CHAPTER 23: MARINE GEOLOGY. Earth’s Water Earth's oceans are unique in the Solar System and are the largest single feature on the planet. 70% of the Earth’s.

Slides:



Advertisements
Similar presentations
Chapter 14 The Ocean Floor.
Advertisements

Marine Sedimentation. Streams Rivers Glaciers Landslide (Gravity)
Introduction to Oceanography
Tim Horner CSUS Geology Department The Sea Floor Physical Geology, Chapter 18.
Chapter 23.1 Studying the Ocean Floor
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.
Notes – Chapter 12 Ocean Waters and the Ocean Floor
Study Guide available! Web site (dusk.geo.orst.edu/oceans) Go to the syllabus page and click on the Study Guide for Test#1.
OCEANIC TOPOGRAPHY By Greg Schwab May 7, Competency 39 The teacher understands structure and function of the hydrosphere The teacher understands.
Today: Chapter 17, part I Earth beneath the Ocean  Techniques of mapping the ocean floor Which parts make up a continental margin, and what is the difference.
“Ocean Floor Features” Titanic on Ocean Floor.
Earth Science, 10e Edward J. Tarbuck & Frederick K. Lutgens.
Earth Science 14.2 Features of the Ocean Floor
Features of the Ocean Floor
Earth Science Spring The Water Planet Global ocean covers 97% of the earth’s surface. Global ocean divided into 3 major oceans: Atlantic Pacific.
Warm Up 2/6/09 What technology do scientists use to measure ocean depth? a. sonar c. rope b. submersible d. laser Differences in ocean-surface height.
SEDIMENTS Text Book – Chapter 5 Why do we care about oceanic sediments? -Continents are sites of erosion; -Oceans are sites of depositions; -Therefore.
Sediments Sediment particles that accumulate in a loose, unconsolidated form. Originate from weathering and erosion of rocks activity of living organisms.
The Ocean Floor Chapter 14 pg 393.
Chapter 14.2 Ocean Floor Features.
Ocean Waters and the Ocean Floor. The Vast World Oceans 81% of the Southern Hemisphere is covered by oceans 61% of the Northern Hemisphere is covered.
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
Chapter 4 Marine Sedimentation.
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
Oceanography Test Review
Chapter 14 The Ocean Floor Who is Stan Hatfield and Ken Pinzke.
Chapter 9 Oceans: The Last Frontier. The Vast World Ocean  Earth is often referred to as the blue planet  Seventy-one percent of Earth’s surface is.
14.2 science OCEAN FLOOR The ocean floor regions are the continental margins, the ocean basin floor, and the mid-ocean ridge. Scientists have discovered.
CH 14.1 The Ocean Floor Oceanography – the study…
11.1 Ocean Basins The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are the Pacific the Atlantic.
The Sea Floor. Origin of the Ocean Water vapor released during degassing of early earth –volcanism Salt from chemical weathering.
The Ocean Basins Section 2 Section 2: Features of the Ocean Floor Preview Objectives Features of the Ocean Floor Continental Margins Deep-Ocean Basins.
The Ocean Basins Section 2 Preview  Key Ideas Key Ideas  Features of the Ocean Floor Features of the Ocean Floor  Continental Margins Continental Margins.
19 Chapter 19 Oceanography. The Blue Planet 19.1 The Seafloor  Nearly 71 percent of Earth’s surface is covered by the global ocean.  Oceanography is.
Oceanography 101, Richard StricklandLecture 5© 2006 University of Washington 1 Sediments of the Sea Floor Figure 3.20.
Chapter 14 The Ocean Floor Who is Stan Hatfield and Ken Pinzke.
Geological Oceanography Ocean Topography The scientific study of the origin, history, and structure of the earth.
The Ocean Floor and Its Sediments Chapter 16. Ocean Floor Features Divided into 2 main regions Divided into 2 main regions –Continental margins –Ocean.
INTRODUCTION What is at the Sea floor?
Sediments Chapter 5.
© 2012 Pearson Education, Inc. Earth Science, 13e Tarbuck & Lutgens.
Chapter 4 Marine Sedimentation ©2003 Jones and Bartlett Publishers.
Oceans.  Pacific  largest  Atlantic  Indian  Arctic  smallest Name the Oceans.
Chapter 19 Study Notes: The Ocean Basins. Chapter 19 Section 1 The Water Planet.
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
Marine Sedimentation.
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.
Spring Hydrology 2016 Mrs. Kummer. The Water Planet  Nearly ¾ of Earth’s surface is underwater  97% of all water on Earth is in the “global ocean” 
Chapter 23 The Ocean Basins.
Oceanography notes (part 1):
Measuring bathymetry Ocean depths and topography of ocean floor
Section 2: Features of the Ocean Floor
CH 14.1 The Ocean Floor Oceanography – the study…
Ocean Topography.
Warm-up What is one topic from this unit that you understand?
14.2 – Ocean Floor Features.
The Ocean Floor.
The surface of the ocean floor is as varied as the land.
Bathymetry of the Ocean Floor
The Ocean Floor Notes December 2, 2018.
Physical Oceanography
Deep-Sea Sediments.
Chapter 16: The Marine Environment
Ocean Floor.
Physical Oceanography
The Marine Environment
The Marine Environment
Presentation transcript:

CHAPTER 23: MARINE GEOLOGY

Earth’s Water Earth's oceans are unique in the Solar System and are the largest single feature on the planet. 70% of the Earth’s surface is ocean water.

