Answer:
Exhibit greater sensitivity to low-level stimuli than extroverts
Explanation:
It is proven through research that introverts have higher sensitivity to low-level stimuli than extroverts. This is because introverts have higher cortical arousal levels. On the other hand, the extroverts are found to have lower cortical arousal levels and this results in need for external excitement and stimulation. Also, introverts have lower pain thresholds than extroverts and react strongly to sensory stimulation. Hence, the only correct option provided here is that introverts exhibit greater sensitivity to low-level stimuli than extroverts.
The sea protected both rome and india and also the sea provided them transportation and food
Answer: correlation vs. causation
Explanation:
Correlation assesses the relationship between variables and can be in the same direction, where the increase in one exists as the same time as an increase in the other variable or inverse where an increase in one variable occurs when there is a decrease in the second variable. However, this correlation does not indicate causation.
Causation signifies that one variable is responsible for the occurrence of an event in the other variable. Clearly, there is no cause and effect between the number of mules and doctorate degrees in a state. Here, there is a correlation but a fundamental causative factor is absent between the two events.
It does represent a function because there are no repeating x values.
Answer:
Cores taken near the oceanic ridges show the age and thickness of the sediment increases as you move away from the ridge. This supports seafloor spreading because it indicates the
- the younger crust nearest the ridges has not been around long enough to accumulate the same thickness of sediment as sections farther out did.
Explanation:
- Seafloor spreading is such a process which takes place when a volcano occurs. Due to which a new oceanic crust is formed which gradually move away from the ridge.
- Cores taken near the oceanic ridges show the age and thickness of the sediment increases as you move away from the ridge. The younger crust nearest the ridges has not been around long enough to accumulate the same thickness of sediment that's why the the sections of crust that are further from the ridges have longer time to have more thickness and age.
