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Using The Venn Diagram For Developing University Students’ Analytical Geographical Thinking

Table 4:

The landform Specific aspects Common aspects Specific aspects The landform
Field/Plain - altitudes below 300 m - deep valleys below 100 m - plain surfaces and interfluves prevail- geology: soft rocks, sedimentary, sands - altitudes above 300 m- deep valleys above 100 m Plateau
Mountain - made by pleated processes, eruptions - steep slopes and ridges - landforms- present in Romania - the altitudes are generated by the raising mountains - lower temperatures compared to the mountains Hill
Plate - altitudes above 300 m - large and plain surfaces - formed by soft rocks as sand and clay - deep valleys over 100 m - altitude between 300 and 800 m- sloping surfaces Hill
Field - low altitudes- plain interfluves - it can be cultivated- it can be used as pastures - altitudes between 200 and 800 m- forests prevail Hill
Hill - sloping surfaces prevail - deep valleys over 100 m- altitudes over 300 m- formed by soft rocks as sedimentary, sands and clay - large and plain surfaces prevail - hard rocks prevail Plateau
Mountain - higher altitudes- above 800 m - they are forms of relief- both have plants and animals - lower than mountains- well populated Hill
Plate - large interfluves and plain surfaces- made of hard rocks and pleat sedimentary - deep valleys, over 100 m- altitudes over 300m- made of soft rocks as sedimentary, sand and clay - sloping areas and slope prevail compared to the interfluves and the plain areas Hill
Mountain - altitudes above 800 m- strong sloping areas prevail - made of rocks- crossed by rivers- present in Romania - lower altitudes under 300 m- plain surfaces prevail- higher temperatures Field
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