Oceanography Exam I Study Guide – Chapters 1-4
I. Introduction to Oceanography – Chapter 1
A. The Earth is a Dynamic
Ever-changing System
1. Know the Earth's major subsystems
2. Be able to draw/ label the Earth's
Cross-section
B. Be able to define Oceanography.
C. Oceanography and the Scientific
Theory
1) Know the Scientific Theory approach to nature: the
basic foundation of all sciences.
· The basic
steps
· Hypotheses
and Theories
· Observations,
Data and Evidence
· Methods of
Testing
· Interpreting
results
2) Understand
the basics of how the approach works.
3) Find/create examples of the ST in the real
world.
D. Be able to describe and explain the commonly-accepted
explanations for the Origin of Galaxies, the Solar System,
Earth, Ocean and Moon, and Life.
1) The Big-Bang hypothesis
2) The Solar nebula "cold" accretion
hypothesis
3) Moltenization
and differentiation periods of early Earth.
4) The origin and evolution of the Earth-Moon
system.
5) The origin and evolution of Earth's early
atmosphere,
oceans, and
continental masses.
6) The
origins of Life on Earth.
7) The
“oxygen revolution”
E. Know what makes the Earth such a
dynamic planet!
1) Generation of INTERNAL HEAT from two key
sources
· Gravitational
heat of accretion (core)
· Radioactive
isotopes barbeque (mantle)
2) The presence of LOTS OF WATER on the
surface.
3) Amazing
set of balanced physical, chemical, and energy
variables that allow water to exist in all three states.
5) SOLAR input.
6) Know and be able to describe the general
physical and
chemical features of both, the Earth's interior and
surface.
ü The Earth's subsystems
ü The global topographic and
geographic surface
patterns, e.g. layout of continental masses,
ocean basins, mountain ranges, trenches,
island arcs, mid-ocean rift valleys, etc.
F. Know what stimulated the voyages of the
early seafaring
civilizations – compare and contrast the
intent and
purpose for voyaging of the:
1) Polynesians and Vikings
2) Phoenicians and Greeks
3) Chinese and Europeans
G. List and describe the essential types of information
found in a marine chart (map)
1) Longitude and latitude
2) Scale
3) Coastlines
4) Bathymetry (water depths and
contours)
H. Describe the important
oceanographic contributions
of the most influential people and organizations throughout the
history oceanography
1) People like: Columbus, Megellan, Henry the
Navigator, Darwin, C. Maury, Captain
Cook, and
John Harrison
2) Organizations within governments, military, and private/
public research institutions
I. List and Describe key technologic
breakthroughs
that helped
advance oceanographic research
1) Seaworthy ships
2) Compass
3) Sextant
4) Chronometer
5) Power winches
6) Electronic sensing
devices (ex: for salinity, currents)
7) Sonar
8) Satellite
9) GPS
10) Computers and data software
II. Plate Tectonics and the Seafloor – Chapter 2
A. Know The Basics of
the Earth's Rock Cycle -
1) What is it? The endless cycle of building-up and
wearing down of the Earth's crust.
§ Building
up by magmatism and crustal
uplift.
§ Worn down
by weathering and erosion.
§ Destroyed/recycled
by subduction.
2) A complex physical and chemical interplay of
processes between five major
material reservoirs:
magma, igneous rocks, sediments,
sedimentary
rocks, and metamorphic rocks.
3) Series of related geologic processes occur between
two material
reservoirs:
4) Three Major Rock Types
ü Each group
defines a variety of rock types that have a common origin.
1) Igneous Rocks - Formed by the cooling and
crystallization of
either, magma deep beneath
the Earth's
surface, or lava extruded on the
surface, or consolidation of volcanic ejecta.
2) Sedimentary Rocks - Formed from the deposited
layers
of clastic and/or chemical sediment via
compaction and cementation.
3)
Metamorphic Rocks - Formed by metamorphic
reactions
of pre-existing solid rock via a unique
combination of extreme heat,
pressure, fluids, and
deviatoric stresses.
