USGS/Cascades Volcano Observatory, Vancouver, Washington
DESCRIPTION:
Magma, Lava, Lava Flows, Lava Lakes, etc.
- Magma, Lava, Lava Flows, etc.
- Cascade Range
- Hawaii
- Lava Domes
- Lava Lakes
- Lava Tubes and Lava Tube Caves
- Obsidian Flows
- Pillow Lavas
Magma, Lava, Lava Flows, etc.
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From:
Tilling, 1985, Volcanoes: USGS General Interest Publication
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Molten rock below the surface of the Earth that rises in volcanic vents is known
as magma, but after it erupts from a volcano it is called lava.
Originating many tens of miles beneath the ground, the ascending magma commonly
contains some crystals, fragments of surrounding (unmelted) rocks, and dissolved
gases, but it is primarily a liquid composed principally of oxygen, silicon,
aluminum, iron, magnesium, calcium, sodium, potassium, titanium, and manganese.
Magmas also contain many other chemical elements in trace quantities. Upon
cooling, the liquid magma may precipitate crystals of various minerals until
solidification is complete to form an igneous or magmatic rock.
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... heat concentrated in the
Earth's upper mantle raises temperatures sufficiently to melt the rock locally
by fusing the materials with the lowest melting temperatures, resulting in
small, isolated blobs of magma. These blobs then collect, rise through conduits
and fractures, and some ultimately may re-collect in larger pockets or
reservoirs ("holding tanks") a few miles beneath the Earth's surface. Mounting
pressure within the reservoir may drive the magma further upward through
structurally weak zones to erupt as lava at the surface. In a
continental environment magmas are generally in the Earth's crust as well as at
varying depths in the upper mantle. The variety of molten rocks in the crust,
plus the possibility of mixing with molten materials from the underlying
mantle, leads to the production of magmas with widely different chemical
compositions.
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If magmas
cool rapidly, as might be expected near or on the Earth's surface,
they solidify to form igneous rocks that are finely crystalline or glassy with
few crystals. Accordingly, lavas, which of course are very rapidly cooled, form
volcanic rocks typically characterized by a small percentage of crystals or
fragments set in a matrix of glass (quenched or super-cooled magma) or
finer grained crystalline materials. If magmas never breach the surface to
erupt and remain deep underground, they cool much more slowly and thus allow
ample time to sustain crystal precipitation and growth, resulting in the
formation of coarser grained, nearly completely crystalline, igneous rocks.
Subsequent to final crystallization and solidification, such rocks can be
exhumed by erosion many thousands or millions of years later and be exposed as
large bodies of so-called granitic rocks, as, for example, those
spectacularly displayed in Yosemite National Park and other part of the
majestic Sierra Nevada mountains of California.
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Lava
is red hot when it pours or blasts out of a vent but soon changes to dark
red, gray, black, or some other color as it cools and solidifies. Very hot,
gas-rich lava containing abundant iron and magnesium is fluid and flows like hot
tar, whereas cooler, gas-poor lava high in silicon, sodium, and potassium flows
sluggishly, like thick honey in some cases or in others like pasty, blocky
masses.
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All magmas contain dissolved gases, and as they rise to the surface to erupt,
the confining pressures are reduced and the dissolved gases are liberated either
quietly or explosively. If the lava is a thin fluid (not viscous), the gases
may escape easily. But if the lava is thick and pasty (highly viscous), the
gases will not move freely but will build up tremendous pressure, and ultimately
escape with explosive violence. Gases in lava may be compared with the gas in a
bottle of a carbonated soft drink. If you put your thumb over the top of the
bottle and shake it vigorously, the gas separates from the drink and forms
bubbles. When you remove your thumb abruptly, there is a miniatures explosion
of gas and liquid. The gases in lava behave in somewhat the same way. Their
sudden expansion causes the terrible explosions that throw out great masses of
solid rock as well as lava, dust, and ashes.
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The violent separation of gas from lava may produce rock froth called
pumice.
