Mapping the Ocean Floor

Slides:



Advertisements
Similar presentations
Chapter 14 The Ocean Floor.
Advertisements

Journey to Bottom of the Ocean
Exploring the Ocean Since ancient times people have studied the ocean such as waters and ocean floor It provides food and services, and serves as a route.
Ocean Floor Features Chapter 14, Section 2.
OCEAN FLOOR.
Features of the Ocean Floor
The Seafloor and its Structures
Deep Seafloor Features Mapping the seafloor – Bathymetry- study and mapping of seafloor elevations – Techniques Early explorers measured depth with rope.
The Ocean Floor Continental slope Volcanic island Continental shelf
Unit 6: Ocean Floor Structure. Sea Floor Features: Earth's rocky surface is divided into two types: oceanic crust, with a thin dense crust about 10 km.
Ocean Bottom Chapter 3. Will lead to unlocking some of the mysteries of the ocean and may give insight into Earth’s past.
Bathymetry of the Ocean Floor The ocean floor is mapped by SONAR. (Sound navigation and ranging) Depth = (time x 1500 m/sec)/2 (round trip) At 25 degrees.
EXPLORING THE OCEAN FLOOR pbs
The Ocean Basins. Five Major Oceans Arctic Pacific IndianAtlantic Southern.
Warm Up What are the four minerals that compose salt water? 1. What are the four minerals that compose salt water? 2. What are the three reasons.
Ocean Topography Main Features.
Ocean Landforms.
The Ocean Floor.
Exploring the Ocean. Why is the ocean difficult to study? 1.It is DEEP! 3.8 km (that’s twice as deep as the Grand Canyon) 2.It is DARK and COLD! (Only.
Ch. 20 The Ocean Basins Ch Features of the Ocean Floor.
The Ocean Basins Section 2 Section 2: Features of the Ocean Floor Preview Objectives Features of the Ocean Floor Continental Margins Deep-Ocean Basins.
3 Bathymetry of the Ocean Floor Bathymetry= measuring ocean depths and charting the shape or topography of the ocean floor “Sounding” lines (started in.
Deep Ocean Technology & The Ocean Floor
Geological Oceanography Ocean Topography The scientific study of the origin, history, and structure of the earth.
The Earth’s Oceans A Dynamic System where many physical and chemical changes are taking place!
1 THE WORLD OCEAN Covers 71 % of the planet (59.4 % is seafloor) Divided into major basins – Atlantic (N & S) Pacific Arctic Indian Southern Pacific –
Topography of the Ocean
Journey to Bottom of the Ocean
Chapter 18 Ocean Motion Chapter 19 Oceanography Chapter 18.3 and 19.1 Notes Guide.
The Physiography of the Ocean Floor
Oceans Basins. Ocean Bathymetry ► The study of underwater depth and ocean floor. ► In the same way that topographic maps represent the three-dimensional.
Physical Oceanography Physical Oceanography Ocean Topography.
Mapping the Ocean Floor. Essential Questions  What are some of the features found on the ocean floor?  What technology is used to map the ocean floor?
Topography of the Ocean Floor.
20.2. Continental Margins The line that divides the continental crust from the oceanic crust is not always obvious. Shorelines are not the true boundaries.
OCEANIC Lithosphere PREDICT: What percent of the earth is covered in water? What percent is land? Explain your prediction.
Geological Features at Sea and on Land. Pangea Nearly 100 years ago Alfred Wegner thought that the map looked like a giant jigsaw puzzel. Nearly 100 years.
Oceanic -- Continental Match-Up. Abyssal Plain Continental shelfOce\ basin Continental Shelf The edges of the continents slope down from the shore into.
Journey to Bottom of the Ocean
Ocean Topography Main Features.
Subsurface Topography
The Ocean Floor.
Ocean Topography Main Features.
Subsurface Topography
Ocean Topography.
Ocean Topography Main Features.
Ocean Topography Main Features.
Ocean Topography Main Features.
Journey to Bottom of the Ocean
Ocean Topography Main Features.
Ocean Topography Main Features.
Ocean Features.
Ocean Features.
Bathymetry of the Ocean Floor
Journey to Bottom of the Ocean
Ocean Features.
EXPLORING THE OCEAN FLOOR
Continental Slope The descending slope which connects the sea floor to the continental shelf.
Ocean Floor Features.
The Ocean Basins.
Ocean Topography Main Features.
Ocean Features.
Ocean Features.
Ocean Features.
Ocean Topography Main Features.
Ocean Features.
Ocean Topography Main Features.
Ocean Floor and Underwater Discovery
Ocean Topography Main Features.
Presentation transcript:

Mapping the Ocean Floor

Essential Questions What are some of the features found on the ocean floor? What technology is used to map the ocean floor?