5. Major rock-forming Processes
a. Heating (any rock) Þ Partial
Melting Þ Magma
b. Transport (magma) Þ Cooling Þ
Crystallization Þ Igneous
Rock
c. Weathering (any rock) Þ Erosion Þ Sediment
d. Deposition (sediment) Þ Compaction Þ Cementation Þ Sedimentary
Rock
e. Heating +/- Pressure +/- Fluids +/-
Stress Þ Metamorphic Rock
6. Be Able to Draw A Simple Rock Cycle Diagram
B. Know The Basics of Earth's Hydrologic Cycle
1) What is it?
· The endless
cycling of water via evaporation, precipitation, and runoff on Earth's surface.
· Major player in controlling Earth's climate
· Powers
weathering and erosion.
· Plays a
key role in mid-ocean hydrothermal systems
· Plays a
key role in subduction zone.
2.
Be Able to Draw/Label A
Simple Hydrologic Cycle Diagram
C. Wegener's Theory of Continental Drift (TCD)
1) Be able
to explain the overall basic concept of CD
2) Know the terms
Pangaea, Gonwanaland, and Luarasia
3) List the major
types of evidence supporting TCD
4) Know the major
obstacle that discredited the TCD
5) Know the key
scientists that developed/supported TCD
D. Know All the Basics of the
Plate Tectonic Theory --
1) Stiff, outermost
shell of solid Earth consisting of
the crust and uppermost mantle called the lithosphere
Broken up
into 6 major plates & 12 minor plates –
Move over
the hot, plastic athenosphere
mantle.
2) Each tectonic plate moves independently:
two adjacent
plates
can interact in one of three ways:
Diverge
Converge
Slide past
one another
3) Three types of plate boundaries and
associated process
· Divergent
= rifting/ seafloor spreading; tensional
· Convergent
= subduction/ collision; compression
· Transform
= strike-slip faulting; shearing
4) Spreading centers and Continental rifts form at divergent
boundaries, where two plates are moving away from
each
other, forming brand-new oceanic crust.
5) Subduction zones and magmatic arcs form at convergent
boundaries,
where an oceanic plate dives beneath
either
a continental or oceanic plate into the mantle.
6) Continental collision zones also form at convergent
boundaries where two continental masses are
meeting head-on.
7) Great, transform strike-slip fault systems are created
where two plates slide sideways, past each other.
8) Three proposed driving mechanisms of plate tectonics
a. mantle convection
b. ridge push
c. slab pull
9) The plate interactions, over time, cause a
number of
spectacular phenomena, including magmatic arcs,
mountain chains, terrane accretion and ocean basin collapses and
openings.
· Describe
the terrane accretion process
· Describe
the Wilson Cycle
10) The plate tectonic theory unifies the observation and hypotheses
which attempt
to explain most geologic phenomena.
11) The Earth's rock cycle is
driven in large part by
E. Seafloor Spreading (SS)
1) Be able to explain the basic
concept of seafloor spreading
2) Know the key terms
associated with seafloor spreading
3) List the major types of
evidence/discovers behind SS
4) Know the key scientist
that proposed
F. Subduction
1) Be able to explain the basic
concept of subduction
2) Know the key terms
related to subduction
3) List the major
evidence/discovers for subduction
4) Know the key scientist
that proposed
G. Important Points concerning Theory of Plate Tectonics - Know that:
1)
Plate Tectonics is a unifying theory because it is able
to explain many geologic phenomena.
2) The so-called
"Wilson Cycle" represents a plate tectonic
cycle of plate motions where an
ocean basin is born,
grows, then shrinks, and finally
collapses.
3) There are 500
million-year Supercontinent
Cycles of plate
motions and
interactions that begins with the break-up of
an old supercontinent and ends with the
formation of a new
supercontinent.
4) Plate tectonics is the cause
of Earth's mountain building,
magmatism, and never-ending resurfacing of the planet.
5) The Earth's rock cycle is
fueled by plate tectonics.
