ROSCOE Vicki Ferrini: Data Representative/Team Leader Breea Govenar: Research Scientist/Data Representative Laishona Vitelli: K-12 Educator David Reeder:

Slides:



Advertisements
Similar presentations
Do Now Think about what you had for breakfast this morning. Think about what you had for breakfast this morning. Where did it come from? Where did it come.
Advertisements

FROM THE MIDOCEAN RIDGES TO THE BLACK SMOKERS. What is it a midocean ridge? A midocean ridge it’s due to the divergence between two plates (e.g. The African.
Plate Tectonics.
What Lies Beneath?. It has been said that the deep oceans are the last unexplored region of Earth. So, there are probably a lot of organisms living there.
“Ocean Floor Features” Titanic on Ocean Floor.
Investigating chemosynthesis
Geol104/BioES154 Deep-Sea Hydrothermal Vent Communities.
What is upwelling? a process in which currents bring deep, cold water to the surface of the ocean is a result of winds and the rotation of the Earth.
The Art of Subduction… The Marianas Trench By Michael Liston Oceanography 1 - Prof. Wiese.
Conditions differ away from shore.
Volcanoes Earth and Space Science. How many are there? About 60 of the ~550 known active volcanoes erupt each year There are many more volcanoes underwater.
Section 13-1 Review Page #324:1-8.
The Ocean Floor Chapter 14. What is Oceanography?  Oceanography  science that draws on the methods and knowledge of geology, chemistry, physics, and.
Section 4 Sea-Floor Spreading
Deep-Sea Hydrothermal Vent Communities
Abyssal Zone Zone on the Bottom of the Ocean. The ocean zone where you would find organisms such as worms, sea urchins, and chemosynthetic bacteria.
Volcanoes and Plate Tectonics
Life in Extreme Environments: A Study of the Prevalence of life in the Depths of an Underwater Rift Zone.
Planet EarthSection 2 Section 2: Earthquakes and Volcanoes Preview Key Ideas Bellringer What are Earthquakes? Measuring Earthquakes Volcanoes.
Notes 11 – Plate Tectonics Earth Science Mrs. Gordon Saturday, October 10, 2015Saturday, October 10, 2015Saturday, October 10, 2015Saturday, October 10,
Chapter 8 Volcanoes Section 1, Why Volcanoes Form
Miss Nelson SCIENCE ~ CHAPTER 6 VOLCANOES. Volcanoes and Plate Tectonics SECTION 1.
Ocean Topography Main Features.
Oceanography Test Review
Mid-Ocean Ridge Science Education for Teachers Ridge 2000 National Science Foundation Penn State University.
 The Importance of Hydrothermal Vents. Completely changed our view of life.  Chemosynthesis.  “Extreme’ life forms.  New ideas on the origin of life.
Zones of the Ocean. It’s all just one big ocean!
Hydrothermal Vents and Deep Sea Exploration
Open Ocean Notes 1. How is the open ocean different from the neritic zone?  Less sunlight—Surface Zone (200 m) is only layer the sun penetrates  The.
Volcanos: Chapter Volcano A volcano is a week spot in the crust where molten material, or magma, comes to the surface.
Geology of Earth Plate Tectonics.
Volcanoes
The Theory of Plate Tectonics. Plate Tectonics The inner structure of the Earth has different layers: is made of two layers The inner structure of the.
Hydrothermal Vents: Frontiers in Ocean Discovery.
Lesson 7.1: Volcanoes and Plate Boundaries. Volcano What is a volcano? How do volcanoes form? Where do volcanoes occur?
A. LEARNING ABOUT THE OCEAN: 1. Trading route 2. Scientific Discoveries 3. Exploring the ocean floor i. Sonar- floor mapping.
Hydrothermal Vents By Taylor, Jarrad and David What are Hydrothermal Vents A hypothermal vent is based on the ocean floor and is known as a hot spring,
Lessons 9-12 Notes Lesson 9: Volcanoes Lesson 11: Volcanoes Create New Landforms L12: Viscosity of Lava.
© 2014 Pearson Education, Inc. Chapter 15 Animals of the Benthic Environment Rocky and sandy shores Coral Reef Deep Sea.
Section 2: Earthquakes and Volcanoes Preview  Key Ideas Key Ideas  Bellringer Bellringer  What are Earthquakes? What are Earthquakes?  Measuring Earthquakes.
Volcanoes Erupting with fun!.
Plate Tectonics.
Deep-Sea Fiji Live Dive on- board RV Falkor
Volcano Notes Ms. Graham and Miss McGee 6th Grade Earth Science
Convection currents in the mantle result in the movement of lithospheric plates. The motion and interactions of the plates can create patterns in the.
Chapter 8 Volcanoes Section 1, Why Volcanoes Form
Handout 3 Standard 2-2 Plate Tectonics.
Volcanoes.
Ocean Topography Main Features.
Plate Tectonics.
Hydrothermal Vent Notes
Oceans.
Ocean Topography Main Features.
2.1 Introduction to Ecology and Ecosystems
9.4 – Testing Plate Tectonics
Ocean Topography Main Features.
Hydrothermal Vents
Mountains and Volcanoes
VOLCANOES CH. 3.1 Volcano (3:08) Volcano.
Life in Extreme Environments
The Ocean Floor Notes December 2, 2018.
Chapter 3: Volcanoes.
Hydrothermal Vents.
Ocean Topography Main Features.
Geologic disasters.
Divergent Plate Boundaries
17.2 Seafloor Spreading.
Food chains in the ocean are long and complex
Deep Sea Vents In 1977, scientists made a stunning discovery on the bottom of the Pacific Ocean that forever changed our understanding of planet Earth.
Sea Floor Spreading Notes
Presentation transcript:

ROSCOE Vicki Ferrini: Data Representative/Team Leader Breea Govenar: Research Scientist/Data Representative Laishona Vitelli: K-12 Educator David Reeder: Curriculum Developer Karin Block: Data Representative Research at Oceanic Spreading Centers: Outreach in Education

Life in extreme environments: exploring underwater volcanoes at oceanic spreading centers The Big Ideas: No one expected to find abundant life in the deep ocean bottom thriving in hot fluids along plate boundaries, but the surprise discovery in 1979 of a rich biologic ecosystem in an environment of high pressure, toxic chemicals, frequent eruptions, and complete darkness completely changed our understanding of how life can exist. Research in the 30 years since the first discovery has helped us better understand how heat from the earth's interior is released through underwater hydrothermal vents, and how the complex interaction of geology and chemistry create an environment where life can be supported through chemosynthesis. Students will recreate the process of discovery and understanding of hydrothermal vents using data and tools available through GeoMapApp, including GMRT and ABE bathymetry data, MediaBank images, and PetdB chemical data.

Outline of major parts of the activity Part 1: Explore the Galapagos spreading center using GeoMapApp – introduce basic functions of the tool using the location of the first discovery and underwater images from the site. Part 2: Create a topographic profile across the East Pacific Rise – explore relationships between locations of hydrothermal vents and the topography of a spreading center using high-resolution data from the Ridge2000 research project at EPR. Part 3: Investigate the life forms that populate the East Pacific Rise – view images taken at the site, make observations, and explore relationships between location, species concentration and diversity, vent structures, and water temperature. Part 4: Dig deeper into the chemistry that supports life on the East Pacific Rise – use chemistry data from rock samples to identify elements that are used by bacteria for chemosynthesis.