Plate Boundaries, Earthquakes, Tectonics Flashcards
destructive plate boundary
found where continental plate meets oceanic plate. oceanic is heavier so continental sinks under. As they scrape together, friction melts the rock and escapes as lava in a violent volcanic eruption along with severe earthquakes
conservative plate boundary
found when two plates slide past eachother along a fault.
No volcanoes are found but severe earthquakes occur
constructive plate boundary
found where two plates move apart. as they do a gap appears and allows lava to eacape. makes gentle volcanic eruption and less violent earthquakes
andesitic magma
low in temp has more silica and dissolved gas more likely to explode when reaches surface very viscous (flows much slower) creates steep sided volcanoes
basaltic magma
high in temp
very low on silica
produces fluid lava with very little explosive activity
non acidic, very runny
creates gentle sides as lava flows before soldifies
composite volcanoes
a tall explosive cone shaped volcano formed by layers of silica rich lava and ash
what are shield volcanoes
a low flat gently sloping volcano built from many flows of liquid, low viscosity basaltic lava
collision zone
fold mountains produced by upthrust
as they have an equal density, when they move together neither of them can sink and the land between them is pushed upwards to form high fold mountains.
No volcanoes, severe earthquakes
how do tectonic plates move
plates float on top of soft rock below upper mantle
earth’s core heats up mantle due to radioactive day and residual heat
causes moltenn rock to rise on convection currents
when the liquid rock reaches surface it moves crust below
it then cools and forms it own crust before sinking down again
inner core
6000 degrees celcius
very dense
solid ball of iron
cant melt as under enormous pressure
outer core
very hot and dense (4500-5500 degrees celcius), made of liquid iron
mantle
thickest layer of earth, 2900km? 1000 to 3700 degrees celcius, mantle is solid and becomes hotter and denser with depth
crust
thinnest layer of the earth
oceanic is 5-8 km thick
continental - 30-40 km thick
astenosphere
highly viscous region of the upper mantle of the earth
lies below the lithosphere, 80-200 km depths below surface
lithosphere
rigid outer part of earth. consists of crust and upper mantle