geog book 4 chap 2 Flashcards
(70 cards)
what is an earthquake
the shaking of the Earths ground due to sudden release of energy in the Earths lithosphere
generally pccurs along plate boundaries and contain faults
how do earthquakes occur
- Rock mass on one side of fault are pushed by tectonic forces
- friction causes rocks to get locked causing stress to build up
- when the stres exceeds the strength of the fault, rocks snap to a new position
- sudden movement causes seismic waves to be released causing ground shaking
what is the focus
point on earths crust where seismic waves are released
origin of the earthquake
what is the epicentre
point on earths directly above the focus
shaking is generally felt the most strength here
what are seismometers
sensitive instruments that detect ground vibrations and determine the magnitude of an earthquake
the higher the seismic energy released during an earthquake, the higher the magnitude
what is rhe richter scale
calculates earthquake magnitude using the height of the largest wave recorded on seismoneters and max seismic intensity reached rather than total seismic energy released
scale is logarithmic and is from 1-10
what is the limitation of the richter scale
would rate an earthquake with a single drastic spike in wave energy to have a higher magnitude than a long earthquake with many large and intense waves and underestimates longer earthquakes that release more overall energy that may cause more damage
hence it is not commonly used except for small local earthquakes
what is the moment magnitude scale
rates earthquake magnitude based on estimated total energy released during the earthquake
more accurate especially for earthquakes with magnitude 8 and above
thus scientists have adjusted magnitudes of past earthquakes such as the 1964 Prince William Sound Earthquake in Alaska from magnitude 8.6 to 9.2
scale is logarithmic
what is a volcano
a landform created when lava erupts onto the earth’s surface
may form a cone-shaped mountain as more lava erupts and accumulates over time
eruptions occur at dpb and cpb
how do tectonic processes at dpb result in volcanic eruptions
plates move apart causing the crust to stretch and fractures to develop
the decrease in overlying pressure causes parts of the underlying mantle to melt forming magma
magma contains dissolved gases and less dense than the surrounding materials
magma rises through weak areas in the crust to the earth’s surface and erupt as lava causing a volcanic eruption
lava cools and solidifies over time forming a volcano
how do tectonic processes at cpb result in volcanic eruptions
plates move towards each other and the denser plate subducts under the other
subducting plate sinks into the mantle and the high pressure forces water out of the oceanic crust
water lowers the melting point of overlying mantle causing it to melt forming magma
magma contains dissolved gases and is less dense than surrounding materials
hence magma rises through weak areas in the crust to the earths surface and erupt as lava causing a volcanic eruption
lava cools, solidifies and accumulates over time forming a volcano
what is high silica magma?
usually associated w stratovolcanoes
more viscous
as magma rises to the earths surface, dissolved gases in the magma cannot escape easily
more pressure builds up until gases escape explosively causing violent and explosive eruptions
give an example an explain a volcano with viscous magma yet does not result in an explosive reaction
Mt merapi is a stratovolcano but its eruption in 2006 was not explosive as viscous magma rose in a way that allowed dissolved gases to escape easily
what is low silica magma
usually associated with shield volcanoes
less viscous
as magma rises to the earths surface dissolved gases in the magma can escape easily
less pressure builds up resulting in gentle effusive eruptions
explain the formation of stratovolcanoes and name an example
high viscosity magma rises through weak areas in the crust to the earths surface and erupts explosively as lava, ash and rocks
ash and rocks settle on the sides of volcano and are later covered by lava
over successive eruptions, a tall volcano consisting if alternating layers of ash and lava develops
as high viscous lava travels a shorter distance before cooling and solidifying, volcano has steep sides and narrow summit
Mt Mayon Philippines
explain the formation of shield volcanoes and name an example
low viscosity magma rises through weak areas in the earths crust to the earths surface and erupts effusively
over successive eruptions, a volcano consisting of layers of lava develops
as the low viscosity lava travels a longer distance before cooling and solidifying, causing the volcano to have gentle sloping sides with a broad summit
Kilauea Hawaii
name the structure of a volcano
- magma chamber
- layers of rock
- pipe/ conduit
- layers of ash
- layers of lava
- lava flow
- vent
- volcano cone
- secondary cone
- crater
- pyroclasts
what is a magma chamber
a reservoir of molten rock beneath the Earth’s crust
as more magma seeps into the magma chamber,
pressure in the magma chamber builds up
giving rise to a volcanic eruption
what is a pipe/conduit
where magma flows from magma chamber to vent
what is a vent
opening in the earth’s surface with a pipe leading into magma chamber
how is the secondary cone formed
during formation of the volcano the vent may be blocked
forcing magma to find new exit route to surface
secondary cone of newer mantle material develops
what are pyroclasts
ash and rock fragments and volcanic bombs ejected during volcanic eruption
mixed with superheated gas, form pyroclastic flow which can reach up to 200m/s
becomes lahar when mixed with water of melted snow/ice causing fast moving mudflow if 40m/s
how is a caldera formed
the summit of a volcano may be blown off durint an explosive eruption
sides of the crater may collapse inwards due to loss of structural support
creates a much larger crater than original volcanic vent
a caldera, large basin-shaped volcanic depression is formed
over time, magma chamber beneath caldera solidifies and volcano bexomes extinct
caldera may then fill with water to form a lake
how are volcanic eruptions measured?
volcanic explosivity index measures magnitude if different volcanic eruptions based om explosivity
the greater the vol of ejected material -> higher VEI
the greater the height of eruption cloud -> higher VEI
the longer the duration of eruption -> higher VEI
measured on a scale of 0-8
- effusive 0 or 1 as they are non explosive with less than 0.0001km³ of material ejected
- value of 8 -> mega-colossal explosive eruption, eject more than 1000km³ of tephra and eruption cloud column height of over 25km
scale is logarithmic