VOLCANOES Earth Science Fall 2012
Feb 24, 2016
VOLCANOESEarth Science Fall 2012
Vocabulary: aa – jagged chunks of lava formed by
rapid cooling on the surface of the lava flow
Vocabulary: Caldera- large basin-shaped depression
formed when an explosion destroys the upper part of a volcanic cone or when the magma chamber below a volcano is emptied during an eruption
Vocabulary: Cinder cone- steep sloped deposit of
solid fragments ejected from a volcano
Vocabulary: Composite volcano- (strato volcano)
steep sloped volcanic deposit with alternating layers of hardened lava flows and pyroclastic materials
Vocabulary: Crater- funnel-shaped pit at the top of a
volcanic cone; bowl shaped depression on the surface of a planetary body
Vocabulary: Felsic lava- silica rich lava
Vocabulary: Fissure- crack in a rock surface through
which lava flows
Vocabulary: Hot spot- area of volcanism within a
lithospheric plate
Vocabulary: Lapilli- pyroclastic particles between
2mm & 64 mm in diamter Lava- magma that reaches the earth’s
surface Mafic lava- dark colored rich in
magnesium and iron Magma- liquid rock produced deep
within the earth Pahoehoe- solidified mafic lava with a
wrinkled surface
Vocabulary: Pillow lava- lava that flows out of fissures
in the ocean floor and cools rapidly in round shapes
Pyroclastic material- the rock fragments ejected from a volcano
Sheild volcano- has a cone of hardened lava that forms a broad base and slopes gently
Stratovolcano- also called composite volcano; steep sloped volcanic deposit with alternating layers of hardened lava flows and pyroclastic material
Vocabulary: Vent- opening through which the molten
rock flows onto the surface Volcanic ash- pyroclastic particles
between 0.25mm and 2 mm in diameter Volcanic block- the largest possible
pyroclastic material that is formed from solid rock blasted from a volcanic fissure
Volcanic bomb- large, spindle-shaped clot of lava thrown out of a volcano
Vocabulary: Volcanic dust- pyroclastic particles that
are less than 2 mm in diameter Volcanism-any activity that includes the
movement of magma toward or onto the earth’s surface
Volcano- lava and pyroclastic material built up on the earth’s surface around a vent
Volcanoes & Plate Tectonics Scientists have no direct way to measure
temperatures within the earth Analysis of seismic waves & hear flow near
the earth’s surface & computer modeling allow scientists to estimate those temperatures
Areas of solid rock melt to form magma Forms when mantle material flows to areas
of lower pressure faster than it can lower its temperature by hear flow or when fluids such as water are added to the mantle material
Volcanoes & Plate Tectonics Volcanism
Any activity that includes the movement of magma toward or onto the surface of the earth
Pockets of magma form due to melting of some of the surrounding rock More rock melts, magma pockets get large
Volcanoes & Plate Tectonics most magma forms at plate boundaries,
where one plate is subducted beneath another plate
Magma that erupts onto the Earth’s surface is lava
The opening through which magma flows to the surface is called a vent
The structured formed by the vent and the material that builds up on the earth’s surface around the vent is called a volcano
Volcanoes & Plate Tectonics Major Volcanic Zones
Most active volcanoes occur in zones near both convergent and divergent boundaries of lithospheric plates
Subduction zones Deep trench forms on the ocean floor where
the continental crust is being subducted The plate of continental crust buckles and
folds, forming a line of mountains along the edge of the continent
Volcanoes & Plate Tectonics Magma erupts to the surface at the trench,
forming volcanic mountains near the edge of the continent
Major zone of active volcanoes is the Pacific Ring of Fire
If 2 oceanic plates collide one plate is subducted, forming a deep trench
After time a string of volcanic islands forms, called an island arc
Island arcs start as small islands and grow to large islands
Ex: Aleutian Islands- small islands Ex: Japan – large islands
Volcanoes & Plate Tectonics Mid-Ocean Ridges
The largest amount of magma comes to the surface at mid-ocean ridges
Major zone of volcanic activity Upwelling magma adds material to the mid-
ocean ridge & creates new lithosphere along the rift Can also form underwater volcanoes
Iceland is located on top of the mid-ocean ridge, it is separated by a fissure
Volcanoes & Plate Tectonics Hot spots
Areas of volcanism within the interior of the lithosphere
Appear to remain stationary, but actually drift slowly; as a result the volcano actually is carried away When the volcano is carried it away, it is moved
away from the hot spot and the activity of the volcano comes to an end
Hawaiian Islands are an example of a chain of volcanic islands formed over a hot spot
Volcanic Eruptions Geologists have concluded that there are
two general types of lava: Mafic lava- dark colored when hard and is
rich in magnesium and iron Forms much of the ocean crust
Felsic lava- contains lots of silica, less magnesium and iron, has a lighter color when hardened Common in continental crust
Volcanic Eruptions When mafic lava cools quickly, the
surface of the lava flow forms a crust The flow continues move and wrinkles up
forming pahoehoe, which means ropey in Hawaiian
If the crust is deformed rapidly or grows too thick to form wrinkles, it breaks into jagged chunks to form aa Sharp blocky texture of the volcanic rock
Volcanic Eruptions Lava cools so rapidly that the outside
hardens leaving a liquid core in the middle, called a lava tube
Lava can also flow out of fissures on the ocean floor, it cools rapidly separating into rounded blobs called pillow lava
Volcanic Eruptions Kind of Eruptions
The composition of the lava that reaches the surface largely determines the force with which a volcano will erupt.
