes.. - Volcanoes can form when
- Two plates collide- One of the plates is then
forced under the other. As the plate sinks,
friction and Earth's heat cause part of it to
melt. This melted part then rises as magma. When
it reaches the surface, it produces a volcano. - Two plates spread apart-
- most such movement takes place on the ocean
floor. As the plates move apart, magma below the
crust moves up between the plates. Large amounts
of lava pour onto the surface and build up the
ocean floor. Magma sometimes creates an
underwater mountain range, such as the huge
Mid-Atlantic Ridge that runs down the length of
the Atlantic Ocean. - Magma Theory- Some scientists believe such
volcanoes develop when a huge column of magma
rises from inside Earth toward the surface. It
comes close enough to the surface that it
sometimes breaks through and forms a volcano. A
number of volcanoes, for example those in Hawaii
lie far from the plate boundaries. And this is
where this theory come in.
http//www.worldbook.com/wb/Students?content_spotl
ight/volcanoes/where
7Creation of Landforms
- There are four main land forms that can occur due
to volcanoes - 1. Lava flows- is a (moving) outpouring of lava,
which is created during a non-explosive effusive
eruption which forms igneous rock when it cools. - 2. Volcanic Peaks- A volcanic peak is what we
tend to think of when we talk about volcanoes. It
is a volcano that has formed a large cone shaped
hill, or mountain. These cones typically have a
large bowl shaped crater in the top center. - 3. Caldera- Calderas are massive crater-like
depressions that can cover many tens of square
miles. These calderas form when volcanoes explode
with terrible destruction, completely
obliterating the original volcano, and
surrounding area. - 4. Volcanic Neck- A volcanic neck is the
remnant of an old volcano. As the volcano died,
the last bit of lava inside of the volcanoes
opening, or neck, cooled and hardened. Over many
hundreds of thousands of years the material
around the neck is removed by erosion, leaving
only the harder neck behind.
www.kidsgeo.com/.../0054-volcanoes-landforms.php
8Lava flow Located in Hawaii Spewing lava 10
miles high.
A Volcanic peak (located above) And a Volcanic
neck (below).
A Caldera Crater Lake
www.kidsgeo.com/.../0054-volcanoes landforms.php
9Volcanoes in your backyard!