Answer:
It is not safe
Explanation:
Because if you have ear buds in you cannot hear siren's of police,fire, or tornado warnings (the tornado warnings a little bit of a long shot but u get the point I think) also you won't be able to hear someone honk at you if they are trying to prevent an collision or warn you of something you would be otherwise oblivious to.
Answer: your question about the answer to the question is confusing to me
Explanation: I don’t know how to do it
Answer:
traditional and non traditional intersections
Explanation:
Answer:
No, on the contrary, I am totally against the granting of extraordinary powers to any political leader, whatever the issue. On the contrary, I think that every government official must have limited powers, controlled by the other branches of government. In this way, they will not be able to exceed their prerogatives, affecting the freedoms and rights of citizens.
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.
