1 km 1000 m.
Sea floor spreading ratez.
For the north atlantic ocean using the map in the lab.
Spreading rate is the rate at which an ocean basin widens due to seafloor spreading.
The east pacific rise is a mid ocean ridge that runs through the eastern pacific ocean and separates the pacific plate from the north american plate the cocos plate the nazca plate and the antarctic plate.
High cretaceous ocean crust production rates have been causally linked to high global sea level and global co 2 due to increased outgassing.
Half spreading rates are based on stage rotations computed from our set of finite reconstruction rotations and spreading asymmetry estimates are based on determining the percentage of crustal accretion between pairs of adjacent isochrons by dividing the angular distance between them.
On the basis of our seafloor isochrons and rotation model we have calculated seafloor spreading half rates and relative proportions of crustal accretion i e spreading asymmetry on conjugate ridge flanks.
Seafloor spreading rates are much more rapid in the pacific ocean than in the atlantic and indian oceans.
The continents bordering the atlantic ocean for example are believed to be moving away from the mid atlantic ridge at a rate of 1 2 cm 0 4 0 8 inch per year thus increasing the breadth of the ocean basin by twice that amount.
Sea floor spreading project answer key lab 4 seafloor spreading paleomagnetism and seafloor spreading 3 7 determin chegg com seafloor spreading grade 9 free printable tests and worksheets.
Seafloor spreading rates displaying top 8 worksheets found for this concept.
Lab seafloor spreading rates worksheet answers.
Rate of spreading distance the sea floor moved length of time or r d t generally expressed as cm yr.
Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.
The rate at which new oceanic lithosphere is added to each tectonic plate on either side of a mid ocean ridge is the spreading half rate and is equal to half of the spreading rate.
At spreading rates of about 15 cm 6 inches per year the entire crust beneath the pacific ocean about 15 000 km 9 300 miles wide could be produced in 100 million years.
Some of the worksheets for this concept are lab work plate tectonics continental drift sea floor spreading and plate tectonics magnetic reversals activity plate tectonics glencoe middle school science problem and solution work 1st grade plate tectonics evidence for continental drift.
This spreading creates a successively younger ocean floor and the flow of material is thought to bring about the migration or drifting apart of the continents.
Spreading rates determine if the ridge is fast intermediate or slow.
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Seafloor spreading rates worksheet answers.
Calculating sea floor spreading.
So 1 km 100 000 cm or 10 5 cm.
