Use of cookies

We use cookies to improve and analyse your browsing experience on our web. You can accept these cookies, reject them or choose your settings by clicking on the corresponding buttons. Please note that rejecting cookies may affect your browsing experience. For more information you can consult our Cookies policy.

Configure cookies

Cookies are an essential part of how our web works. The main goal of cookies is to make your browsing experience more comfortable and efficient and to improve our services and the web itself.
Here you can find all the information about the cookies we use and you can activate and/or deactivate them according to your preferences, except for those cookies that are strictly necessary for the operation of the web. Blocking some cookies may affect your experience on the web and how the site works. For more information you can visit our Cookie Policy.

Strictly necessary (technical) cookies

These Cookies are necessary for the web to function and cannot be disabled on our systems. They are generally only set up in response to actions you may take such as requesting services, setting your privacy preferences, logging in or completing forms. You can set your browser to block or warn you about these cookies, but some parts of the web will not work. Information about Cookies.

Analytical cookies

These Cookies allow us to count the number of visits and traffic sources so that we can measure and improve the performance of our site. They help us to find out which pages are the most popular and least popular, and to see how visitors move around the web. All information collected by these Cookies is aggregated and therefore anonymous. If you do not allow these Cookies we will not know when you visited our web. Information about Cookies.

Third party cookies

These cookies are used to analyse your activity in order to show you personalised advertisements. Information about Cookies.

Accept Decline Configure cookies Confirm selected

tester
Search
×
Notes
Search
There are no notes
  • Activities. Studying the ocean floor
  • To customise Pencil press Alt + Down Arrow
  • To customise Highlighter press Alt + Down Arrow

    Change theme

    Error - please check your internet connection...
    Back

    Blink Help

    x
    Error - please check your internet connection...

    How can we help you?

    No results

    View full manual

    Couldn't find what you were looking for?

    Please describe the issue you are experiencing and provide as many details as possible. Let us know the book, class, access device, licence code, username, used browser or if it occcurs in our app:

    Thickness:
    Font size:
    Filter
      No resources found
      Revision mode

      Revision mode

      Activities. Studying the ocean floor
      Tectonic plates
      Without background sound
      Logo

      Studying the ocean floor. Activities 25- 40

      NaN/0
      t0-multimedia
      Activities. Studying the ocean floor
      Tectonic plates
      Without background sound
      Logo

      Activity 25

      P

      Apply

      Use the diagram to explain how sonar works.

      Ship using sonar

        1 attempt
      Done
      Activities. Studying the ocean floor
      Tectonic plates
      Without background sound
      Logo

      Activity 26

      0/15
      Understand

       

      Use an atlas or Internet application such as Google Maps or Google Earth to find the names of the Island arcs (1-8) and the ocean ridges (A-G).

      Philippines

      Lesser Anntilles (Caribbees)

      Tonga

      Southwest Indian Ridge

      East Pacific Rise

      South Georgia and the South Sandwich Islands

      Southeast Indian Ridge

      Aleutian Islands

      Japan

      Kuril Islands

      Pacific Antarctic Ridge

      Mid-Atlantic Ridge

      Mariana Islands

      Juan de Fuca Ridge

      Central Indian Ridge

      Island arcs Ocean ridges
      1. A.
      2. B.
      3. C.
      4. D.
      5. E.
      6. F.
      7. G.
      8.  

       

        Philippines Lesser Anntilles (Caribbees) Tonga Southwest Indian Ridge East Pacific Rise South Georgia and the South Sandwich Islands Southeast Indian Ridge Aleutian Islands Japan Kuril Islands Pacific Antarctic Ridge Mid-Atlantic Ridge Mariana Islands Juan de Fuca Ridge Central Indian Ridge

        3 attempts
      Done
      Activities. Studying the ocean floor
      Tectonic plates
      Without background sound
      Logo

      Activity 27

      0/5

      Analyse

      What differences can you see between these two oceans?

      • There is a trench next to the continent and the continent has volcanoes.

      • There are no trenches nor volcanoes near the coast of the continent.

      • There is a volcanic mountain range in the continent.

      • The continental slope connects the continental shelf with the abyssal plain.

      • There is a guyot and a volcanic island.

      Ocean on the left

        Ocean on the left

        Ocean on the right

          Ocean on the right

            /*%%SmartyNocache:14335235876820bf96c3e4b1_27503817%%*/smarty->registered_plugins[Smarty::PLUGIN_FUNCTION]['textweb'][0], array( array('name'=>"slide_classify_initial_group",'value'=>"Ninguno",'value_en'=>"Reset"),$_smarty_tpl ) );?> /*/%%SmartyNocache:14335235876820bf96c3e4b1_27503817%%*/ Ocean on the left Ocean on the right

            3 attempts
          Done
          Activities. Studying the ocean floor
          Tectonic plates
          Without background sound
          Logo

          Activity 28

          P

          Create

          Guyots are extinct and submerged volcanoes, with flat tops. Make a hypothesis to show the formation of guyots. What effect do you think their formation had on isostasy?

            1 attempt
          Done
          Activities. Studying the ocean floor
          Tectonic plates
          Without background sound
          Logo

          Activity 29

          0/1

          Analyse

          Compare the thickness, age and density of the continental and oceanic crust.

          • Oceanic crust is thinner, younger and less dense than the continental crust.

          • Correct answer
            Wrong answer
          • Oceanic crust is thinner, older and denser than the continental crust.

          • Correct answer
            Wrong answer
          • Oceanic crust is thinner, younger and denser than continental crust.

          • Correct answer
            Wrong answer

            3 attempts
          Done
          Activities. Studying the ocean floor
          Tectonic plates
          Without background sound
          Logo

          Activity 30

          0/1

          Analyse

          What happens to the thickness of sediment further away from the ridge? What could be the cause of this?

          The difference between the oceanic and continental crust
          • The thickness decreases because, the further away we go from the ridge, the older the ocean floor is, so sediment has been depositing on it for longer.

          • Correct answer
            Wrong answer
          • The thickness increases because the further away we go from the ridge, the younger the ocean floor is, so sediment has been depositing on it for longer.

          • Correct answer
            Wrong answer
          • The thickness of sediment near and far way from the ridge is always the same, as the sediment has been depositing everywhere at the same time.

          • Correct answer
            Wrong answer

            3 attempts
          Done
          Activities. Studying the ocean floor
          Tectonic plates
          Without background sound
          Logo

          Activity 31

          P

          Create

          Describe the landforms found on the ocean floor that are not found on the continents.

            1 attempt
          Done
          Activities. Studying the ocean floor
          Tectonic plates
          Without background sound
          Logo

          Activity 32

          P

          Create

          Find information about the first big oceanographic expedition carried out by the Challenger, in the 19th century. Compare its technology with modern oceanographic ships.

            1 attempt
          Done
          1. 1
          2. 2
          3. 3
          4. 4
          5. 5
          6. 6
          7. 7
          8. 8
          9. 9
            Eraser
            Rich text editor
            Editor toolbarsBasic Styles Bold Italic Underline Strikethrough Transform Text Switcher Text Color Background Color Subscript SuperscriptParagraph Insert/Remove Numbered List Insert/Remove Bulleted List Decrease Indent Increase IndentLine spacingLine spacingparagraph2 Align Left Center Align Right JustifyInsert Link Table Insert Special CharacterStylesFontFontSizeSize

            Press ALT 0 for help
            Back to top
            close