Both igneous and metamorphic. They would both wear down after enough weathering
Answer: Canada follows a parliamentary system while the US follows a presidential one.
Explanation:
Answer: The overall lateral lenght of the San Andreas Fault is estimated by measuring the distance on similar terranes on both sides of the fault (continental x pacific). The lenght is increased by eathquake occurrence (here given as 5m per event) and a regular annual displacement rate (estimated in 0,10m per year).
Also, it is acceptable to consider a time lapse of 45 years between each earthquake (considering the major events of 1857, 1906, 1957 and 1989).
Those values of lenght on the fault are considered to vary from 150 to 350 miles. If we apply simple median arithmethical value of 250 miles between these numbers, against the obtained displacement rate of 5,1 meters (let´s set the annual displacement rate aside to balance) we have: 250 miles divided for 0,003 miles (5,1 meters converted to miles) is equal to: 83.333.
So, more than 80.000 thousand eathquakes (considering the movement was mostly made by these earth intercurrences) would be an acceptable number to account for the total actual displacement on the SAF.
The eyewall of a hurricane has the greatest wind speeds.
<h3>What are the characteristics of a hurricane?</h3>
There are five primary components to a hurricane: the outflow, feeder bands, eyewall, eye, and storm surge. The high-level clouds that are leaving the hurricane are known as outflow. The locations where it rains heavily and there are strong winds are known as feeder bands. As the storm gets stronger, they become more obvious. The hurricane's eyewall is a belt of dense clouds, strong wind, and heavy rain. Here, the air is moving erratically in the direction of the cloud's eye and upward. The storm's calmer center is known as the eye. The torrent of ocean water pushed inland as the cyclone nears land is known as a storm surge.
Learn more about hurricane's eyewall here:
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