large chambers of magma cool
underground and form domes of
igneous rock
Dykes and sills
magma flows into gaps in the
surrounding rock, cools and forms
vertical dykes and horizontal sills
Cooling
Cracks
cracks may form as
the magma cools
Extrusive
Lava Eruptions
Basaltic lava - Constructive
temperature of eruption over 950
flows easily and gas can escape easily.
eruptions aren't violent, usually frequently
and long periods
Andesitic and Rhyolitic - Destructive
750-950 degrees eruption. rhyolitic is less than 750
flow less easily and often have blockages. gases
can't escape so pressure build and the blockage
is cleared by a violent eruption. short lived and
intermittent
Volcanos
Dome- Destructive. lava is rhyolitic or andesitic. thick
lava causes steep sides as it flows shorter distances
Caldera- Destructive. andesitic and
rhyolitic. central part collapses as the
magma chamber below empties
Shiled- Constructive.
Basaltic lava. long linear
vent can be several km
long
Hot Springs
places where groundwater emerges at
the surface. if the source is close to an
area of recent intrusive activity the water
is heated and becomes a hot spring
temperature varies from 20-90
degrees. tourist attractions
Geysurs
type of hot spring here hot water
and steam are ejected from the
surface in a fountain.
groundwater is heated above boiling
point by magma in the crust
hot water becomes pressurised
and forces its way to the
surface
Boiling mud pool
another hot spring, form in areas with fine
grained soil, water mixes with the soil to make
a hot muddy pool