Ocean Mapping Techniques and History
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Questions and Answers

What is the primary difference between a white smoker and a black smoker?

  • White smokers release water rich in iron and magnesium, while black smokers release water rich in hydrogen sulfide.
  • White smokers release cooler water, while black smokers release hotter water. (correct)
  • White smokers form chimneys made of calcium carbonate, while black smokers form chimneys made of iron sulfide.
  • White smokers are located near mid-ocean ridges, while black smokers are found in abyssal plains.
  • Which of the following is NOT a characteristic of abyssal plains?

  • They are commonly found in the Atlantic and Indian Oceans.
  • They are formed by the suspension settling of fine particles.
  • They are characterized by abundant hydrothermal vents and seamounts. (correct)
  • They are some of the deepest and flattest parts of Earth.
  • What is the primary method used in satellite-based ocean mapping?

  • Measuring the temperature variations in the ocean.
  • Analyzing the reflection of sound waves from the seafloor.
  • Measuring the gravitational pull of the seafloor. (correct)
  • Tracking the movement of ocean currents.
  • What is the primary difference between active and passive continental margins?

    <p>Active margins are located near plate boundaries, while passive margins are not. (A)</p> Signup and view all the answers

    Which of the following is NOT a feature found on a continental margin?

    <p>Abyssal plain (C)</p> Signup and view all the answers

    What is the primary advantage of using echo soundings to map the seafloor?

    <p>It can map large areas of the seafloor quickly and efficiently. (D)</p> Signup and view all the answers

    Which of the following ocean provinces is characterized by the presence of hydrothermal vents?

    <p>Mid-ocean ridges (A)</p> Signup and view all the answers

    What is the primary difference between a seamount and a guyot?

    <p>Seamounts have a conical shape, while guyots have a flat top. (B)</p> Signup and view all the answers

    What is the primary source of information for creating a hypsographic curve?

    <p>All of the above (D)</p> Signup and view all the answers

    Which of the following best describes the term 'fathom'?

    <p>A unit of measurement for the depth of the ocean, equal to six feet. (C)</p> Signup and view all the answers

    Study Notes

    Ocean Mapping

    • Methods used to map the seafloor have strengths and weaknesses.
    • Three major ocean provinces and their subdivisions with key features are listed and described.
    • Active and passive continental margins are contrasted, including differences in tectonic activity and sediment accumulation.
    • Interplate features like seamounts and guyots and their formation are identified and described.
    • The hypsographic curve is used to discuss the height of land, depth of the ocean, and the area of Earth covered by land and sea.

    Early Ocean Mapping

    • Early methods included nautical instruments and maps.
    • Fathoms (feet) and meters are both used to measure depths.

    HMS Challenger

    • Conducted the first systematic ocean floor measurements in 1872.
    • Stocked 144 miles of rope.
    • Made 492 bottom soundings.
    • Found that the deep ocean floor has relief.

    Echo Soundings

    • Echo sounders use sound waves to measure depth.
    • Depth is calculated from the time it takes for the sound to travel to the seafloor and return.
    • The formula to calculate depth is D = 1/2 * v * t.

    GLORIA Side Scanning Sonar

    • A geological instrument utilizing long-range inclined acoustic sensors.
    • Measures the shape of the seafloor.
    • Images from GLORIA provide data gaps, showing an incomplete survey of the seafloor.

    Mapping from Space

    • Satellite measurements are used to study sea floor features.
    • Measurements of sea surface bulges caused by gravitational anomalies, are used to indirectly calculate bathymetry (sea depth and shape).

    Comparing Bathymetric Maps

    • Bathymetric maps illustrate seafloor topography.
    • Comparing maps from various resources (ship v. satellite).
    • Ship-based methods and satellite-based methods vary, and are compared.

    Ocean Profiles

    • Displays various topographic cross sections of different ocean areas (based on echo sounder data).
    • Depicts the varied topography of ocean basins.

    Ocean Provinces

    • Shows different ocean provinces (Continental margins, ocean basins).
    • Demonstrates the Mid-Atlantic Ridge, a submarine mountain range.
    • Identifies the continental margin for both North and South America as well as Europe and Africa.

    Continental Margin

    • Continental margins include the shelf, shelf break, slope, and rise.
    • A diagram illustrates these features in a cross-section.

    Active and Passive Margins

    • Active margins are located close to plate boundaries and exhibit tectonic activity.
    • Passive margins are not close to plates boundaries and show little tectonic activity.
    • Active margins have steeper slopes, less wide shelves, and trenches, while passive margins have gentler slopes and wider shelves.

    Passive Margins

    • Passive margins are not close to any plate boundaries.
    • They have no major tectonic activity.
    • East coast of the United States is an example of a passive margin.

    Active Margins

    • Active margins are located close to or on plate boundaries.
    • These areas have variable tectonic activity like trenches (e.g., Mariana Trench).
    • The Pacific Ring of Fire is an active region with numerous trenches and volcanoes.

    Deep Ocean Basin: Abyssal Plains

    • Abyssal plains extend from the base of continental rises.
    • They are the deepest, flattest parts of the Earth.
    • Fine particles settle, forming the flat surface.
    • Well developed in the Atlantic and Indian Oceans.

    Abyssal Hills and Seamounts

    • Abyssal hills are small, gently sloping hills.
    • Seamounts are large, isolated underwater volcanic mountains.
    • Table mount or guyots are submerged volcanic mountains with flattened tops.

    Mid-Ocean Ridges

    • Mid-ocean ridges are underwater mountain ranges where seafloor spreading occurs.
    • Show varying water depths across the mid-ocean ridge, indicating geological features and plate movement.

    Mid-Ocean Ridges: Hydrothermal Vents

    • Hydrothermal vents are openings in the seafloor where hot, mineral-rich water emerges.
    • Vent activity is related to magma chambers.

    White Smokers

    • Release cooler water (30-350°C).
    • Rich in barium, calcium, and silicon.
    • Mineral precipitates create white "smokes".

    Black Smokers

    • Water temperatures exceed 350°C.
    • Solutions exiting vents are acidic.
    • Rich in hydrogen sulfide.
    • Creates black precipitates, forming chimneys.

    Hypsographic Curve

    • Illustrates the percentage of Earth's surface covered by land and sea at various elevations and depths.
    • Shows the average elevation of land and the average depth of the oceans.
    • Shows how land and water are distributed across the planet.

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    Ocean Mapping Lecture Notes PDF

    Description

    Explore the various methods and historical milestones in ocean mapping, from early nautical instruments to advanced echo soundings. This quiz covers the strengths and weaknesses of different mapping techniques, interplate features, and significant expeditions like the HMS Challenger. Test your knowledge on the key concepts of ocean provinces and continental margins.

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