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MAGMA
CHAMBER
A large underground pool of
liquid rock found beneath the
surface of the Earth. The
molten rock in such a
chamber is under great
pressure, and given enough
time, that pressure can
gradually fracture the rock
around it creating outlets for
the magma.
MAGMA
The form of
molten rock,
stored deep
within the
Earth’s surface
CONDUIT
The pipe that magma
travels through to reach
the Earth’s surface
CRATER
Roughly circular depression
in the ground caused
by volcanic activity. It is
typically a bowl-shaped
feature within which occurs a
vent or vents
CALDERA
Large
volcanic
craters
LAVA
A molten rock generated
by geothermal energy
and expelled through
fractures in planetary
crust or in an eruption,
usually at temperatures
from 700 to 1,200 °C.
LAVA
Bright yellow (over 1000 °C)
Orange (800-900 °C)
Dull red colors (600-700 °C)
PAHOEHOE
Southern Part of Hawai’i
PAHOEHOE
A smooth and continuous lava crust
Only low-viscosity lava can form pahoehoe
Lava flow that was originally pahoehoe may
transform into a’a lava
Pahoehoe is also known as ropy lava and it has
several more varieties named
Special conditions are needed for pahoehoe to
form: lava with low viscosity, low effusion rate,
and gentle slope.
A’A
Near the Western Coast of La Palma, Canary Islands
A’A
A rough rubbly crust of a lava flow.
Walking on it is very slow and potentially
dangerous even if one has good hiking boot.
The uppermost part of a’a lava is composed
of loose unstable blocks
Flow rates exceeding 5-10 m3/s clearly
favors the formation of a’a lava
BLOCKY
La Palma, Canary Islands
BLOCKY LAVA
 Common if the silica content of
lava is higher.
 They have irregular surfaces but
they contain larger lava blocks
with smoother sides and angular
edges.
PILLOW
Pillow lava near Fasoula. Troodos Ophiolite Complex, Cyprus
PILLOW LAVA
 A type of lava that is always associated
with water.
Form when lava flows out of the Earth’s
crust underwater
Usually demonstrate a convex upper and
concave or flat lower surface.
The surfaces of pillow lava are glassy.
VENTS
Spot in the Earth’s
crust where gases,
molten rock, lava
and rocks erupt
SILL
A flat piece of rock
formed when magma
hardens in a crack in
a volcano.
FLANK
The side of the
volcano
PARASITIC CONES
Cone-shaped
accumulation of volcanic
material that is not a part
of the central vent of a
volcano. It forms from
eruptions from fractures
on the flank of the
volcano.

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Volcanic Landforms and Features Explained

  • 1.
  • 2.
  • 3. MAGMA CHAMBER A large underground pool of liquid rock found beneath the surface of the Earth. The molten rock in such a chamber is under great pressure, and given enough time, that pressure can gradually fracture the rock around it creating outlets for the magma.
  • 4. MAGMA The form of molten rock, stored deep within the Earth’s surface
  • 5. CONDUIT The pipe that magma travels through to reach the Earth’s surface
  • 6. CRATER Roughly circular depression in the ground caused by volcanic activity. It is typically a bowl-shaped feature within which occurs a vent or vents
  • 8. LAVA A molten rock generated by geothermal energy and expelled through fractures in planetary crust or in an eruption, usually at temperatures from 700 to 1,200 °C.
  • 9. LAVA Bright yellow (over 1000 °C) Orange (800-900 °C) Dull red colors (600-700 °C)
  • 10.
  • 12. PAHOEHOE A smooth and continuous lava crust Only low-viscosity lava can form pahoehoe Lava flow that was originally pahoehoe may transform into a’a lava Pahoehoe is also known as ropy lava and it has several more varieties named Special conditions are needed for pahoehoe to form: lava with low viscosity, low effusion rate, and gentle slope.
  • 13. A’A Near the Western Coast of La Palma, Canary Islands
  • 14. A’A A rough rubbly crust of a lava flow. Walking on it is very slow and potentially dangerous even if one has good hiking boot. The uppermost part of a’a lava is composed of loose unstable blocks Flow rates exceeding 5-10 m3/s clearly favors the formation of a’a lava
  • 15.
  • 17. BLOCKY LAVA  Common if the silica content of lava is higher.  They have irregular surfaces but they contain larger lava blocks with smoother sides and angular edges.
  • 18. PILLOW Pillow lava near Fasoula. Troodos Ophiolite Complex, Cyprus
  • 19. PILLOW LAVA  A type of lava that is always associated with water. Form when lava flows out of the Earth’s crust underwater Usually demonstrate a convex upper and concave or flat lower surface. The surfaces of pillow lava are glassy.
  • 20. VENTS Spot in the Earth’s crust where gases, molten rock, lava and rocks erupt
  • 21. SILL A flat piece of rock formed when magma hardens in a crack in a volcano.
  • 22. FLANK The side of the volcano
  • 23. PARASITIC CONES Cone-shaped accumulation of volcanic material that is not a part of the central vent of a volcano. It forms from eruptions from fractures on the flank of the volcano.