To determine the texture of rock when rock is forming , you must test the mohs hardness scale and wait for the feedback. Then analyze the information into categories of largest to smallest. Once you do that you must share your answer if it is either igneous, metamorphic, or sedimentary.
The relationship between an igneous rock's texture and where it was formed is that the texture depends on whether or not the rock is an extrusive rock or an intrusive rock. Those two different types of classifications for rocks tell you what the texture will be. For example, Intrusive rocks have a coarse-grained texture like granite and extrusive rocks have a fine-grained texture like basalt.
What is the relationship between a rock's texture and where it was formed?
Texture refers to the size of the particles or mineral crystals that make up the rock.
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Its color
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because fossils are in sedimentary rock
fossils of once living things provide clues that support contenental drift
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Its color
Definitions: an author may provide a word's meaning within the sentence. Synonyms: words with similar meanings can help decipher the meaning of an unfamiliar word. Antonyms: words with opposite meanings can provide clues to the meaning of an unfamiliar word. Descriptive details: surrounding information can hint at the meaning of a word. Example sentences: examples within a text can provide context for unfamiliar words.
A rock's texture will most definitely yield clues as to how a rock formed and often to where it formed. Coarse grained igneous rocks formed below the surface from magma. Fine grained igneous rocks formed at or near the surface from lava. Large crystals scattered among fine grained rock indicates an igneous rock that may have partly formed underground, and finished forming above ground. Layers can indicate rocks that are sedimentary and the grain size can indicate the source of the sediments. Banded and foliated rocks indicate high pressure formation and metamorphosis, and the coarse recrystallization of quartz in quartzite indicates a high temperature metamorphosis. These are just a few examples. For information on different rock textures, click on the link below.
A rock's texture will most definitely yield clues as to how a rock formed and often to where it formed. Coarse grained igneous rocks formed below the surface from magma. Fine grained igneous rocks formed at or near the surface from lava. Large crystals scattered among fine grained rock indicates an igneous rock that may have partly formed underground, and finished forming above ground. Layers can indicate rocks that are sedimentary and the grain size can indicate the source of the sediments. Banded and foliated rocks indicate high pressure formation and metamorphosis, and the coarse recrystallization of quartz in quartzite indicates a high temperature metamorphosis. These are just a few examples. For information on different rock textures, click on the link below.
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Mineral texture provides clues as to the origin of the rock particles and the processes which lead to the rock's formation. Texture would include the size and arrangement of the mineral crystals or particles found in the body of a rock.
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They can learn about conditions deep inside Earth, where these rocks formed. In addition, forces inside Earth sometimes blast rock to the surface from depths of more than 100 kilometers. These rocks provide clues about the interior.