They really help in the process of Africa's state building, creating commercial networks between parts of the continent, and introducing literacy ( especially on northern part of Africa)
They also controlled the sea route between Asia and Africa and managed to maintain the relationship between Africa and the middle east
Answer:
Conglomerate rock
Explanation:
This is a type of sediment rock that has a coarse-grained texture. It is made up of small pieces of gravel-sized clasts, such as pebbles and cobbles. The mechanism of conglomerate rock formation is by consolidation and lithification.
Conglomerates are found in a variety of sedimentary environments such as, Deepwater marine, Shallow marine, Fluvial, Alluvial, and Glacial environments.
Answer:
New Orleans, located near the mouth of The Mississippi River is an example of <u>relative</u><u> </u><u>locat</u><u>ion</u><u>.</u>
<em>Hope</em><em> this</em><em> answer</em><em> correct</em><em> </em><em>:</em><em>)</em>
Hello. This question is incomplete. The full question is:
What can scientists learn from magnetic striping patterns? Select the three correct answers.
1. the cause of magnetic pole reversals
2. the year the next magnetic reversal will take place
3. the location of ancient faults caused by seismic activity
4. the exact location of the next earthquake along the California coast
5. the direction plates are moving relative to each other
6. the speed of one plate as it subducts below another plate
Answer:
The direction plates are moving relative to each other
The speed of one plate as it subducts below another plate
The location of ancient faults caused by seismic activity
Explanation:
Magnetic striping patterns are very valuable systems for understanding the factors that promote polar variability of the ocean floor. This is because these systems are formed exactly by changes in this polarity, presenting lines (similar to a zebra), which allow scientists to interpret them and have valuable information about the movement of the direction plates towards each other, the speed that a plate reaches the subduz below another plate and the location and old faults that were caused by the existence of seismic activities.
