<u>Fourth Amendment Law Enforcement explained below: </u>
- The Fourth Amendment permits the right to be free from non-reasonable searches by the government.
- The government should complete an analysis of the commitment of crime that had taken place before the search warrant to be given.
- They also have permission to search the area whether the area has done any illegal things.
- The government is much more careful in protecting the law right to liberty and they are so consciousness in not disturbing the normal people.
Answer:
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are you a conexus student as well
Explanation:
Answer:
Correct Answer:
E. That the manufacturer did not give a sample or a model of the seeds.
Explanation:
As an attorney of the manufacturer, the best argument in the case between my client and the seed buyer, Joe would be on the fact that, the manufacturer did not give a sample or model of the seeds to Joe to verify if it meets his requirements.
<em>Also, Joe never requested to see sample of the seeds as was standard with buying of agricultural products.</em>
A cost-Benefit analysis (CBA) is the process used to measure the benefits of a decision or taking action minus the cost associated with taking the action. A CBA involves measurable financial metrics such as revenue eared or costs saved as a result of the decision to pursue a project.
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An earthquake is caused by a sudden slip on a fault. The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel.
In California there are two plates - the Pacific Plate and the North American Plate. The Pacific Plate consists of most of the Pacific Ocean floor and the California Coast line. The North American Plate comprises most the North American Continent and parts of the Atlantic Ocean floor. The primary boundary between these two plates is the San Andreas Fault. The San Andreas Fault is more than 650 miles long and extends to depths of at least 10 miles. Many other smaller faults like the Hayward (Northern California) and the San Jacinto (Southern California) branch from and join the San Andreas Fault Zone.
The Pacific Plate grinds northwestward past the North American Plate at a rate of about two inches per year. Parts of the San Andreas Fault system adapt to this movement by constant "creep" resulting in many tiny shocks and a few moderate earth tremors. In other areas where creep is NOT constant, strain can build up for hundreds of years, producing great earthquakes when it finally releases.