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5 Written questions

5 Matching questions

  1. Tidal currents
  2. Longitudinal dunes
  3. Marine Scarp
  4. T-
  5. What is the second basic cause of precipitation?
  1. a consist of long, narrow ridges orientated parallel with the direction of the prevailing wind and may be many miles long and only a few yards high.. or may have a Sief dune
  2. b tundra; associated with E climate
  3. c the forced lift of moist air over mountain barrier. Generated by the forced ascent of moist air over a mountain barrier is termed orographic precipitation.
  4. d rising tides set in motion in bays and estuaries currents of water
  5. e the waves from erosion form a steep bank, the waves then retrear steadily under the erosion of the storm waves

5 Multiple choice questions

  1. Arid (desert)
  2. lies between two large anticyclones (high pressure systems) one of cold dry polar air and the other of warm moist maritime air mass. Air is converging from opposite directions on both sides of the front.. with the formation of the occluded fronts
  3. when particles and chemical pollutants are present in considerable density over an urban area
  4. dry season in summer
  5. the widening and building shoreward of a beach...sand arrives at a particular section of the beach more rapidly than it can be carried away.

5 True/False questions

  1. Nimbostratusa cumuliform cloud that develop tall stalk-like shapes and penetrates high into the troposphere (thunderstorm clouds)

          

  2. New Landbarren expanses of silt and clay exposed at low tide but covered at high tide

          

  3. Lagoonare more or less circular coral reefs enclosing a lagoon but without any land inside (just lagoon). Most are built on a foundation of volcanic rock- volcanoes rising from ocean floor.

          

  4. Adiabatic processchange of temperature within a gas because of compression or exmpansion, without gain or loss of heat form the outside. Therefore, expansion always results in cooling and compression results in warming

          

  5. Deltais a sediment deposit built by a stream entering a body of standing water and formed by the stream load

          

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