What are some of the features found on the ocean floor?

Continental Shelf A flat, wide margin is found around every continent The average width of a continental shelf is 70 kilometers Slopes at an angle of 0.1°, or 1.7 meters per kilometer

Continental Slope The continental slope is about 16 kilometers wide, on average, and descends to a depth of about 2.4 kilometers The slope of the ocean floor becomes much steeper, typically a 4° slope, or 70 meters per kilometer. is grooved by submarine canyons and gullies.

Continental Rise The slope moderates to a mere degree or two from horizontal which is called the continental rise

Submarine Canyon is a steep-sided valley on the sea floor of the continental slope cutting the continental slopes have been found at depths greater than 2 km below sea level.

Oceanic Trench Is where an oceanic crust plate begins to descend beneath another oceanic crust plate Oceanic trenches typically extend 3 to 4 km below the level of the surrounding oceanic floor. Trenches are generally parallel to a volcanic island arc, and about 200 km from a volcanic arc. The greatest ocean depth to be sounded is in the Challenger Deep of the Mariana Trench, at a depth of 10,911 m below sea level.

Abyssal Plain The abyssal plain, which is the deepest, most level part of the ocean, is found where the continental rise ends, at a depth of about 4 kilometers. The abyssal plain is dotted with thousands of small, extinct volcanoes called abyssal hills.

Mid-Ocean Ridge a long, undersea mountain chain that usually extends down the middle of the ocean The Mid-Atlantic Ridge, for example, snakes down the middle of the Atlantic most of the way from the North Pole to Antarctica.

Rift Valley Along the center of the mid-ocean ridge is the rift valley, a deep V-shaped notch. From this valley, new oceanic crust is constantly being extruded from Earth's mantle by processes not yet fully understood. In the case of the Mid-Atlantic rift valley, one sheet flows east and the other west, each moving at about half an inch per year. This causes sea floor spreading.

Guyot is an isolated underwater volcanic mountain, with a flat top over 200 meters (660 feet) below the surface of the sea. the diameters of these flat summits can exceed 10 km.

Seamount is a mountain rising from the ocean seafloor that does not reach to the water's surface, and thus is not an island. these are typically formed from extinct volcanoes, that rise abruptly and are usually found rising from a seafloor of 1,000–4,000 metres depth

Hydrothermal vent is a fissure in a planet's surface from which geothermally heated water issues are commonly found near volcanically active places, areas where tectonic plates are moving apart, ocean basins, and hotspots

Interesting facts Mauna Kea, Hawaii, rises 33,474 feet from its base on the ocean floor; only 13,680 feet are above sea level The ocean ridges form a great mountain range, almost 64,000 km long, that weaves its way through all the major oceans. It is the largest single feature on Earth Deepest point - 36,198 feet in the Mariana Trench in the western Pacific.

What technology is used to map the ocean floor?

Historically For hundreds of years, the only way to measure ocean depth was the sounding line, a weighted rope or wire that was lowered overboard until it touched the ocean floor. Not only was this method time-consuming, it was inaccurate; ship drift or water currents could drag the line off at an angle, which would exaggerate the depth reading. It was also difficult to tell when the sounding line had actually touched bottom

Present Day SONAR is a technique that uses sound propagation acronym for SOund Navigation And Ranging is a technique that uses sound propagation SONAR waves are sent from a ship and the time for the waves to return is measured the farther the distance the longer the time, the shorter the distance the smaller the time

Sea 3-D: Charting the Ocean Floor - KQED QUEST http://www.youtube.com/watch?v=1h4vaERMNbs 5:59

Oceanfloor Legacy http://video.google.com/videoplay?docid=862857452234843312# 28:

America's New Frontier http://video.google.com/videoplay?docid=-7837963317498620058# 27:30