Answer:
The Late <u><em>Laramide orogeny</em></u> was a time of active mountain building.
Explanation:
The Laramide orogeny can be described as a time of mountain building which took place during the<u><em> Late Cretaceous</em></u> period.
There is still a dispute over the beginning and ending time of the Larmide orogeny. Most of the rocky mountains which can be seen today can be attributed to this period. Deep-seated deformation was a major feature of the Laramide orogeny. During this period, mountain summits were close to sea level as compared to today.
Answer:
Answer in explanation below!
Explanation:
I used a punnett square to figure this out!
phenotypic ratio ( meaning how it will look ) = 1 : 1 ( Gg = 50% & gg = 50% )
genotypic ratio ( the allele combo ) = 1 : 1 ( Gg = 50% & gg = 50% )
I hope this helps, good luck!
In photosynthetic organisms, NADPH is produced by ferredoxin-NADP+ reductase in the last step of the electron chain of the light reactions of photosynthesis. It is used as reducing power for the biosynthetic reactions in the Calvin cycle to assimilate carbon dioxide.
the correct answer would be they receive the same amount from the ocean as they release to the atmosphere
hoped this helped have a great day :)
The answer to this question would be hydrolysis
There is amylase enzyme inside saliva that will break down starch into maltose sugar. Maltose is the sugar that <span>causing </span>the sweet sensation in the tongue. Since it will take for the reaction to happen, the sweet taste only appears after a few moments after you chewing the bread.
The reaction that was catalyzed by amylase is hydrolysis.
