Oceanic lithosphere subducts while continental lithosphere does not due to differences in density and thickness. When these two plate types converge, the denser, thinner oceanic plate subducts into the upper mantle while the thicker, less dense continental plate remains buoyant.
The oceanic lithosphere subducts while the continental lithosphere does not because of differences in their composition and thickness. Continental lithosphere is generally thicker and less dense than oceanic lithosphere, making it rather buoyant. Consequently, when an oceanic plate and a continental plate converge, the denser, thinner oceanic plate is often readily thrust down into the upper mantle, creating a subduction zone.
This subduction process leads to significant pressure and temperature increases, causing the subducted plate to melt several hundred kilometers below the surface. The material from the melted plate gets recycled into a downward-flowing convection current, balancing the upward flow of material along rift zones.
In contrast, collisions between two continental plates usually result in the buckling and folding of Earth's crust, creating mountain ranges rather than subduction zones.
#SPJ3
a. True
b. False
other molecule?
a ADP
b ATP
C NADPH
d FADHA
Answer:
A
Explanation:
Sometimes scientists make a mistake, or error, and need to do the experiment again.
The errors can occur at various stages, including experimental design, data collection, analysis, or interpretation.
Recognizing these mistakes and errors is an important part of the scientific process.
Thus, the complete sentence is "Sometimes scientists make a mistake, or error, and need to do the experiment again".
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#SPJ6
Complete question.
Complete the sentence.
Sometimes scientists make a mistake, or ___, and need to do the experiment again.