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Ivahew [28]
3 years ago
11

Which group first settled in New Zealand?

Geography
2 answers:
Dmitry [639]3 years ago
3 0
The awnswer is b.

hope  this helped
tester [92]3 years ago
3 0
I believe A is your correct answer, Aborigines.
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What are the differences and similarities between topographic maps and orthophoto maps in terms of data source used to create th
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<span>The correct answer for the question that is being presented above is this one: "Topographic maps feature contour lines to portray the shape and elevation of the land. Topo maps render the three-dimensional ups and downs of the terrain on a two-dimensional surface. It also includes contours. Orthophoto maps</span> show land features using color-enhanced photographic images which have been processed to show detail in true position. They may or may not include contours."
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Please please please help me out now.....​
gtnhenbr [62]

Answer:

Aquifer

Explanation:

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D. the arrangement of mineral grains into a foliation

Explanation:

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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.

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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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2. Recrystallization of minerals to form new grains that grow in the direction of the preferred orientation.

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How does the tilt of Earth's axis affect how the sun's rays strike eachother?
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