Some of this froth is so light -- because of the many gas bubbles --
that it floats on water. In many eruptions, the froth is shattered
explosively into small fragments that are hurled high into the air in the form
of volcanic cinders (red or black),
volcanic ash (commonly tan or gray), and volcanic dust. ...
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Most
composite volcanoes
have a crater at the summit which contains a central
vent or a clustered group of vents. Lavas either flow through breaks in the
crater wall or issue from fissures on the flanks of the cone.
Lava, solidified within the fissures, forms
dikes that act as ribs which greatly strengthen the cone. ...
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In some
shield-volcano eruptions,
basaltic lava pours out quietly from long
fissures instead of central vents and floods the surrounding countryside with
lava flow upon lava flow, forming broad plateaus.
Lava plateaus
of this type
can be seen in Iceland, southeastern Washington, eastern Oregon, and southern
Idaho. ...
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Volcanic or lava domes
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. ...
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Congealed magma, along with fragmental volcanic and wallrock materials,
can be preserved in the feeding conduits of a volcano upon cessation of
activity. These preserved rocks form crudely cylindrical masses, from which
project radiating dikes; they may be visualized as the fossil remains of
the innards of a volcano (the so-called "volcanic plumbing system") and are
referred to as volcanic plugs or necks. The igneous material in a
plug may have a range of composition similar to that of associated lavas
or ash, but may also include fragments and blocks of denser, coarser grained
rocks -- higher in iron and magnesium, lower in silicon -- thought to be samples
of the Earth's deep crust or upper mantle plucked and transported by ascending
magma. ...
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Lava, erupting
onto a shallow sea floor or flowing into the sea from land, may cool so rapidly
that it shatters into sand and rubble. The result is the production of huge
amounts of fragmental volcanic debris. The famous "black sand" beaches of Hawaii
were created virtually instantaneously by the violent interaction between hot
lava and sea water. On the other hand, recent observations made from
deep-diving submersibles have shown that some submarine eruptions produce flows
and other volcanic structures remarkable similar to those formed on land. ...
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Ash and Tephra and Pumice and Scoria Menu
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Lava Plateaus and Flood Basalts Menu
From:
Myers and Brantley, 1995, Volcano Hazards Fact Sheet: Hazardous Phenomena
at Volcanoes, USGS Open-File Report 95-231.
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Molten rock (magma)
that pours or oozes
onto the Earth's surface is called lava.
The higher a lava's silica content, the more viscous it becomes.
For example, low-silica basalt lava can form fast-moving (10-30 miles per hour),
narrow lava streams or spread out in broad sheets up to several
miles wide. Between 1983 and 1993, basalt lava flows erupted at
Kilauea Volcano in Hawaii destroyed nearly 200 houses and severed
the coast highway along the volcano's south flank.
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In contrast, higher-silica andesite and dacite lava flows tend to
be thick, move slowly, and travel short distances from a vent.
Dacite and rhyolite lava flows often form mound-shaped features called
domes.
From:
Wright and Pierson, 1992, Living With Volcanoes, The
U. S. Geological survey's Volcano Hazards Program, USGS Circular 1973
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Streams of molten rock that either effuse quietly
from a vent or are fed by lava fountains.
Fluid basalt flows can move at velocities from 15 to as high
as 50 kilometers per hour on steep slopes and travel up to tens of kilometers
from their source. Viscous andesite flows move only a few kilometers per
hour and rarely extend more than 8 kilometers from their vent. Lava flows
destroy everything in their path, but most move slowly enough that people can
escape.
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Lava (usually dacite or rhyolite)
that is too sticky to flow far from its vent forms steep-sided mounds called
lava domes.
From:
Miller, 1989,
Potential Hazards from Future Volcanic Eruptions in California:
USGS Bulletin 1847, 17p.
