To calculate 10x238/12, you need to first multiply 10 and 238 which gives you 2380. Then divide the result by 12, which gives you 198.33 (rounded to two decimal places).
Therefore, 10x238/12 = 198.33.
how do i find 10x238/12
3 answers
The unequal heating of Earth's surface can cause local winds to form. The denser cooler air rushes in to replace the less dense warmer air forcing the warmer air upwards creating the local winds in a given area.
The unequal heating of Earth's surface can cause local winds to form. The denser warmer air rushes in to replace the less dense cooler air forcing the cooler air upwards creating the local winds in a given area.
The unequal heating of Earth's surface can cause local winds to form. The less dense cooler air rushes in to replace the denser warmer air forcing the warmer air upwards creating the local winds in a given area.
The unequal heating of Earth's surface can cause local winds to form. The less dense warmer air rushes in to replace the denser cooler air forcing the cooler air upwards creating the local winds in a given area.
The unequal heating of Earth's surface can cause local winds to form. The denser warmer air rushes in to replace the less dense cooler air forcing the cooler air upwards creating the local winds in a given area.
The unequal heating of Earth's surface can cause local winds to form. The less dense cooler air rushes in to replace the denser warmer air forcing the warmer air upwards creating the local winds in a given area.
The unequal heating of Earth's surface can cause local winds to form. The less dense warmer air rushes in to replace the denser cooler air forcing the cooler air upwards creating the local winds in a given area.
The correct statement is:
The unequal heating of Earth's surface can cause local winds to form. The denser cooler air rushes in to replace the less dense warmer air, forcing the warmer air upwards and creating the local winds in a given area.
The unequal heating of Earth's surface can cause local winds to form. The denser cooler air rushes in to replace the less dense warmer air, forcing the warmer air upwards and creating the local winds in a given area.