Arabian Sea
After suffering from starvation and dehydration, most of the crew died before the survivors were rescued in February In retelling the story of the crew's ordeal, Philbrick utilizes an account written by Thomas Nickerson , who was a teenage cabin boy on board the Essex and wrote about the experience in his old age; his account was lost until but was not authenticated until before being published, abridged, in The book also utilizes the better known account of Owen Chase , the ship's first mate , which was published soon after the ordeal.
In the Heart of the Sea won the U. National Book Award for Nonfiction. The film was scheduled for release in the US on December 11, , but was released in major markets like Brazil, Russia, India and 37 other countries, as well as parts of the US, on December 3, to avoid competition from Star Wars: From Wikipedia, the free encyclopedia.
Seven Seas - Wikipedia
For the film adaptation, see In the Heart of the Sea film. In the Heart of the Sea film.
The Tragedy of the Whaleship Essex. Retrieved 6 November In the winter of , the New England whaling ship Essex was assaulted by something no one could believe: Both are about 10 times saltier than seawater.
Lakes are temporary storage areas for water. Rivers and streams bring water to the lakes, and other rivers carry water out of lakes. Thus, lakes are really only wide depressions in a river channel that have filled with water.
What's the difference between an ocean and a sea?
Water flows in one end and out the other. All the water that flows into these lakes escapes only by evaporation. When water evaporates, the dissolved salts are left behind. So a few lakes are salty because rivers carried salts to the lakes, the water in the lakes evaporated and the salts were left behind. After years and years of river inflow and evaporation, the salt content of the lake water built up to the present levels. The same process made the seas salty.
Rivers carry dissolved salts to the ocean. Water evaporates from the oceans to fall again as rain and to feed the rivers, but the salts remain in the ocean. Because of the huge volume of the oceans, hundreds of millions of years of river input were required for the salt content to build to its present level.
Rivers are not the only source of dissolved salts. About twenty years ago, features on the crest of oceanic ridges were discovered that modified our view on how the sea became salty. These features, known as hydrothermal vents, represent places on the ocean floor where sea water that has seeped into the rocks of the oceanic crust, has become hotter, and has dissolved some of the minerals from the crust, now flows back into the ocean.
With the hot water comes a large complement of dissolved minerals. Estimates of the amount of hydrothermal fluids now flowing from these vents indicate that the entire volume of the oceans could seep through the oceanic crust in about 10 million years. Thus, this process has a very important effect on salinity.