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What does the ocean floor look like, and what controls the temperature, salinity and density of seawater?

Describe the features of the ocean floor (continental shelf, slope, abyssal plain, mid-ocean ridge, trench) and explain how temperature and salinity control seawater density (Virginia 2018 Earth Science SOL ES.10).

A SOL-level answer on the ocean for the Virginia Earth Science EOC: the features of the ocean floor and how they relate to plate tectonics, what salinity is and what changes it, how temperature and salinity control seawater density, and why this drives deep circulation, with worked exam questions.

Generated by Claude Opus 4.812 min answer

Reviewed by: AI editorial process; not yet individually human-reviewed

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  1. What this topic is asking
  2. Features of the ocean floor
  3. Salinity
  4. How temperature and salinity control density
  5. Try this

What this topic is asking

Virginia Earth Science SOL standard ES.10 asks you to describe the ocean floor and the properties of seawater. The EOC tests this with labeled cross sections of the ocean floor (match the feature), with the link between ocean-floor features and plate tectonics, and with reasoning about density from temperature and salinity. The density idea then explains the deep currents covered in the next topic.

Features of the ocean floor

The ocean floor is not flat: it records plate tectonics directly. New crust is made at the ridges and destroyed at the trenches, which is why the youngest seafloor is at the ridge and the oldest near the trenches.

Salinity

So a tropical sea with high evaporation is saltier than the mouth of a large river, where fresh water dilutes the salt.

How temperature and salinity control density

This single rule, cold and salty equals dense and sinks; warm and fresh equals less dense and floats, explains the layering of the ocean and sets up the deep currents in the next topic.

Try this

Q1. Name the deep-ocean feature where new oceanic crust forms. [1]

  • Cue. The mid-ocean ridge (a divergent boundary, seafloor spreading).

Q2. Explain how evaporation changes the salinity of seawater. [2]

  • Cue. Evaporation removes water as vapor but leaves the dissolved salts behind, so the remaining water has a higher salinity.

Exam-style practice questions

Practice questions written in the style of VDOE exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

VA Earth Science SOL 2023 (style)1 marksWhich ocean-floor feature is the gently sloping, shallow, submerged edge of a continent? (A) the abyssal plain. (B) the continental shelf. (C) the mid-ocean ridge. (D) the trench.
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A 1-point multiple-choice item on ocean-floor features.

The correct answer is B. The continental shelf is the shallow, gently sloping submerged edge of a continent, where the water is relatively shallow and biologically productive. The abyssal plain (A) is the flat deep-ocean floor, the mid-ocean ridge (C) is the underwater mountain chain where new crust forms, and a trench (D) is the deepest part, formed at subduction zones.

The test rewards matching each feature to its position and origin, starting at the shallow shelf near land.

VA Earth Science SOL 2024 (style)2 marksTwo samples of seawater are at the same temperature, but sample X is saltier than sample Y. (a) State which sample is denser and why. (b) Explain what happens when cold, salty water meets warmer, less salty water at the surface.
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A 2-point item on seawater density.

(a) 1 point: sample X (saltier) is denser, because adding dissolved salt increases the mass per unit volume of the water.
(b) 1 point: the colder, saltier (denser) water sinks below the warmer, less salty (less dense) water, which drives vertical (density-driven) circulation in the ocean.

Markers reward identifying the saltier sample as denser in (a) and the sinking of denser water in (b).

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