Shear stress causes objects to be smeared out in the direction of applied stress.
sedimentary rocks undergo metamorphism under certain heat and pressure to give the metamorphic rocks. the affect of this formation on environment is negligible as this frames the part of rock cycle. further these metamorphic rocks melts to form magma. magma further cools and solidify to form igneous rocks.
The minerals which appear are quite similar chemically but not physically. In metamorphic rocks, foliation can be seen-bands of rocks formed by great pressure, whereas in igneous rocks, this is never present because igneous rocks specifically need to have just previously melted, so therefore, these bands are disorganized and lost. Therefore, igneous rocks clearly don't seem to have any patterns unlike metamorphic rocks. Also, some minerals only form during metamorphism/melting+cooling. Therefore, the chemical composition is usually slightly different. E.g. Garnet is only formed under high-grade metamorphism-high temperatures and pressures. Also, the crystals sizes in igneous rocks depend on how long the rock has had to cool. So therefore, an igneous rock's crystals could be a lot bigger or smaller than a metamorphic rock's crystals. But then again, both rocks have interlocking crystals unlike sedimentary rocks, so in that way, at first glance, they can sometimes look very similar, (depending if it is intrusive of extrusive-metamorphic rocks will look a lot more like intrusive igneous rocks because of how the air affects the magma, (how magma looks when it cools), extrusive rocks look different, (blacker, smaller crystals etcetera).
Soil structure is the term used to describe the arrangement of soil particles into aggregates or peds. This arrangement affects soil properties such as porosity, permeability, and root penetration.
Soil composition refers to the arrangement or proportion of different components in soil, which include minerals, organic matter, water, and air. It is an important factor that affects soil fertility, structure, and ability to support plant growth.
The greatest volume of metamorphic rock is produced during mountain-building events, such as collision of tectonic plates or subduction zones. The intense pressure and heat generated during these processes can reshape existing rocks into metamorphic rocks.
sedimentary rocks undergo metamorphism under certain heat and pressure to give the metamorphic rocks. the affect of this formation on environment is negligible as this frames the part of rock cycle. further these metamorphic rocks melts to form magma. magma further cools and solidify to form igneous rocks.
Plastic deformation in metamorphic rock primarily alters the rock's texture and structure. It affects the alignment of mineral grains, leading to foliation or lineation, which can enhance the rock's strength and change its overall appearance. This process occurs under high temperature and pressure conditions, allowing minerals to recrystallize and reorganize without breaking. Consequently, plastic deformation significantly influences the physical characteristics and properties of the metamorphic rock.
direction affects power by saying yo this is the right answer..
Metamorphism affects basalt by altering its mineral composition and texture due to increased temperature and pressure conditions, often resulting in the formation of metamorphic rocks such as amphibolite. During this process, minerals in basalt, such as plagioclase and pyroxene, can recrystallize or transform into new minerals like garnet or hornblende. The resulting texture may become more foliated or granular, depending on the specific metamorphic conditions. Overall, metamorphism enhances the physical properties and stability of the original basalt material.
Yes, the rock cycle significantly affects minerals in rocks. As rocks undergo processes like weathering, erosion, and metamorphism, the minerals within them can change in composition, structure, or form. For example, sedimentary rocks can form from the accumulation and cementation of mineral particles, while metamorphic rocks can develop new minerals under heat and pressure. This dynamic cycle continually alters the mineral content of rocks throughout geological time.
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The minerals which appear are quite similar chemically but not physically. In metamorphic rocks, foliation can be seen-bands of rocks formed by great pressure, whereas in igneous rocks, this is never present because igneous rocks specifically need to have just previously melted, so therefore, these bands are disorganized and lost. Therefore, igneous rocks clearly don't seem to have any patterns unlike metamorphic rocks. Also, some minerals only form during metamorphism/melting+cooling. Therefore, the chemical composition is usually slightly different. E.g. Garnet is only formed under high-grade metamorphism-high temperatures and pressures. Also, the crystals sizes in igneous rocks depend on how long the rock has had to cool. So therefore, an igneous rock's crystals could be a lot bigger or smaller than a metamorphic rock's crystals. But then again, both rocks have interlocking crystals unlike sedimentary rocks, so in that way, at first glance, they can sometimes look very similar, (depending if it is intrusive of extrusive-metamorphic rocks will look a lot more like intrusive igneous rocks because of how the air affects the magma, (how magma looks when it cools), extrusive rocks look different, (blacker, smaller crystals etcetera).
Soil structure is the term used to describe the arrangement of soil particles into aggregates or peds. This arrangement affects soil properties such as porosity, permeability, and root penetration.
Soil composition refers to the arrangement or proportion of different components in soil, which include minerals, organic matter, water, and air. It is an important factor that affects soil fertility, structure, and ability to support plant growth.
No. The order of adding vectors does not affect the magnitude or direction. of the result.
It will cause acceleration in the direction of the net force.
Beryl, for one, reacts by emitting X-rays characteristic of Be.