The five principles used to determine the relative ages of rock include original
A) horizontality, superposition, cross cutting, inclusion, and faunal succession.
B) horizontality, nonconformity, cross cutting, inclusion, and faunal succession.
C) inclusion, superposition, uniformitarianism, horizontality, and fossil succession.
D) horizontality, uniformitariansism, cross cutting, stromatolite, and faunal succession.
Question 2
When tilted or folded sedimentary layers are covered by younger, horizontal rock layers it is called
A) an intrusion.
B) an angular unconformity.
C) a syncline.
D) conformable.
Where mangrove diversity is high, mangrove species show clear patterns of vertical zonation relative
The original Magdeburg hemispheres (lower left) used to demonstrate Otto von Guericke's vacuum
GENERAL PRINCIPLES OF CELL COMMUNICATION
The relative proportions of body region representation in the motor cortex (anterior to the central
Determining the Ages of Rocks Using Fossils
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