11_Ocean Floor
Ocean Floor Overview
Presenter: Dr. Jackie Miranda
Date: February 24, 2025
Agenda
60-Second News Update: Muhammad and Autumn
Key Topics:
Ocean Basins
Continental Margins & Ocean Ridges
Seafloor Mapping
Ocean Sediments
Seafloor Lab
News Updates
Muhammad and Autumn: Updates related to ocean research and events.
Upcoming Events
Tampa Bay Youth Ocean Summit
Date: March 1
Time: 9 AM – 5 PM
Themes:
Wildlife over Waste
Save Florida’s Whales
Protect Coral in the Florida Keys National Marine Sanctuary
Climate Change and Our Ocean
Denis Phillips Guest Lecture
Date: March 26
Time: 7 PM – 8:45 PM
Location: Tarpon Springs Campus, Chris Sprowls Workforce Innovation Hub
Focus: Community service, social media, and weather
Quiz Questions Review
Quiz Question 1: Type of stream in the image?
Options: A. Braided stream, B. Low sinuosity stream, C. Steep terrain stream, D. Meandering stream
Quiz Question 2: What is the top horizon of soil called?
Answer options: A. True, B. False
Importance of Oceans
Climate: Contributes to global climate patterns
Resources: Energy extraction and transportation of goods
Recreational Use: Provides areas for recreation
Oceans Statistics
Earth's Surface: 71% is covered by oceans and marginal seas
Ocean Coverage:
Northern Hemisphere: 61% ocean
Southern Hemisphere: 80% ocean
Ocean Basins
Major Ocean Basins:
Pacific Ocean: Largest, deepest (average depth: 4,282 m)
Atlantic Ocean: Second largest, less depth (average depth: 3,926 m)
Arctic Ocean: Shallowest (average depth: 1,205 m)
Indian Ocean: Similar depth to Atlantic (average depth: 3,741 m)
Southern Ocean: Equivalent depth to Atlantic and Indian (average depth: 3,270 m)
Deep Ocean Exploration
Exploration Status: Only 5% of the world’s oceans have been explored; 26.1% of the ocean floor mapped as of June 2024.
Continental Margins and Ocean Ridges
Types of Margins:
Active Margins: Associated with tectonic plate boundaries, experience volcanism and earthquakes.
Passive Margins: Not associated with plate boundaries, experience little volcanism.
Continental Shelf: Shallow, flooded edge of the continent, often containing oil and mineral deposits.
Continental Slope: Steeper area leading from the shelf to deeper regions.
Continental Rise: Where continental slope becomes gradual and accumulates sediment.
Submarine Canyons and Turbidity Currents
Submarine Canyons: Deep, steep valleys on continental slopes, often formed by turbidity currents.
Turbidity Currents: Dense, sediment-laden water flows downslope, depositing turbidite layers characterized by graded bedding.
Active Continental Margins
Found mainly around the Pacific, featuring deep ocean trenches and significant volcanic activity.
Deep-Ocean Trenches
Long, narrow, and the deepest parts of oceans located primarily in the Pacific. Associated with volcanic activity and plate tectonics.
Abyssal Plain
Deep ocean floor covering depths from 4,500 to 6,000 m, characterized by thick sediment accumulations.
Seamounts and Guyots
Undersea volcanic peaks that can emerge as islands or erode to become flat-topped structures (guyots).
Oceanic Ridge System
Mid-Ocean Ridge: Longest topographic feature on Earth, characterized by extensive faulting and volcanic structures, spanning approximately 70,000 km.
Hydrothermal Vents
Critical for supporting unique ecosystems; formed near tectonic plate boundaries with geothermally heated water.
Review Questions
World's Oceans Coverage: About 71% of Earth.
Southern Hemisphere Ocean Coverage: True – more ocean coverage than Northern Hemisphere.
Seafloor Mapping Technology
Tools:
Echo sounders for depth measurement.
Sidescan sonar and multibeam sonar for detailed mapping.
Satellite altimeter for measuring the ocean surface shape from space.
Seafloor Sediments
Main types of sediments include:
Terrigenous: Weathered material from land.
Biogenous: Derived from marine organisms.
Hydrogenous: Minerals crystallized directly from seawater.
Climate Impact of Sediments
Provide a record of life and climatic conditions, essential for understanding Earth's climate history.
What Did You Learn Today?
Reflect on three key takeaways and the most confusing aspects of today’s class.