a’a
is lava with a rough, jagged surface composed of broken lava blocks called clinkers, ---lava forms when lava has cooled, and its viscosity has been increased.
andesitic magma
higher viscosity and lots of dissolved gas, so it tends to erupt explosively, intermediate to felsic
ash
a pyroclastic that is less than 2mm in diameter, very powdery and remains suspended in the air for a long time, created during explosive eruptions
basaltic magma
has a lower viscosity and less dissolved gas trapped in it, so it tends to erupt gently, mafic magma
batholith
LARGE magma chamber that solidifies underground, has an exposed surface area greater than 100 km2
caldera
Large depressions are caused by the collapse of the ground above an emptied magma chamber, found at continental hotspots
cinder cone volcano
The “ant hills” of the volcano world - can pop up in any plate tectonic setting, steep slopes and an abnormally large crater
clinkers
composed of broken lava blocks, part of a’a lava, makes a clinking sound
coarse-grain
with large crystals, between fine and very course, also called phaneritic; granite, diorite, gabbro
concordant
forms parallel to surround rock (country rock), many types
crystallization
the process of forming crystals; the longer it takes to cool, the larger the crystals will be
dike
discordant; leads to two types of volcanic features, volcanic pipe and volcanic neck
create mini lines like scars leading to volcanic features
discordant
cuts across layers of surrounding rock (country rock), usually vertical-ish
extrusive (volcanic)
surface, forms on the exterior of the planet, forms from volcanoes
felsic
high silica, light color, low Mg and Fe levels
magma that is more ----- it will have a higher viscosity, larger amount of gas trapped, and more explosive
fine-grained
smallest crystals, without being coarse, also called aphanitic; rhyolite, basalt, andesite
glassy
this texture is formed when lava forms very quickly above the surface, obsidian has this
hornito
a small spatter cone that forms on the surface of a lava flow (usually pahoehoe), typically steep sided and form standalone pinnacles or stacks.
igneous rock
FIRE = formed from magma or lava
intermediate
between felsic and mafic; in between silica, color, and Fe and Mg composition
intrusive (plutonic)
under the surface, interior of the Earth, forms from plutons
kipuka
a small piece of land completely surrounded by lava flows, like an island in lava, a piece of land lava misses
laccolith
forms when magma is injected between two layers of sedimentary rock underground, the pressure of the magma intruding between preexisting layers causes the overlying rocks to dome up, creating a mushroom shape
lahar
rapidly flowing mixture of rock debris and water that originates on the slopes of a volcano, also referred to as volcanic mudflows/debris flows.
What it takes to create it:
loose volcanic debris (ash, lapilli etc.)
water (often rains after eruption due to water vapor and condensation nuclei added to air also melting from snowcap)
steep slope (Composite Cones are steep)
lapilli
Latin for “little stone,” and is a pyroclastic that is between 2mm and 64mm (a tennis ball) in diameter, least deadly pyroclastic
lava
hot, molten or semi-molten rock that has reached the surface
Only liquid and solid
Most dissolved gases have escaped
lava bench
is a platform formed by new lava flows that extends the old shoreline, making new land, highly unstable because they often are underlain only by loose material such as sand and wave-eroded rock.
lava block
is a pyroclastic larger than 64 mm, comes from parts of volcanic cone getting blasted in air
lava bomb
is a large pyroclastic that is still molten as it flies, Bombs often have a streamlined shape (like Pele’s tears)
lava lake
large volumes of molten lava, usually basaltic, contained in a volcanic vent, crater, or broad depression
Mt. Nyiragongo is the largest ------ in the world
tree molds
are cylindrical hollows left behind in a lava flow if the lava has completely incinerated the tree it once flowed around
lava tree
are formations created when pahoehoe flows around a tree and cools to form a crust around the trunk.
lava tube
is a natural conduit through which lava travels beneath the surface of a lava flow. Tubes form by the crusting over of lava channels and pahoehoe flows.
mafic
low silica content but high magnesium and iron content (“mafic” stands for “magnesium” and “iron”), generally darker in color
magma
hot, molten or semi-molten rock located under ground
------is made up of solid, liquid, and gas:
the liquid portion is referred to as the melt
the solid portion is made of minerals that crystallize directly from the melt; known as the mush
solid rocks picked up on the way out called xenoliths or inclusions
the gaseous portion is dissolved into the magmaocation beneath the vent of a volcano where molten rock (magma) is stored prior to eruption
magma chamber
la partially or totally molten body located in the earth's crust and capable of supplying magma to volcanic eruptions, location beneath the vent of a volcano where molten rock (magma) is stored prior to the eruption
pahoehoe
lava that has a smooth (yet often wrinkled) surface.
