hazardous earth Flashcards
what are the tree primary concentric layers to the earth?
-core
-mantel
-crust
how are the core and mantel seprated?
sharp boundry at 2900km
also called moho
what are the two layers of the upper mantel?
100km-300km down = asthenosphere, this layer is semi molten or viscous
above this is the lithospshere = a ridgid layer samwhiched between the crust and the asthensosphere
thickness of crust
mean = 35km
density of crust
contiental - 2.6-2.7
oceanic - 3.0
minrel composition of crust
granitic
silicone
aluiminium
thickness of mantel
to a depth of 2900km
desnity of mantel
moho=3.3
core=5.6
minrel composition of mantel
rich in magnesium and iron
what do the lithosphere and crust make up?
congenital and oceanic plates
where do convection currents exits?
ashensosphere
what causes the convection currents?
caused by the vast amount of heat generated deep in the mantel as a result of the semi molten asthensophere flows carrying with it the solid lithoshpere and crust
contiental drift theory orgin?
durin the 18th centrey maps of the world multiplied and became more accurate and the shapes of the continents and their relationship to each other attracted intrest
first writer on the fit between northeast south America and the west coast of Africa?
Alexander Von Humbodt
who came up with the contiental drift theory?
Alfred Wenger 1912
key ideas of the contiental dirft theory?
-prosed that in the carboniferous period, 250 million years ago a large continent Pangea exited and this slowly broke apart into two large land masses
Alfred Wenger geological evidence?
-fit of continents such as the south America and south Africa on either side of the Atlantic
-mountine chains of rock sequenses on either side of the ocean show great simularity e.g northeast Canada and northen Scottland
-glacial evidnece is present at rocks on continents that are now located close to the equator
-glaciers leave deposit behind such as till, which is the sediment depoisted under a glacier as it retrets
sucsess level of mitgation will depend upton
record of past events
-time gap since past event (gap theory)
-nature of tectonic activity
- attutuide
-resilliance of people effected
mitgation against the event
land zoning
tusnami defense - sea walls and water breakwaters
lava diversion
mitgation against vunrebility
community prepration and eductaion
aseismic buildings
adaptation
mitgation against loss
long term aid
insurance
land zoning
relocation and avoiding building on certain areas
- low cost, relocation
-prevents economic development
-requires struct reenfourcement
tusnami defense
sea walls and water breakwaters
-reduce damage, sense of security
-if over topped it can cause damage
-expensive and unsightly
lava diversion
builds channels and cools lava with water
-divert away from important buildings, cheap compared to damage,
-only works for basaltic lava
-not feasable for most expolsive volcanos
mitgation against vunrebility
high tech montering
can be accurate and save lives
-costly, cry wolf syndrom
-property is still damages
community prepration and eductaion
-low cost and orgnised by NGO’S, saves lives localy
-property still damaged and hard to implemnt in rural areas