The ship Darwin was the naturalist on during his famous voyage
The Wilkes Expedition (U.S. Exploring Expedition) contributed to expanding the geographic and scientific knowledge of the Pacific region and played a crucial role in establishing the Smithsonian Institution
The Challenger Expedition laid the foundation of modern oceanography, having made groundbreaking discoveries regarding ocean depths, marine life, and ocean temperatures
Proposed explanation made on the basis of limited evidence as a starting point for further investigation
Experiment
A procedure undertaken to make a discovery, test a hypothesis, or demonstrate a known fact
You can't prove a hypothesis because scientific testing can only reject hypotheses or support them with evidence, not prove them definitively
Experimental group
The group in an experiment that receives the treatment or the variable being tested
Control group
A group in an experiment that does not receive the treatment and is used as a baseline to compare results against
Variable
Any factor, trait, or condition that can exist in differing amounts or types and can influence the outcomes of an experiment
Theory
A well-substantiated explanation of some aspect of the natural world that is acquired through the scientific method and repeatedly tested and confirmed through observation and experimentation
The Pacific ocean is the largest and deepest ocean
71% of the earth's surface is ocean
The southern hemisphere is more dominated by ocean
Layers of the Earth
Crust: The outermost solid shell of the planet, which is brittle and thin compared to other layers
Mantle: Below the crust, composed of silicate rocks that are denser than crustal materials; it is semi-solid and can flow slowly
Outer Core: A liquid layer composed of iron and nickel that lies below the mantle
Inner Core: The deepest layer, a solid sphere made primarily of iron and nickel
Oceanic crust
Denser and usually younger than continental crust
Continental drift
The movement of continents over geological time
Pangaea
A supercontinent that existed around 335 million years ago
Plate tectonics
Explains the movement of Earth's plates; new crust is made at mid-ocean ridges, plates come together at convergent boundaries, and transform boundaries are where plates slide past each other
Seafloor spreading
The creation of new seafloor as plates diverge at mid-ocean ridges
Subduction zones
Where an oceanic plate sinks beneath another plate
Faults
Cracks in Earth's crust where movement occurs
Shear boundaries
Where plates slide past each other
The Atlantic ocean is getting bigger, while the Pacific is getting smaller
Evidence for plate tectonic theory includes fossil patterns, rock formations, and the fit of continental coastlines
Lithosphere
The rigidouter layer of the Earth
Asthenosphere
The softer layer beneath the lithosphere that allows tectonic plates to move
The earth doesn't get bigger because new crust creation is balanced by crust being recycled at subduction zones
Lithogenous sediments
Derived from rock debris
Biogenous sediments
Originate from biological material
Continental margins
The regions of the ocean floor that are adjacent to the continents, consisting of the continental shelf, continental slope, and continental rise
Continental shelf
Shallow, wide, and covers about 8% of the ocean
Continental slope
Steeper than the shelf, marking the boundary between continental and deeper oceanic crust
Continental rise
An underwater feature found between the continental slope and the abyssal plain, where sediments accumulate
Types of continental margins
Passive margins (found at places like the U.S. East Coast), feature little volcanic or seismic activity
Active margins (like the U.S. West Coast), are tectonically active with trenches and volcanoes
Deep-sea floor
Rugged and features submarine channels (underwater riverbeds), abyssal hills (small elevations), seamounts (underwater mountains), and guyots (flat-topped seamounts)