I believe the answer is: experience-dependent
experience-dependent brain function refers to the function that crated after individual experiences somehow alter the way we perceive everything around us. This could be seen in things such as the acquiring process of a language, and the development of spatial/cognitive skills after forcing ourselves into a certain daily habit.
Answer:
False
Explanation:
False statement.
Kant claims that desires and feelings are contingent. Morality needs to be based in necessity.The categorical imperative is a device that tests our interests and emotions to determine whether our behavior follows the moral law or not. It is important to base morality on necessity. Kant insists that a conceptual necessity is the ultimate reason / justification for any moral action.
Answer: Racism is a problem in Colombia and everywhere else and the problem is people choosing to to except others for their skin color, race, religious belief, or ethnicity
Explanation:
Answer:
stereotype; better
Explanation:
In one study, participants were presented with a list of traits about a hypothetical person while simultaneously watching a video about Indonesia. In one condition, the traits were accompanied by an applicable stereotype (e.g., skinhead); in the other condition, the traits were presented without a stereotype. Results showed that participants in the stereotype condition remembered the trait information better and performed better on a surprise multiple-choice quiz about Indonesia.
Because of the fluctuation.
In most ocean regions, wind-driven circulation, which has been the focus of discussions so far, does not reach below the first kilometer of the oceans. The renewal of the waters below this depth is achieved by currents that are guided by differences in density produced by effects of temperature (thermals) or salinity (halinos). The associated circulation is therefore referred to as the thermohaline circulation. Since these movements are mostly quite slow, it is very unlikely to use direct current meters (current meters); they are usually estimated by the distribution of the physical properties of the water and the application of geostrophy.
The driving force of thermohaline circulation is the formation of water bodies. Water bodies with well-defined salinity and temperature characteristics are created in specific regions by surface processes; they then sink and slowly mix with other bodies of water as they move. The two main processes for the formation of water bodies are deep convection and subduction. Both are linked to the dynamics of the mixing layer on the surface of the ocean; thus, it is necessary to first discuss thermohaline aspects of the surface ocean first.