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Lava flows
are streams of molten rock that erupt relatively nonexplosively from
a volcano and move slowly downslope. The distance traveled by a lava flow
depends on such variables as the viscosity of the lava, volume erupted,
steepness of the slope, and obstructions in the path of the flow. Basalt flows
may reach 50 kilometers from their sources, but few andesite flows extend more
than 10-15 kilometers. Because of their high viscosity, dacite and rhyolite
lava extrusions typically form short, thick flows or
domes.
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Lava flows cause extensive damage or total destruction by burning, crushing, or
burying everything in their paths. They need not directly threaten people,
however, because they usually move a few meters to a few hundred meters per
hour, and their paths of movement can be at least roughly predicted. Lava flows
that move onto snow or ice can cause destructive debris flows and floods, and
those that move into forests can cause fires. The flanks of lava flows
typically are unstable during their growth and collapse repeatedly, occasionally
producing
explosive blasts and (or) small
pyroclastic flows. ...
From:
Clynne, et.al., 1998,
How Old is "Cinder Cone"? -- Solving a Mystery in Lassen Volcanic National Park, California:
USGS Fact Sheet 173-98
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Scoria forms when blobs of gas-charged lava are thrown into the
air during an eruption and cool in flight, falling as dark volcanic rock containing
cavities created by trapped gas bubbles.
From:
Hoblitt, Miller, and Scott, 1987,
Volcanic Hazards with Regard to Siting Nuclear-Power Plants
in the Pacific Northwest, USGS Open-File Report 87-297
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Lava flows are streams of molten rock
that erupt relatively nonexplosively
from a volcano and move downslope.
The distance traveled by a lava flow depends
on such variables as the effusion rate,
fluidity of the lava, volume erupted,
steepness of the slope, channel geometry,
and obstructions in the flows path.
Basalt flows are characterized by relatively
low viscosity and may reach more than 50 kilometers
from their sources; in fact,
one Icelandic basalt flow reached 150 kilometers.
Andesite flows have higher viscosity and
few extend more than 15 kilometers; however,
one andesite flow of Pleistocene age
in the Cascades is 80 kilometers long.
Because of their high viscosity,
dacite and rhyolite lava extrusions typically form short,
thick flows or
domes.
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Lava flows cause extensive damage or total destruction by burning,
crushing, or burying everything in their paths. They
seldom threaten human life, however, because of their
typically slow rate of movement, which may be a few meters to a
few hundred meters per hour. In addition, their paths of
movement generally can be predicted. However, lava flows that
move onto snow or ice can cause destructive
lahars and floods,
and those that move into forests can start fires. The flanks
of moving lava flows typically are unstable and collapse repeatedly,
occasionally producing small explosive blasts or small
pyroclastic flows.
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Lava flows have been erupted at many vents in the Cascade Range during
Holocene time; their compositions range from
basalt to rhyolite. The longest known basalt, andesite,
and rhyolite lava flows erupted at Cascade volcanic centers during
Holocene time are, respectively, the 45-km-long Giant Crater
basalt flow at
Medicine Lake volcano
the 12-kilometer-long Schriebers Meadow andesite flow at
Mount Baker,
and the 2-kilometer-long Rock Mesa rhyolite flow at
Three Sisters.
Lava flows of varied composition are likely to erupt again in the
Cascade Range and will endanger all non-movable objects in
their paths.
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Cascade Range Menu
From:
Tilling, Heliker, and Wright, 1987, Eruptions of Hawaiian Volcanoes:
Past, Present, and Future: USGS General Interest Publication, 54p.
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Scientists use the term lava for molten rock
(and contained gases) that
breaks through the Earth's surface, and the term
magma for molten rock underground. ...
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Lava flows form more than 99 percent of the above-sea parts of
Hawaiian volcanoes.
Pahoehoe (pronounced "pah-hoy-hoy") and aa
(pronounced "ah-ah") are the two main types of Hawaiian lava flows, and these
two Hawaiian names, introduced into the scientific literature in the late 19th
century, are now used by volcanologists worldwide to describe similar lava-flow
types. Pahoehoe is lava that in solidified form is characterized by a smooth,
billowy, or ropy surface, while aa is lava that has a rough, jagged, spiny, and
generally clinkery surface. In thick aa flows, the rubbly surface of loose
clinkers and blocks hides a massive, relatively dense interior.
