unit 4 1-50 test 51-55 quiz 6 56-60 quiz 7 Flashcards
what is the diameter of the earth?
8,000 miles
what is the diameter of the sun?
800,000 miles
what is earths circumference?
24,000 miles
describe earths three distinct, concentric layers
iron core is larger than 1/2 of earths diameter
mantle composed of ultramafic rocks and minerals
two types of earth crust
oceanic mafic crust (basalt)
continental felsic crust (granitic)
what two types of crust does the earth have?
oceanic mafic crust (basalt)
continental felsic crust (granitic)
describe the three sources of earths residual heat?
heat from gravitational energy
heat derived from kinetic energy generated by planetesimal collisions
heat generated from later meteor impacts (4.6-3.8 billion years)
heat from within the earth is continually generated by
radioactive decay
with melting metallic iron and nickel sank to the center of the earth to form the iron core (iron catastrophe)
the remaining melt was composed of mafic or basaltic rocks that surround the ultramafic earths mantle
what is a lithosphere and where is it located?
rigid outer layer containing crust and a frozen part of the upper mantle
what is the asthenosphere and where is it located?
partially melted upper mantle that has plastic-like properties
describe the lower mantle and where is it located?
(sometimes called the mesosphere) solid layer of rocks between the asthenosphere and iron core
describe the components of earths core and where are they located
liquid iron core molten iron with some nickel and rocks (half diameter of earth)
solid iron core +6,000 degrees celceus
what happened to most of the hydrogen and helium that accumulated with earths mass?
most of it escaped from earth because earth did not have enough gravity to hold these elements within its atmosphere
how much free oxygen was available very early in earths history?
there was almost no free oxygen with earths original atmosphere
what does the presence of pyrite grains in early sedimentary rocks imply?
proof that there was no free oxygen cause they didn
describe the occurrence of banded iron formations during early times(2.5-2.0 billion years)
having more generated free oxygen the banded iron formations (that require abundant oxygen) became thick and cover vast areas. by this time, free oxygen consumed all the dissolved iron in the oceans
which ancient life forms were present at least 3.5 billion years ago that began creating earths free oxygen?
ancient bacteria and algae these life forms used photosynthesis to combine co2 and water into organic molecules and release free oxygen as a waste product into the atmosphere
what is the approximate percentage composition of earths atmosphere today?
approximately 78% nitrogen and 21% oxygen (rounded 80%-20%)
what happened to most of the co2 that was present in early earths atmosphere?
a small fraction of co2 was converted into oxygen
seawater absorbs co2 from the atmosphere
because of limestone we have very little co2 in our atmosphere
how long did it take earths oceans to reach its current salinity levels?
as early as the oceans formed 3.5 to 4.4 billion years
alfred wegener was famous for proposing which scientific theory?
continental drift theory in 1915
what was pangaea.
the last known super-continent in which all the present-day continents did not stay in the same area over geologic time.
remember that wegener used fossils, striations and age of rocks to prove continental drift?
a super continent model because
similarities in shoreline of continents
dist\tinctive rock formations on matching continents
distinctive matching fossil groups
why was the theory of continental drift rejected?
he could not provide a mechanism to move the continents
what is the current theory about the creation of earths magnetic field?
creates a huge magnetic shield that prevents the earth from being blasted by cosmic particles from the sun