Answer:
The Finance Cluster and the Business, Management, and Administration Cluster
Explanation:
Yes because if the car is old and gets totaled you would want insurance to get some money back from your old car to put towards a new one
Yes Because its your fault your gonna need to pay for their damages. ( i live in Florida so ion know much bout that cause we a no fault state )
Answer:
B. Employers are not liable for the acts of their supervisors, regardless of whether the employer is aware of the sexual harassment act.
Explanation:
In this case, the Supreme Court mentioned that an employer isat risk. That means that the empolyer does nor have a defense when sexual harassment by a supervisor involves a tangible employment action. Courts hope that employers educate supervisors so they do not commit any type of behavior that could be considered as sexual harassment. Also, all employees must be educated so as to understand their rights and responsibilities .
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.
