You wanna die? Talk about why you don’t want to die.
Answer:
d. officers becoming personally involved with informants.
Explanation:
An informant is a person who gives his testimony in relation to a situation as a way to help in the investigation of something. These people cannot be considered a witness of a situation, because they are not formally obliged to speak the truth about the facts of the situation (the witness is obliged to speak the truth), and they can tell fanciful, uncooperative and incorrect information.
In this case, it is extremely unethical for the information that an informant provides to be overestimated, because that information may be false. moreover, an informant cannot be intimidated or coerced into contributing to a given situation, nor can he be deceived about its relevance in the investigation, through false praise. However, in terms of ethics and morals, nothing prevents officers from personally getting involved with informants.
Answer:
Informed and active members of their community think and act with integrity and respect for others and the natural environment, understanding and contributing to the common good. ... They have an understanding of our systems of government, and actively engage in decision-making in a variety of ways.
brain list please
The thickness of the continental crust is normally 40 km (25 miles), whereas the thickness of the oceanic crust is only 6 km (4 miles). The difference in the average heights of the continental and oceanic crust is a result of the varying densities of the lithospheric rock.
Because of its greater buoyancy and lower density, the continental crust floats significantly higher in the mantle. The average depth of the marine crust is 3,790 meters, while its average height above sea level is 840 meters (2,750 feet) (12,400 feet). The two main layers of the Earth's surface are created by this density differential.
Subduction zones are where the majority of continental crust is created. Rock scraped off the top of oceanic plates when they subduct beneath continental boundaries contributes to lateral expansion (the submarine edge of the continental crust). These boundaries are identified by lines of volcanoes, frequently in the form of volcanic arcs that add to the crust. Additionally, volcanic arcs known as island arcs are produced by subduction zones found inside ocean basins (when one oceanic plate sinks beneath another).
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