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Chapter 15
Oceanography
Deals with the study of
world oceans using the
methods and knowledge of
biology, chemistry, physics,
and geology.
The four major oceans are
Atlantic, Pacific, Indian,
and Arctic. Pacific ocean is
considered as the largest
ocean, and has the greatest
average depth.
Characteristics of ocean
water:
1. Temperature. Is not
uniform, surface layer has
warm temperature, next
layer is thermocline which
has rapid temperature
change. And the last layer
is the deep water where
temperature decreases
slowly as depth increases.
2. Salinity. Refers to the
proportion of dissolved
salts to pure water and is
expressed in parts per
thousand (‰). Average
salinity in the open ocean
ranges from 35‰ to 37‰.
Principal elements of
ocean salinity; Chlorine
and sodium. Primary
sources of ocean salinity;
chemical weathering of
rocks and outgassing.
Salinity changes with
increasing depth, surface
zone has the higher
salinity.
Halocline, is the layer
that is characterized by
rapid decreasing salinity.
Ocean floor topography
Echo sounders and
Multibeam sonars are
devices that can
determine the depth of
the ocean through sonic
signals that bounce off the
ocean floor. Mapping can
also be done by using
satellite.
1. Continental margin. Is
the zone of the ocean
floor that separates the
thin oceanic crust from
the thick continental
crust.
2. Passive continental
margin. Is characterized
by a firm connection
between continental and
oceanic crust. There is a
little volcanic activity
occurring in this
boundary. Contains
continental shelf,
continental slope, and
continental rise.
3. Submarine canyons. Are
deep, steep-sided valleys
that originate on the
continental slope.
4. Active continental margin.
Is the subduction of an
oceanic lithospheric plate
beneath a continental plate.
Has a narrow continental
shelf which grades into a
deep-ocean trench. Located
around Pacific Ocean.
Accretionary wedge is a
body of sediments that has
been scraped off the surface
of oceanic lithosphere as it
moves downward beneath a
continent.
5. Mid oceanic ridge. Is a
submarine mountain
chain that extends
through the entire ocean
basin. It is the site for
seafloor spreading.
6. Ocean basin. Lies
between the continental
margin and the mid-
oceanic ridge system.
Features found on the
ocean basin floor; deep-
ocean trenches, abyssal
plains and seamounts.
Ocean floor sediments
1. Terrigenous sediment.
Consists mineral grains
that were weathered
from continental rocks
and transported to the
ocean.
2. Biogenous sediment.
Consists of shells and
skeletons of marine
animals and plants.
3. Hydrogenous sediment.
Includes minerals from
crystallized seawater.
Reefs
Three criteria for organizing
habitats of marine life:
Availability of light,
Distance from the shore,
and Water depth.
Reefs are wave-resistant
structures and composed of
animal skeletons
particularly corals.
3 types of reef:
1. Atoll. Is formed from
corals that grow on the
flanks of sinking
volcanic islands.
2. Fringing reef. Lie
close to the shore of an
island or continent.
3. Barrier reef. Is similar
to fringing reef, except
that they are separated
from the mainland by
lagoon.
Importance of ocean
• in removing carbon from
the atmosphere and
providing oxygen.
• Has capacity to collect,
drive and mix water,
heat, and carbon dioxide.
• Economy of communities
• Source of biomedical
organisms
Geological resources in
the ocean floor
 Sources of Foods (fish &
shellfish)
 Sources of minerals
(crude oil, salt, sand,
gravel, manganese,
copper, nickel, iron,
cobalt, diamond, gold,
silver through mining.
However, mining can have
negative effect.

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Unit iii chapter 15 (oceanography)

  • 2. Oceanography Deals with the study of world oceans using the methods and knowledge of biology, chemistry, physics, and geology. The four major oceans are Atlantic, Pacific, Indian, and Arctic. Pacific ocean is considered as the largest ocean, and has the greatest average depth.
  • 3.
  • 4. Characteristics of ocean water: 1. Temperature. Is not uniform, surface layer has warm temperature, next layer is thermocline which has rapid temperature change. And the last layer is the deep water where temperature decreases slowly as depth increases.
  • 5. 2. Salinity. Refers to the proportion of dissolved salts to pure water and is expressed in parts per thousand (‰). Average salinity in the open ocean ranges from 35‰ to 37‰. Principal elements of ocean salinity; Chlorine and sodium. Primary sources of ocean salinity; chemical weathering of rocks and outgassing. Salinity changes with increasing depth, surface zone has the higher salinity.
  • 6. Halocline, is the layer that is characterized by rapid decreasing salinity. Ocean floor topography Echo sounders and Multibeam sonars are devices that can determine the depth of the ocean through sonic signals that bounce off the ocean floor. Mapping can also be done by using satellite.
  • 7. 1. Continental margin. Is the zone of the ocean floor that separates the thin oceanic crust from the thick continental crust. 2. Passive continental margin. Is characterized by a firm connection between continental and oceanic crust. There is a little volcanic activity occurring in this boundary. Contains continental shelf, continental slope, and continental rise.
  • 8. 3. Submarine canyons. Are deep, steep-sided valleys that originate on the continental slope. 4. Active continental margin. Is the subduction of an oceanic lithospheric plate beneath a continental plate. Has a narrow continental shelf which grades into a deep-ocean trench. Located around Pacific Ocean. Accretionary wedge is a body of sediments that has been scraped off the surface of oceanic lithosphere as it moves downward beneath a continent.
  • 9. 5. Mid oceanic ridge. Is a submarine mountain chain that extends through the entire ocean basin. It is the site for seafloor spreading. 6. Ocean basin. Lies between the continental margin and the mid- oceanic ridge system. Features found on the ocean basin floor; deep- ocean trenches, abyssal plains and seamounts.
  • 10. Ocean floor sediments 1. Terrigenous sediment. Consists mineral grains that were weathered from continental rocks and transported to the ocean. 2. Biogenous sediment. Consists of shells and skeletons of marine animals and plants.
  • 11. 3. Hydrogenous sediment. Includes minerals from crystallized seawater. Reefs Three criteria for organizing habitats of marine life: Availability of light, Distance from the shore, and Water depth. Reefs are wave-resistant structures and composed of animal skeletons particularly corals.
  • 12. 3 types of reef: 1. Atoll. Is formed from corals that grow on the flanks of sinking volcanic islands. 2. Fringing reef. Lie close to the shore of an island or continent. 3. Barrier reef. Is similar to fringing reef, except that they are separated from the mainland by lagoon.
  • 13. Importance of ocean • in removing carbon from the atmosphere and providing oxygen. • Has capacity to collect, drive and mix water, heat, and carbon dioxide. • Economy of communities • Source of biomedical organisms
  • 14. Geological resources in the ocean floor  Sources of Foods (fish & shellfish)  Sources of minerals (crude oil, salt, sand, gravel, manganese, copper, nickel, iron, cobalt, diamond, gold, silver through mining. However, mining can have negative effect.