We can calculate an average rate of seafloor spreading by measuring the distance
ID: 298840 • Letter: W
Question
We can calculate an average rate of seafloor spreading by measuring the distance between MOR's, then divide the distance by the and age of seafloor rocks collected there (e.g. such as from ODP cores). Recall: Rate (r) = Distance (d) ÷ Time (t) or r = d / t
1. What is the average spreading rate of the Atlantic Ocean basin measured along the Equator? Use the outer edge of the continents of S America and Africa to determine the edge of the oceanic plate. The oldest ocean floor, basalt rocks collected at the base of the continental shelf are midCretaceous in age. (Show your calculations below)
http://www.science.earthjay.com/instruction/CR_eureka/GEOL_15/lecture_05/geol_15_activity_2.pdf
Explanation / Answer
1. The distance traveled by the North American plate from the African plate from the mid cretaceous( approximately 90my) age is 2250 km.
so the half spredding rate of the Antlantic ocean basin is r = d / t
here d = distance traveled by the plate = 2250km
t = time = 90 my
r 1/2= 2250 / 90
= 25 km / my
It is equal r1/2 = 2.5 cm / year
the full spreadding rate of atlantic basin r = r1/2 *2
= 25*2 = 50km / my
i.e equals to r = 5 cm / year
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