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.
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The sand is primarily derived from weathering of Cretaceous sandstones in North Africa. When these sandstones were deposited in the Cretaceous, the area where they are now was a shallow sea. The original source of the sand was the large mountain ranges that still exist in the central part of the Sahara. These mountains are volcanic and intrusive, and the granite rock weathers out to leave behind quartz sand grains that are carried by rivers to the sea. These sand deposits eventually formed into sandstone, and as they were uplifted began to weather and break down into sand again.
Only about 10% of the Sahara is actually covered by sand, and parts of the Sahara are in fact covered by soil. More than half of the area comprises soils known as yermosols, with shallow profiles over gravel or pebble beds. These soils have been developing over the past 50 million years.
Answer:
the first one as in, 'Then I followed the steps to build the frame and shape my volcanic mountain.'
Explanation: