<u>Answer</u>:
The outside of the <em>Pacific Ocean remains around 40 cm higher than the Atlantic Ocean concerning the 1000-decider surface</em>, and the North Atlantic and North Pacific stand individually around <em>14 and 17 cm higher than the South Atlantic and Pacific.</em>
<u>Explanation:</u>
<em> The Atlantic Ocean is known to have higher ocean surface saltiness than the Pacific Ocean at all scopes. </em>
This is believed to be related with the Atlantic Meridional Overturning Circulation and profound water development in the high scope <em>North Atlantic – a wonder not present anyplace in the Pacific.</em>
<span>False, Agriculture greatly alters the composition of the organic content of the soil. The soil nutrients completely depend on the crop that has been grown in this location the prior several growing seasons. Many crops use high levels of nitrogen and phosphorus and therefore leave the soil lacking these nutrients. Reworking the left over material into the soil after the crops helps a little but crop cycling is required to really replenish the soil. This would mean planting crops the add nutrients back into the soil such as legumes.</span>
They are the descendants of Persian Jews.
From the Persian Empire aka Iran.
Answer and Explanation:
About two-thirds of the Earth's surface lies beneath the oceans. The depths of the open ocean were mostly a matter of speculation before the 19th century. Most people thought ocean floor was flat and featureless. In the early 16th century, a few navigators found that the open ocean can differ considerably in depth by taking soundings with hand lines, which shows that the ocean floor was not as flat as it believed.
At the beginning of the 1950s, scientists used magnetic instruments adapted from airborne devices to recognize odd magnetic variations across the ocean developed during World War II to detect submarines. They found that the iron-rich and volcanic rock make up the ocean floor-- contains a strongly magnetic mineral and can distort compass readings. In the early 18th century, this distortion was recognized by Icelandic mariners. Magnetite gives measurable magnetic properties; these magnetic variations help to study the deep ocean floor.