SOLUTION: San Jose State University Volcanic Landforms Questions


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Volcanic Landforms
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Volcanic landforms

Lahar refers to the collected or hot compound of hurl and instil litter that runs down a
displosive increase into a large stream lowering. Lahars usually supervene adjacent or on stratovolcanoes and are
commonly referred to as displosive mudflows accordingly they convey docile hurls and hot ash, which
can liquify the ice to effect a compound of ash and instil in the produce of mudflow. Lahars produces
when displosive ash mixes delay instil to produce a thicker key that lifts the larger hurls to the
surface of the run. When it actuates below, it mobilizes all bignesss of hurls and carries them
along as they pursuit down the lowering delay accelerating hurry. They can, hereafter, extend past than
ten times their moderate bigness as they actuate downincrease separate from the volcano where they thus-far
decelerate and shelter its commits.

Pyroclastic runs are limpid compounds of valid valid and gas displosive litter delay low
viscosity; hereafter can actuate either upincrease or down a increase depending on the momentum they
generate. A pyroclastic run burns everything on its route accordingly it is hot and generally supervenes
from displosive exumations. Pyroclastic run produces when a displosive exumation supervenes and expels
gases, ash, and lava, which thus-far destroy upward momentum, hereafter, escheatment to the foundation.
Pyroclastic runs can so produce when the expelled displosive remnant b...

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