Transcript THE OCEAN
THE OCEAN Ocean Zones and the Ocean Floor Text Book pages # 350 - 356 The Ocean Floor For many years, nobody knew what was at the bottom of the ocean’s floor. Because of the darkness, cold, and extreme pressure, scientists have had to develop new technology to enable them to study the deep ocean floor. Scientists discovered the best way of mapping the ocean’s floor was to use Sonar (Sound Navigation and Ranging) Sonar – A device that determines the distance of an object under water by recording echoes of sound waves. It creates a picture of the ocean’s floor using the recorded sound waves. The Ocean Floor Scientist now know that the ocean’s floor is not flat. Intertidal zone – An area that stretches from the highest high-tide line on land out to the point on the continental shelf exposed by the lowest low-tide. Intertidal Zone Intertidal zones can look like sandy beaches. Or rocky shores Intertidal Zone Organisms that live in the rocky intertidal zone must be able to tolerate the pounding waves and changes in salinity (saltiness) and temperature. The Intertidal Zone is over the beginning of the Continental Shelf Continental Shelf - A gently sloping, shallow area of the ocean floor that extends outward from the edge of a continent. Continental Shelf Continental Shelf extends in to the Neritic Zone. The Continental Shelf is also called the Neritic Zone. The Neritic Zone is full of life! Neritic Zone of the ocean that extends from the low-tide line out to the edge of the continental shelf. The shallow water over the continental shelf receives sunlight and a steady supply of nutrients washed from the land into the ocean. The Continental Shelf The Continental Shelf is home to the coral reef. Many animals live around coral reefs and this is a popular place for people to scuba dive. The Continental Slope This is where the Neritic Zone ends. The dropoff or slope at the end of a continental shelf. The Abyssal Plain - The smooth, nearly flat region of the deep ocean floor. Abyssal Plain The Abyssal Plain: Open Ocean The Abyssal Plain is also known as the Open Ocean. The Open Ocean is divided into two levels: A. The Surface Zone B. The Deep Zone Abyssal Plain: The Surface Zone The only part of the ocean that receives enough sunlight to support the growth of algae. Open Ocean - The Deep Zone The deep regions of the ocean where sunlight cannot reach. Often compared to a desert due to its harsh conditions. Few organisms live in this cold, dark, wet place. Open Ocean – Mid Ocean Ridge Longest mountain range in the world in the middle of ocean floor Mid-ocean ridges of the world are connected and form a single global mid-oceanic ridge system that is part of every ocean. Deep Zone Life Deep Zone Life Organisms often create their own light. This is known as bioluminescence Remember! Intertidal Neritic Open Ocean Shore(high to low tide) Continental Shelf Abyssal Plain Videos • http://video.nationalgeographic.com/video /news/us-ocean-floor-mappingvin?source=relatedvideo http://www.schooltube.com/video/945c3a7d 2010a9c05ff4/GMA%20%20The%20Great%20Pacific%20Garbage %20Patch