it is usually a cone shaped mountain or hill that slopes downward to a pool of molten rock below the surface of the earth
VOLCANO
it is a vent or 'chimney' that connects molten rock (magma) from within the earth's crust to the earth's surface
VOLCANO
the interior of the earth has a very high temperature and pressure that can cause rocks to melt as well as dissolve other substances
earth needs to release excess heat. thus volcanoes are important in maintaining the thermal balance of earth's system
some volcanoes even exist underwater, along the ocean floor or sea bed. what are they called
VOLCANO DE AGUA
the study of the relief features of earth's crust
GEOMORPHOLOGY
the three primary geologic forces that continually after the planet's surface
DIATROPHISM, EROSION, VOLCANISM
it refers to the vertical and horizontal movement of the crust that typically produces the mountains
DIATROPHISM
the physical removal of rock or wearing down of landmasses by geomorphic agent such as running water, glacial ice, and wind
EROSION
often called volcanicity, is the phenomenon related to various processes associated with surface discharge of magma or hot water and steams including volcanoes, geysers, fumaroles, and hot springs
VOLCANISM
the side of a volcano
FLANK
the highest portion or apex of a volcano
SUMMIT
the large underground pool of liquid rock found beneath the earth's crust
MAGMA CHAMBER
a channel or pipe conveying liquid material such as magma
CONDUIT
the barrier or obstacles in a volcano
DIKES
a basin-like depression over a vent at the summit of the cone
CRATER
the opening through which an eruption takes place
VENT
a volcanic depression much larger than the original crater
CALDERA
usually composed of mixture of lava and pyroclastic
CONE
these vary in size and shape depending on the type of magma that is ejected by a particular volcano
CONE
the rock or magma expelled from a volcano during eruption
LAVA
its temperature upon ejection can reach up to 700°C hence, it flows until it cools and hardens
LAVA
the entrance of a volcano
THROAT
expelled in the atmosphere; volcanicash or ashcloud is composed of pulverized rock and glass created during eruption
ASHCLOUD
the chunks of lava blasted into the air which solidify before reaching the ground
VOLCANICBOMBS
their sizes may vary and can be measured up to 64mm in diameter
VOLCANICBOMBS
fast moving current of hot gases and rock travelling downhill from a volcano
PYROCLASTIC FLOW
the gases can reach temperature of more than 1000°C and can move up to a speed of 700km/hr
PYROCLASTIC FLOW
also called mudflows; are flowing mixture of volcanic debris and water
LAHAR
volcanoes form when magma reaches the earth's surface, causing eruptions of lava and ash
forming volcanoes occur at destructive and constructiveplateboundaries
the size of the volcano depends on the frequency of the eruption and how much magma is ejected into the surface
magma that contain more gases such as water vapour and carbon dioxide is less vicious and is thus resistant to flow
magma that contains more dissolved silicates is vicious and is thus resistant to flow
less vicious magma thus creates a slow steady eruption
whereas more vicious magma will create a strong and violent eruption