Features of the Ocean Floor
MID OCEAN RIDGES CHAINS OF SUBMARINE VOLCANIC MOUNTAINS CREATE HYDROTHERMAL VENT ECOSYSTEMS
Mid-Ocean Ridges
Trenches DEEPEST PARTS OF THE OCEAN MARIANA’S TRENCH DEEPEST 1,580 MILES LONG 7-11 miles deep
Marianas Trench
SEA MOUNTS VOLCANO THAT DOES NOT RISE ABOVE SEA LEVEL
Hot Spot ACTIVE VOLCANIC ISLANDS REACH ABOVE SEA LEVEL EXAMPLE: HAWAII creation of new island
CONTINENTAL SHELF GENTLY SLOPING part of continent 8% OF OCEAN MOST BIOLOGICALLY RICH
CONTINENTAL SHELF
SUBMARINE CANYONS DEEP GROOVES CUT INTO CONTINENTAL SLOPES USED TO BE RIVER EDGES
CONTINENTAL SLOPE EDGE OF ACTUAL CONTINENT DEEP DROP OFF TO OCEAN BOTTOM
Upwelling will carry nutrients upward over corals, creating a nutrient rich environment
BIG DIFFERENCE FROM EAST TO WEST COAST
WEST COAST OF US
ACTIVE MARGINS
WEST COAST ACTIVE MARGINS Lots of Tectonic Activity & Steep Rocky Shorelines
PASSIVE MARGINS Flat Coastal Plains and Gradual Slopes
ABYSSAL PLAINS ABOUT 10,000 TO 13,000 FEET RELATIVELY FLAT area of deep ocean COVERED BY THICK LAYERS OF SEDIMENT
SONAR HOW WE MAP OCEAN FLOOR measuring the length of time a sound signal takes to return. Scientists "See" Ocean Floor via Sonar - YouTube