Sedimentary rocks ar he secondary rocks to form over the earth due to the competition and solidification of sediments in various layers of rocks. In geologically cross-breeding is the cross-stratification of the rocky mass layering which is aligned to the angle of the bedding plane.
It forms depositional of the inclined surfaces such as triples and dues. And is indicated by the depositional environment of the earth like the deltas.
The cross-bedding tells the geologist of the area's historical significance and the conditions in which the present landscape has evolved. Other sources being the internal sorting patterns and Geometries like the tabular horizontally extended beds and the cross-beds formed by the inclined base of the rocks.
<u>An example of the phenomenon is cross-bedding in the Waddens Cove formation of Nova Scotia.</u>
One meter is 100 cm which implies 30 meters is 30*100 cm which is 3000 cm. So the continent has moved 3000 cm in 1000 years. So the distance traveled in one year will be 3000 cm divided by 1000 that is 3000/1000 which is 3cm/year So the rate at which a continent is traveling is 3 cm/year.
Explanation:the sun is very hot so it automatcily rules out a b it cant be d because the sun has to high magnetic pull there are no spots that have less or more so it has to be c or e
