In addition to access to markets and national resources, another reason for europes interest in dominating africa and asia was to

Another reason for Europe interest in dominating Africa and Asia was to SEEK PROFITABLE INVESTMENT OPPORTUNITIES FOR SURPLUS CAPITAL.

During the period of 1870s and 1900, Africa and Asia faced a lot aggression from the Europeans, which eventually led to their conquest and the colonization of their continents. The major reasons why the Europeans had interest in these two continents were because of economic gain, political domination and religious domination. The major economic aim of the European was to get the control of market and resources of these continents in order to increase their own capital base.

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the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)