Presentation is loading. Please wait.

Presentation is loading. Please wait.

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.

Similar presentations


Presentation on theme: "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."— Presentation transcript:

1 CHAPTER 23: MARINE GEOLOGY

2 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.

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

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

5 Oceans

6 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?

7 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?

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

9 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

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

11 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?

12 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.

13 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?

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

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

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

17 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”?

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

19 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?

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

21 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

22 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

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

24 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.

25 Oceanic crust is formed at mid-ocean ridges

26 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?

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

28 Abyssal hills are seamounts extending above the sediments of the seafloor

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

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

31 The major world trenches

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

33 Human impacts to the oceans are global in extent

34 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.


Download ppt "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."

Similar presentations


Ads by Google