Latitude lines are drawn horizontally across the globe whereas longitude lines are drawn vertically.
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1- The terrestrial lithosphere is composed almost of 80% by igneous rocks, they are also known as magmatic rocks and are formed at high temperatures due to magma solidification, they come from the superior mantle and terrestrial coast. Its texture is super resistant with significant hardness to obtain minerals and other derived materials. They can be divided into extrusive and intrusive.
2- Through experiments, Bowen has defined a sequence of mineral formation when a magma begins to cool. There are two types of magmatic differentiation defined by Bowen, the continuous series and the discontinuous series. In the continuous series the internal structure of the magma is not altered and all minerals have iron and magnesium, they are formed: aluminum, silica and sodium and calcium.
In the discontinuous series decreasing the temperature reacts the previously formed mineral with the existing liquid, and thus a new mineral with different internal structure and composition is formed. They are formed: olivine, pyroxena, amphibole and biotite.
The weathering of the mountain peak will be mostly through the influence of the wind, water, and ice, while the bedrock under a forest will be influenced by the plants.
Explanation:
The weathering is a process that occurs everywhere in the world, on the surface and close to the surface of the planet. This process is basically the breaking up of particles from larger masses of rocks. Which type of weathering will be dominant at a particular place depends n multiple factors, such as:
- topography
- vegetation
- climate
- presence/absence of water
A bear mountain peak will be exposed to strong winds. Also, the lack of vegetation will enable the water from the rainfall to have big influence, while in the colder months the formation of ice will contribute to significant weathering. On the other side, the bedrock under a forest will have minimal influence from wind, water, and ice, as the vegetation provides protection. The vegetation on the other hand, with its roots, as well as with the decomposition will manage to weather the rocks, both on the surface and inside the ground.
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