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enot [183]
3 years ago
9

Discuss the ways in which North American culture is adapted to high levels of spatial (geographic mobility) mobility

Geography
1 answer:
leonid [27]3 years ago
3 0

Answer:

Discussed as below.

Explanation:

  • The state of North America is divided into 50 states among which there lies the concept of geographic mobility as the state on the map is aligned in the shape of boxes line square on a plain sheet of paper.
  • By geographic mobility, we mean how the population and goods move over time. It also is a static measure that migration among the population. This mobility is largely due to the socio-psychological factors of a community.
  • Data on US mobility patterns given by The USCB united states census bureau, that is based on the comparison of the place of residence people make each year. The CPCS current population survey records all such data of people on the move.
  • These may include work-related data, marital status, and retirement also. Other factors like the size of the population in and out of the census bureau.
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The petrographic characteristics of these rocks are especially complicated, given the solid state transformation processes that they have suffered, usually accompanied by intense deformation. Due to the gradual nature of metamorphic (and deformational) transformations, the characteristics of this type of rock also range from igneous or sedimentary to purely metamorphic.

<u>Foliation </u>

The term foliation (foliatus: leaf-shaped) refers to any planar (almost flat) arrangement of mineral grains or structural features of the interior of a rock. Although there is foliation in some sedimentary rocks and even in a few types of igneous rocks, it is a fundamental characteristic of rocks that have undergone regional metamorphism, that is, rocky units that have folded and deformed greatly. In metamorphic environments, foliation is caused, ultimately, by the compressive efforts that shorten the rock masses, causing the mineral grains of pre-existing rocks to develop parallel or almost parallel alignments. Examples of foliation are the parallel alignment of minerals with planar habit and / or elongated minerals; the parallel alignment of mineral particles and flattened edges; the compositional bandeado where the separation of dark and light minerals generates a laminar appearance, and the blackboard when the rocks easily separate into thin and tabular layers along parallel surfaces. These different types of foliation can be formed in many different ways, such as:

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3. Changes in shape in equidimensional grains to elongated shapes that align in a preferred orientation.

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