EXAM REVIEW - THE FOURTH DIMENSION ANSWERS
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They become smaller, more rounded, more well-sorted, and less diverse mineralogically. |
All minerals found in igneous and metamorphic rocks can also occur in sedimentary rocks. Some minerals are unique to sedimentary rocks. |
With reference to minerals: an orderly arrangement of the atoms. With refernce to rocks: A texture of intergrown, interlocking grains. |
Many igneous (e.g., granite), most metamorphic (e.g., marble) and some sedimentary rocks (e.g., evaporites) have crystalline textures. |
Fast rates produce small grains. |
Vesicles form as gases bubble out of lavas. This happens most easily at the surface of a mass of lava. Since the cooling rate is very rapid at lava surfaces, the lava ends up being glass as atoms don't have the time to link up to form compounds (minerals). |
If, when lava is erupted, the melt contains needle-shaped minerals formed in the magma chamber from which the lava came, these minerals may align themselves parallel to the direction of lava flow. |
Folds are the result of plastic deformation. This tpe of deformation is favored by elevated temperatures most likely to be found at some depth beneath the earth's surface. |
Grain size tends to increase, clastic textures to become crystalline, platy minerals to align themselves. |
Oceanic trenches, volcanoes, earthquakes, mountain ranges. |
1990 |
two half lives = 1000 million years |
See 'Unfolding The History Of The Earth - Examining a Sample of Earth History'. Layer 10 is older than 200 million years. |
An object included in a matrix is older than the matrix. |
Refer to 'Unfolding The History Of The Earth - Questions and Conclusions' and come to your own decision. Be prepared to provide evidence in support of your position. |
©2003
David J. Leveson