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The contrast between the surfaces of pahoehoe and aa flows is
immediately obvious to anyone hiking Hawaiian lava fields. Walking on dense
pahoehoe can almost be as easy as strolling on a paved sidewalk. But walking
across aa is like scrambling over a building-demolition site or battle zone,
strewn with loose, unstable debris of all shapes and sizes. The jagged rubble
of aa flows quickly destroys field boots and, should the hiker stumble or fall
(not at all uncommon), it can tear clothing and flesh.
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Many Hawaiian lava flows solidify as pahoehoe
throughout their extent, and a few
flows solidify completely as aa.
Most flows, however, consist of both pahoehoe
and aa in widely varying proportions. In a given flow, pahoehoe upstream
commonly changes to aa downstream, but aa lava flows do not change into pahoehoe
flows. ...
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Hawaiian lava is fluid enough to travel great distances, especially if it is
transported through
lava tubes.
Some historic flows are longer than 30 miles; in general, pahoehoe flows
tend to be longer than aa.
Lava tubes may be preserved when the eruption ends and the lava drains away to
leave open tunnels. They may be as much as several tens of feet in diameter,
and some have been followed by spelunkers (cave explorers) for nearly 10
miles. Ancient Hawaiians used lava tubes as places of shelter and as burial
caves. ...
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During long-lived eruptions, lava flows
tend to become "channeled" into a few main streams. Overflows of lava from
these streams solidify quickly and plaster on to the channel walls, building
natural levees or ramparts that allow the level of the lava to be
raised. Lava streams that flow steadily in a confined channel for many hours to
days may develop a solid crust or roof and thus change gradually into streams
within lava tubes. Because the walls and roofs of such tubes are good
thermal insulators, lava flowing through them can remain hot and fluid much
longer than surface flows. Tube-fed lava can be transported for great distances
from the eruption sites. For example, during the 1969-74 Mauna Ulu
eruptions at Kilauea, lava flows traveled underground through a lava-tube
system for more than 7 miles long to enter the ocean on five occasions. ...
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Link to: Hawaiian Volcano Observatory Website
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[Image,64K,JPG]
Aerial view, Novarupta Dome, Katmai Vicinity, Alaska.
-- USGS Photo by Gene Iwatsubo, July 29, 1987
From:
Hoblitt, Miller, and Scott, 1987,
Volcanic Hazards with Regard to Siting Nuclear-Power Plants
in the Pacific Northwest, USGS Open-File Report 87-297
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Volcanic domes are mounds that form when viscous lava is erupted slowly
and piles up over the vent, rather than moving
away as a lava flow.
The sides of most domes are very steep and typically are mantled with
unstable rock debris formed
during or shortly after dome emplacement. Most domes are composed of
silica-rich lava which may contain enough
pressurized gas to cause explosions during dome extrusion.
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Lava Domes Menu
From:
Tilling, Heliker, and Wright, 1987, Eruptions of Hawaiian Volcanoes:
Past, Present, and Future: USGS General Interest Publication, 54p.
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Another common lava product is the ponded flow or lava lake ...
The surface of lava that is ponded is smooth, broken only by polygonal cooling
cracks, formed in much the same way as shrinkage cracks in mud that has been
dried by the sun.
From: Smithsonian Institution Global Volcanism Program Website, 2003
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Erta Ale
is an isolated basaltic
shield volcano
that is the most active volcano in
Ethiopia.
The broad, 50-kilometer-wide
volcano rises more than 600 meters from below sea
level in the barren Danakil depression. Erta Ale is the namesake
and most prominent feature of the Erta Ale Range.
The 613-meter-high volcano contains a 0.7 x 1.6 kilometers,
elliptical summit crater housing steep-sided pit craters.