Ocean volcanoes, those that erupt on the ocean floor and on oceanic islands, usually are produced by mafic lava Mafic lava is very hot and thin and flows easy Because gases escape quickly these eruptions
are very quiet
Volcanic Eruptions Felsic lavas of continental volcanoes tend
to be cooler and thicker Contain large amounts of trapped gases and
when the vent or fissure opens up, the dissolved gases within the lava boil out explosively, sending molten and solid particles shooting into the air
Volcanic Eruptions Volcanic Rock Fragments
Felsic lava explodes through pyroclastic material into the air Rock fragments ejected from a volcano Some forms when cooling magma breaks into fragments,
other forms when a spray of lava cools and solidifies Volcanic ash and dust generally land close the volcano Lapilli are larger than ash and dust and generally land
near the volcano Volcanic bombs are formed when large clots of lava
harden in the air Volcanic blocks can be a large as a house
Volcanic Eruptions Volcanic Features
Piles of volcanic material are volcanic cones Types of volcanoes
Volcanic cones that are broad at the base and have gently sloping sides are called shield volcanoes
Covers a wide area & generally results from lava eruptions
Slowly build up Ex: Hawaiian islands
Volcanic Eruptions Cinder cones- cause by explosive eruptions
Made of solid fragments ejected from the volcano Usually have very steep slopes Rarely more than a few hundred meters tall
Composite volcanoes (stratovolcanoes) Are formed by both quiet and explosive eruptions Cone usually formed from lava flows Explosive eruptions deposit lots of material around
the vent Cone is made of alternating layers of lava and
pyroclastic material Ex: Mount Fuji , Mount Raineer, Mount Hood
Volcanic Eruptions Craters & Calderas
Craters Formed when material is blown out of the volcano
by explosions Usually gradually becomes wider A small cone can form within a crater
Caldera When the magma chamber below a volcano is
emptied, the cone may collapse, leaving a large, basin-shaped depression
Can also be caused by eruptions that discharge large amounts of magma
Volcanic Eruptions Predicting Volcanic Eruptions
Scientist use measuring devices to detect geologic events that may signal the beginning of an eruption Small earthquakes
Result from growing pressure on the surrounding rocks as magma works it way upward
Temperature changes within the rock Slight bulging of the surface of the volcano Change in composition of the gases given off
by the volcano Study previous eruptions
Extraterrestrial Volcanism Many of the planets and moons of the
solar system were volcanically active at one time.
The Moon Near side is covered with basaltic lava flows Craters on the moon’s lunar surface come
from meteorite bombardment Maria – large impacts early in the moon’s
history created deep basins that later flooded with lava
We don’t know how magma was formed on the moon
Extraterrestrial Volcanism Mars
There are numerous volcanoes and volcanic features on the surface of Mars
Largest volcano on Mars is Olympus Mons. Rise nearly 28 km above the surface 600 km across Caldera is 70 km across
We don’t know if the Martian volcanoes are still active
Extraterrestrial Volcanism Io
Moon of Jupiter 1st planetary body other than Earth where
there have been active volcanoes found Probably the most volcanically active body
in the solar system The material that erupts from these
volcanoes is a bright yellow-red Scietists think that it is primarily sulfur and
sulfur dioxide
Review Temperature and pressure generally
keep the rocks in the athenosphere below melting point. Pink True Yellow False
Review Solid rock located deep in the mantle is
called magma.
Pink- TrueYellow- False
Review Magma may sometimes break through to
the earth’s surface.
Pink- trueYellow- false
ReviewMagma is able to rise upward through the
earth’s crust because it is less dense than the surrounding rocks.
Pink- trueYellow- false