Many appearances:
toe
ropy
coil
entrail
Pele
the Hawaiian goddess of vocanoes
Pele’s Hair
is a naturally-spun volcanic glass that is blown away from lava fountains, cascading lava falls, or turbulent lava flows, gold in color and very fine (diameter of less than half a millimeter)
Pele’s Tears
small bits of molten lava in fountains can cool quickly and solidify into glass particles shaped like spheres or tear drops
pillow basalt
a volcanic igneous rock that forms when lava of basaltic composition comes from an underwater volcano
pluton
igneous rock formations that cool and solidify below the surface
magma is molten underground
formed after the magma has cooled underground
erosion exposes them at the surface
pyroclastics (tephra)
fragments of volcanic rock and lava blasted into the air by a volcanic eruption
Classified by size
Ash-->lapilli-->blocks & bombs
more deaths than lava & poison gas
pyroclastic flow
is a ground-hugging avalanche of hot ash, rock fragments, and volcanic gas that rushes down the side of a volcano at 100 - 400 mph or more!!
the temperature within may be greater than 500° C.
The deadliest hazard in a volcanic eruption
rhyolitic magma
Magmas here are felsic (remember that means highest in silica content), the fancy name
Rift Eruption (Curtain of Fire)
part of divergent volcanism, on land, a wall of lava fountains erupted from a crack
Ring of Fire
refers to region surrounding the Pacific plate where an increased amount of volcanism takes place due to subduction, lots of stratovolcanoes
shield volcano
Volcanoes made at oceanic hotspots; very tall and very wide, made mostly of lava flows piling up over and over, eruptions here will generally be mild due to less silica and lower viscosity (mafic and basaltic magmas)
silica
oxygen and silicon, the more ---- the thicker and more viscous it is, higher presents in felsic rocks/lava
sill
Pluton that is concordant (Parallel to bedding structures), surrounded by country rock (rock that was originally layered)
Ex: Palisades of NY & NJ on Hudson River
skylight
an opening in the roof of a lava tube
stock
smaller version of a batholith, has an exposed surface area less than 100 km2
stratovolcano (composite volcano)
formed at convergent subduction volcanism
are the “classic volcano shape”
Taller than wide, made of alternating layers of lava and pyroclastics
lots around Ring of Fire
texture
is affected by cooling rate; larger crystals the longer it takes to cool
three main -----:
glassy
vesicular (gassy and full of air holes)
fine-grained/aphanitic
coarse-grain/phaneritic
very coarse-grain/pegmatitic
tsunami
can be generated when a volcanic eruption abruptly displaces ocean water by either an explosion or landslide, a Japanese word with the English translation, "harbor wave”,
very-coarse grained (pegmatitic)
with largest crystals, took longer to cool; pegmatite
vesicular
gassy and full of air hole, no crystals; pumice, scoria, vesicular basalt
viscosity
measures a liquid’s resistance to flow
Thicker = High Viscosity
“High viscosity” flows slowly
“Low viscosity” flows fast
The more silica a magma has in it, the thicker and more viscous it is
Volcanic Explosively Index (VEI)
measures the amount of ash and debris thrown into the atmosphere during eruptions, eruptions with a large --- can significantly alter the climate for years
scale from 1 (less ash and debris, 0.0001 km) - 10 (most ash and debris, 1,000 km)
volcanic fissure
a crack in the ground that allows lava to shoot into the air
volcanic neck
vertical structure left exposed once the outside of the volcano weathers and erodes away, discordant
*the volcano around it has been eroded away
volcanic pipe
solid lava conduit from magma chamber to surface, discordant
*there is a volcano surrounding it
Mined for diamonds in northern Canada!
xenolith (inclusion)
solid rocks picked up by magma, a piece of rock within an igneous rock that is not derived from the original magma but has been introduced from elsewhere, especially the surrounding country rock
volcanism
refers to the activity of magma forming and coming toward surface
volcano
the landform created when magma reaches the surface through an opening in Earth’s crust
country rock
rock that was originally layered
volcano
is the landform created when magma reaches the surface through an opening in Earth’s crust
volcanism
refers to the activity of magma forming and coming toward surface