Another larger 1.8 x 3.1 kilometer-wide depression elongated
parallel to the trend of the Erta Ale range is located to
the southeast of the summit and is bounded by curvilinear fault
scarps on the southeast side. Fresh-looking basaltic
lava flows from these fissures have poured into the
caldera
and
locally oveflowed its rim.
The summit caldera is renowned
for one, or sometimes two longterm lava lakes that have been
active since at least 1967, or possibly since 1906.
Recent
fissure eruptions have occurred on the northern flank of Erta
Ale.
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Lava Lakes Menu
Lava Tubes and Lava Tube Caves
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[Image,47K,JPG]
Ape Cave, Mount St. Helens National Volcanic Monument
-- U. S. Forest Service Image, courtesy Mount St. Helens National Volcanic Monument
From:
Tilling, Heliker, and Wright, 1987, Eruptions of Hawaiian Volcanoes:
Past, Present, and Future: USGS General Interest Publication, 54p.
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During long-lived eruptions, lava flows
tend to become "channeled" into a few main streams. Overflows of lava from
these streams solidify quickly and plaster on to the channel walls, building
natural levees or ramparts that allow the level of the lava to be
raised. Lava streams that flow steadily in a confined channel for many hours to
days may develop a solid crust or roof and thus change gradually into streams
within lava tubes. Because the walls and roofs of such tubes are good
thermal insulators, lava flowing through them can remain hot and fluid much
longer than surface flows. Tube-fed lava can be transported for great distances
from the eruption sites. For example, during the 1969-74 Mauna Ulu
eruptions at Kilauea, lava flows traveled underground through a lava-tube
system for more than 7 miles long to enter the ocean on five occasions.
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Lava Tubes and Lava Tube Caves Menu
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[Image,114K,JPG]
Glass Mountain from Medicine Lake caldera rim
-- USGS Photo by J. Donnelly-Nolan
From:
Donnelly-Nolan, et.al., 1990,
Post-11,000-Year Volcanism at Medicine Lake Volcano, Cascade Range,
Northern California:
IN: Journal of Geophysical Research, v.95., no.B12, p.19,699.
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Glass Mountain
consists of a spectacular, nearly treeless, steep-sided
rhyolite and dacite obsidian flow that erupted just outside the eastern
caldera
rim and flowed down the steep eastern flank of Medicine Lake volcano. ...
From:
Sherrod, et.al., 1997,
Volcano Hazards at Newberry Volcano, Oregon:
USGS Open-File Report 97-513
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Newberry volcano is a broad shield volcano located in central Oregon.
It has been built by thousands of eruptions, beginning about
600,000 years ago. At least 25 vents on the flanks and summit have
been active during several eruptive episodes of the past 10,000 years.
The most recent eruption 1,300 years ago produced the
Big Obsidian Flow.
Thus, the volcano's long history and recent activity indicate
that Newberry will erupt in the future.
From:
Tilling, Heliker, and Wright, 1987, Eruptions of Hawaiian Volcanoes:
Past, Present, and Future: USGS General Interest Publication, 54p.
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Fluid lava erupted or flowing under water may form a special structure called
pillow lava. Such structures form when molten lava breaks through the
thin walls of underwater tubes, squeezes out like toothpaste, and quickly
solidifies as irregular, tongue-like protrusions. This process is repeated
countless times, and the resulting protrusions stack one upon another as the
lava flow advances underwater. The term pillow comes from the
observation that these stacked protrusions are sack-or pillow-shaped in cross
section. Typically ranging from less than a foot to several feet in diameter,
each pillow has a glassy outer skin formed by the rapid cooling of the lava by
water. Much pillow lava is erupted under relatively high pressure created by
the weight of the overlying water; there is little or no explosive interaction
between hot lava and cold water. The bulk of the submarine part of a Hawaiian
volcano is composed of pillow lavas. ...
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[Glossary of Hazards, Features, and Terminology] ...
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01/05/07, Lyn Topinka