<span>i just did the answer on USA test prep and the answer is B high rising sea level </span>
The prediction of Darwin depends on the sizes of both the moth's tongue and the tube of blooming flowers.
<h3>What do you mean by Species?</h3>
Species may be defined as a group of organisms that can reproduce naturally with one another and create fertile offspring.
The moth's long tongue helps them to take the nectar from the tube of blooming flowers which are also very long. In this situation, the moths that possess long tongues survive in both conditions whether the tube of blooming flowerers is short or long.
This same concept was also predicted by Charles Darwin. The long tongue of the moth gives them the advantage in every situation of the tube's length.
Therefore, the prediction of Darwin depends on the sizes of both the moth's tongue and the tube of blooming flowers.
To learn more about Charles Darwin, refer to the link:
brainly.com/question/14533001
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A "broken nose" is usually identified solely as the breaking of one or both nasal bones. When we talk about fracturing involving the nose and the nasal cavity we can also include more bones that could be fractured: the vomer, t<span>he </span>perpendicular<span> plate of the </span>ethmoid<span> bone</span>, the nasal conchae and the perpendicular plate<span> of the </span>palatine<span> bone.</span>
Answer:
The rock cycle is a basic concept in geology that describes transitions through geologic time among the three main rock types: sedimentary, metamorphic, and igneous. Each rock type is altered when it is forced out of its equilibrium conditions. For example, an igneous rock such as basalt may break down and dissolve when exposed to the atmosphere, or melt as it is subducted under a continent. Due to the driving forces of the rock cycle, plate tectonics and the water cycle, rocks do not remain in equilibrium and change as they encounter new environments. The rock cycle explains how the three rock types are related to each other, and how processes change from one type to another over time. This cyclical aspect makes rock change a geologic cycle and, on planets containing life, a biogeochemical cycle.
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