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Chapter 8
Chapter 8

... repeated non explosive eruptions. Because the lava is very runny, it spreads out over a wide area. Over time the layers of lava create a volcano with gently sloping sides. Although their sides are not very steep, shield volcanoes can be enormous. . ...
Volcano Menu
Volcano Menu

... *Form as a result of subduction. ...
The Eruption of Mount Pinatubo
The Eruption of Mount Pinatubo

... Characteristics of volcanoes ...
Rocks Rock! Part 1
Rocks Rock! Part 1

... about rocks and minerals line their bookshelves. They own rock hammers, goggles, work gloves, and magnifying glasses. They have sturdy rock tumbling equipment to polish their finds, and some sort of container in which to display their rocks. It may be an old egg carton, or it may be a wooden display ...
volcano_powerpoint_semi_final[1]
volcano_powerpoint_semi_final[1]

... • Shield volcanoes are big and made up of fluid lava flows. • They get their name because the sloping hills that surround them have a fan shaped pattern that looks like a shield. • They have broad, sloping sides. • Shield volcanoes are formed from the action of the gas or steam or water vapor with ...
ROCK DETECTIVE CLIFFORD LAMBETH!!
ROCK DETECTIVE CLIFFORD LAMBETH!!

... Sedimentary • earth's surface is constantly being eroded. This means that rocks are broken up into smaller pieces by weathering agents such as wind, water, and ice. These small pieces of rock turn into pebbles, gravel, sand, and clay. They tumble down rivers and streams. These pieces settle in a ne ...
and benefits - of volcanic eruptions
and benefits - of volcanic eruptions

... was built by the steam explosions resulting from the incandescent torrent rushing into water, a crater being there formed, surrounded by a heap of black sand. This horse shoe heap was 75 feet high above sea level, and the front of it had broken down on the ocean side, revealing a section of bedded s ...
Volcanoes
Volcanoes

... • Commonly gas output from a volcano increases or changes composition before an eruption. – As magma rises to the surface it releases (exsolves) much of its gas content. – This can be measured ...
Volcanoes - St John Brebeuf
Volcanoes - St John Brebeuf

... • Commonly gas output from a volcano increases or changes composition before an eruption. – As magma rises to the surface it releases (exsolves) much of its gas content. – This can be measured ...
Volcanoes Powerpoint
Volcanoes Powerpoint

... • Commonly gas output from a volcano increases or changes composition before an eruption. – As magma rises to the surface it releases (exsolves) much of its gas content. – This can be measured ...
Composite volcanoes
Composite volcanoes

... explosive way. This is usually caused by viscous (thick) magma. • When very viscous magma rises to the surface, it usually clogs the craterpipe, and gas in the craterpipe gets locked up. • Therefore, the pressure will increase resulting in an explosive eruption. ...
Volcano Types (39)
Volcano Types (39)

... in magma by the pressure of the surrounding magma and rock. • As magma nears the surface, it is under less pressure, which allows gases to escape, causing non explosive volcanoes. • Gas that builds up to high pressures eventually causes explosive eruptions ...
• Once magma reaches the surface, it is called lava. • An example of
• Once magma reaches the surface, it is called lava. • An example of

... A huge hole left behind when a volcano collapses is a caldera. A volcano that erupts explosively produces ashes, cinders, and bombs. A sill forms when magma hardens between rocks in a horizontal layer. A batholith forms when a large amount of magma hardens beneath the crust. Hot water from undergrou ...
Course Learning Outcomes for Unit IV Reading Assignment Igneous
Course Learning Outcomes for Unit IV Reading Assignment Igneous

... form plutons (leading to batholiths and laccoliths), sills, and dikes. These will be exposed when the surrounding area erodes away (USGS, 1997). Approximately 640,000 years ago, a supervolcano erupted in what is now known as Yellowstone National Park. The eruption sent ash as far as Missouri. The Ca ...
rock
rock

... • Rocks formed from lava at the surface are classified as extrusive, or volcanic rocks • Rocks formed from magma that crystallizes at depth are termed intrusive, or plutonic rocks ...
Rocks - CRHS
Rocks - CRHS

... • the rock is moved into an environment in which the minerals which make up the rock become unstable and out of equilibrium with the new environmental ...
Kangaroo Valley Rocks for the Pioneer Museum Park
Kangaroo Valley Rocks for the Pioneer Museum Park

... hinged together, one larger than the other a rock made up of mixed sand, pebbles and cobbles a rock which has floated out to deeper water on or in ice, then dropped when the ice has melted ancient remains of plants or animals that have been covered up with sediment and preserved a rock that was form ...
These mountains are formed by compression Fault structures is a
These mountains are formed by compression Fault structures is a

... •Hawaiian-out pouring of fluid lava and little explosive activity. •Peleean-violent eruption with viscous lava “ nuees ardentes ’’. ...
Rocks Rock Homework
Rocks Rock Homework

... goggles, work gloves, and magnifying glasses. They have sturdy rock tumbling equipment to polish their finds, and some sort of container in which to display their rocks. It may be an old egg carton, or it may be a wooden display case with many different compartments. Every rock hound knows that rock ...
3_Types of Rocks
3_Types of Rocks

... weight of other sediment and the water on top of it. This process is called compaction. In some rocks, minerals dissolve as the water soaks into the rock, forming a natural cement that sticks the larger pieces of sediment together. ...
What is a volcano? - Mr. LaFranca`s Earth Science Class
What is a volcano? - Mr. LaFranca`s Earth Science Class

... • Lava is magma that reaches the surface of the crust. Affects are very localized • Pyroclastic Ash is a mixture of tiny rocks and dust that form huge clouds. Affects are localized and regional. • Pyroclastic Ash can be very thick and block out sunlight destroying crops. • The ash can settle on loca ...
CASCADES OF LAVA. 441 through these numerous craters into the
CASCADES OF LAVA. 441 through these numerous craters into the

... plete silence, and without any convulsion of the ground. Of the mountain, Mouna Loa, itself, a fearful ertiption took place in 1840, and it has since given repeated evidences of its activity. An eruption also occurred in 1843 from a crater about 2000 feet below the summit. A river of lava pouring do ...
Volcanic Landforms (pages 217*223)
Volcanic Landforms (pages 217*223)

... a. Batholiths form on the surface. b. Batholiths are large masses of rock. c. Batholiths may form dome mountains. ...
HELP
HELP

... Igneous rocks crystallise from molten rock called magma. Molten magma reaching the Earth’s surface is called lava. Magma that cools quickly forms igneous rocks with small crystals. Lava/magma that cools slowly forms igneous rocks with large crystals. Igneous rocks contain different minerals, this gi ...
Chapter 13 Section 2
Chapter 13 Section 2

... Volcanic Eruptions Types of Magma/Lava • Mafic - describes magma or igneous rock that is rich in magnesium and iron and that is generally dark in color • Felsic - describes magma or igneous rock that is rich in feldspar and silica and that is generally light in color • Mafic rock commonly makes up t ...
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Tuff



Tuff (from the Italian tufo) is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is compacted into a solid rock in a process called consolidation. Tuff is sometimes called tufa, particularly when used as construction material, although tufa also refers to a quite different rock. Rock that contains greater than 50% tuff is considered tuffaceous. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Since it is common in Italy the Romans used it often for construction. The Rapa Nui people used it to make most of the moai statues in Easter Island.Tuff can be classified as either sedimentary or igneous rocks. They are usually studied in the context of igneous petrology, although they are sometimes described using sedimentological terms.
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