F. Be Able to Identify All Major Plate
Tectonic Boundaries
On a Map or Globe
1) Circum-Pacific basin and adjoining continents
2) North and
3)
G. Be Able to Identify Elements of Plate
Tectonics in a
Geographic Illustration (see online practice
exam)
)1 Match plate
processes (ex. seafloor spreading)
with
associated geographic features (ex. mid- ocean ridges)
H. Understand and be able to explain the concept of isostacy.
III. Marine Provinces -- Chapter 3
A. Know the Geographic Significance of Seafloors
1) Oceans and seas cover over 70% of Earth's
surface
2) Earth's seafloors constitute a global-scale
topographic
region of low-lying relief that
contrasts to the high-
standing relief of the continents
3) Seafloors represent the most vast (by far)
depositional
environment on Earth
· Site of
massive sedimentation and region of sedimentary
rock production
4) The evidence used to establish and support
the Theory
of Plate Tectonics was established
from the scientific
study of seafloors and its sediments
B. Know Components and Nature of Continental Margins
· Shelf –
flat portion nearest shoreline
· Slope –
steep outer edge of shelf
· Rise –
base of slope where continebt
and oceanic crust meet
1) Shelf-slope
break, Submarine canyons, Turbidity currents
2) Continental margin seafloors consist mainly of
Granitic crust = outer edges of continents
Covered primarily by Terriginous
sediments
3) Water depths are shallow; up to 200 meters
on shelves
4) Explain
difference between Passive versus Active
continental margins
C. Know Components and Nature of Deep Ocean Basins
§ Abyssal
plains and hills
§ Oceanic
trenches
§ Oceanic
ridge systems and fracture zones
§ Hydrothermal
vents
§ Oceanic
islands, atolls, guyouts,
and seamounts
1) Ocean basins have rugged, variable topography
2) Oceanic basin seafloors consist of
· Basaltic
crust = ophiolite package
· Pelagic
clays and oozes (sediments)
·
Pelagic clays derived from continents
·
Oozes consist mainly of skeletons of microscopic marine organisms
3) Water depth of deep ocean
average 4,000 meters
IV. Seafloor Sediments - Chapter 4
D. List and Describe the Types of Seafloor Sediments
1) Four types of marine-based
sediment - See Table 5.2
· Lithogeneous
· Biogenous
· Hydrogeneous
· Cosmogenous
2) Pelagic clays derived from primarily three land-based
sources
· Rivers
· Volcanic
eruption (ash falls)
· Windblown
material
· Consist
mainly of quartz and clay
3) Describe the two main types of Biogenous
Oozes
· Calcium
carbonate oozes
· Siliceous
oozes
· Constitute
fecal pellets from larger animals
· Fine sand-
to silt-size particles
4) Define the sources of calcium carbonate oozes
· Foraminifera
· Cocoliths
· Found on
bottoms less than 4,500 meters deep (CCCD)
5) Define the sources of siliceous oozes
· Tropical
Radiolarians
· Polar
Diatoms
6) Define types of hydrogenous sediments
· Manganese
nodules
· Phosphate
nodules
· Massive
metal sulfide deposits
· Evaporites
E. Describe and Explain the Distribution of Seafloor
Sediments -
1) Study Table 5.3 very carefully
2) Study
Figure 5.13 very carefully
3) Distribution of each sediment type
controlled by several
environmental factors:
· Proximity
to sediment source
· Rate of
sedimentation (each specific sediment type)
· Chemical
stability at site of deposition
4) Unique distribution pattern for each sediment type
Study Distribution Map shown in
Figure 5.13
· Lithogeneous -
· Biogenous
· Hydrogeneous
· Cosmogenous
F. Define the Rates of Seafloor Sedimentation
1) Deep ocean sedimentation rates
are very low
2) Each type of deep seafloor sediment has
specific rate
· Lithogeneous - 2 millimeters per
1000 years
· Biogenous - 1 to 6 centimeters per 1000 years
· Hydrogeneous - 1 to 10
millimeters per 1 million years
· Cosmogenous - Negligible
G. List and Describe Methods of Seafloor Sediment
Sampling
· Piston Coring samplers
· Drag bucket
and Clamshell samplers
H.
List and Describe Types of Seafloor Mineral Resources
1) Continental Margins
§ Oil and
gas (hydrocarbons)
§ Sand and
Gravel
2)
· Manganese
nodules
· Massive metal-sulphide deposits
· NO gold
and silver
V. Vocabulary Lists - Chapters 1-4
A. Study the Terms and Concepts Lists Found at the End
of Each Chapter
1) Attempt to remember them
2) Be ready to define many of these (at least the
ones
that I have included in this study guide)