Earth’s Water With an average depth of 3,800 metres, the oceans contain ~97% of Earth's water.

Marine Geology is the study of geologic processes within ocean basins The five recognized oceans and the three largest seas

Oceans

Salinity Chemical weathering and hydrothermal processes dissolve ions and compounds. >90% of all dissolved ions are chloride and sodium. Average global salinity ~35 parts per 1,000 Can you explain the distributions of some of the areas of very high and very low salinity? Why are the oceans salty?

Oceanic Gyres There are numerous surface-ocean currents, and in several areas they have circular patterns known as oceanic gyres Why are ocean gyres clockwise in the northern hemisphere and counter-clockwise in the southern hemisphere?

Currents at Depth In addition to the surface currents ocean waters (and the heat energy they contain) are also redistributed by currents at depth

Ekamn Transport As the Coriolis Effect deflects a current, water in lower layers deflects more slowly than surface water. The resulting movement of water is known as Ekman Transport

Shelf, Slope and Rise The continental margin consists of the shelf, slope, and rise.

Continental Shelf A continental shelf is the submerged border of a continent What type of crust (oceanic or continental) would you expect to find beneath a continental shelf?

Continental Shelves Continental shelves are also rich in marine life Canada’s Atlantic shelf is rich with oil and gas deposits, which are exploited by almost 330 active wells (red dots). By comparison, the U.S. Gulf of Mexico has almost 4,000 active wells.

Margins Passive Margins lack active plate boundaries Active Margins, located at plate boundaries, may have Accreted Terrane. Canada has 3 ocean margins. Which are active and which are passive?

Submarine Canyons Submarine Canyons are valleys that cut into the shelf and slope.

Turbidity Currents Turbidity Currents result from the collapse of an unconsolidated sedimentary deposit on the slope or shelf edge

Continental Margin Most ocean sediment is deposited on the continental margin U.S. Continental Shelf, Gulf of Mexico

Neritic and Hemopelagic Sediments Neritic Sediments (between the shoreline and the shelf edge) can be of several different types: – Detrital – Biogenic – Eolian – Residual – Authigenic – Relict Hemipelagic Sediments - draped on the upper and middle slopes - grade from terrigenous muds into biogenic sediments In this context what is the difference between “detrital” and “authigenic”?

Detrital Sediment from a stream Wind blown (eolian) detrital sediment

Deltas Some deltas contain so much detrital sediment that the topography of the continental shelf is hidden by the submarine fan. Why does the Ganges Brahmaputra delta and submarine fan have so much sediment?

Pelagic Sediment Pelagic sediment covers the abyssal plains Why do the Atlantic ocean margins have so much more sediment than the Pacific ones?

Calcareous Ooze Calcite is stable in shallow ocean water but below the Carbonate Compensation Depth (CCD) (which is typically around 4000 m) CaCO3 dissolves. foraminifera coccolithophores

Diatoms and Radiolaria Diatoms and radiolaria make their tests out of silica, and they accumulate on the sea floor to form siliceous mud (as opposed to calcareous mud) radiolaria diatoms

Pelagic Sediment Pelagic sediment distribution reflects water depth, biological productivity and terrigenous inputs

Mid-Ocean Ridge The mid-ocean ridge is the site of seafloor spreading. The water depth near to the ridge is typically about half of what it is elsewhere.

Oceanic crust is formed at mid-ocean ridges

Marine Stratigraphy across the Mid-Atlantic Ridge Why does calcareous sediment accumulate on the mid- Atlantic ridge, but not on the sea-floor away from the ridge?

Marine Stratigraphy along a N - S section through the Pacific Ocean NorthSouth

Abyssal hills are seamounts extending above the sediments of the seafloor

Why does the source and composition of sediment change between the coast, shelf, rise, abyssal plain, and oceanic ridge?

Oceanic trenches Oceanic trenches occur at subduction zones Why are some of the trenches the deepest parts of the oceans?

The major world trenches

Human impacts to reefs include pollution, over fishing, and climate change What are two climate-related impacts to tropical reefs?

Human impacts to the oceans are global in extent

COPYRIGHT Copyright © 2014 John Wiley & Sons Canada, Ltd. All rights reserved. Reproduction or translation of this work beyond that permitted by Access Copyright (The Canadian Copyright Licensing Agency) is unlawful. Requests for further information should be addressed to the Permissions Department, John Wiley & Sons Canada, Ltd. The purchaser may make back-up copies for his or her own use only and not for distribution or resale. The author and the publisher assume no responsibility for errors, omissions, or damages caused by the use of these programs or from the use of the information contained herein.