Go Back to 625-101 (Earth Sciences, Faculty of Science, v4, p185)
NOTE: These differences were detected by computer program - they may or may not be substantive.
Different CONTACT
Source=[39 lectures (three a week), 39 hours practical (three hours a week)]
Xref = [39 lectures (three each week), 39 hours practical (three hours each week)]
Different CONTENT
Source=[The Earth The origin of the Earth in a planetary system; the physical and chemical structure of the Earth; the geosphere; hydrosphere; and atmosphere; origin and composition of the atmosphere. Geological Materials Minerals: the nature of crystalline substances; the relationship between crystalline structure, chemical composition and physical properties of common minerals; rocks as aggregates of minerals; an introduction to igneous, sedimentary and metamorphic rocks. Plate Tectonics Why plate tectonics; where plates collide: volcanoes, earthquakes, continental collision and mountain building; where plates part: continental drift, sea-floor spreading, mid-oceanic ridges; within plates: uplift, weathering and erosion, transport of sediment, subsidence and sedimentation, volcanism. The Basics of Weather and Climate The Earth in space; the importance of its orbital characteristics; the ellipticity of the orbit; eccentricity, obliquity, cold poles and warm equator. The Atmosphere Basic properties of the troposphere, stratosphere, mesosphere; the friction layer; temperature; pressure and density in the vertical; the lapse-rate; mean sea-level; distributions of pressure, temperature, rainfall.]
Xref = [<i>The Earth</i> The origin of the Earth in a planetary system; the physical and chemical structure of the Earth; the geosphere; hydrosphere; and atmosphere; origin and composition of the atmosphere. <i>Geological Materials</i> Minerals: the nature of crystalline substances; the relationship between crystalline structure, chemical composition and physical properties of common minerals; rocks as aggregates of minerals; an introduction to igneous, sedimentary and metamorphic rocks. Plate Tectonics Why plate tectonics; where plates collide: volcanoes, earthquakes, continental collision and mountain building; where plates part: continental drift, sea-floor spreading, mid-oceanic ridges; within plates: uplift, weathering and erosion, transport of sediment, subsidence and sedimentation, volcanism. <i>The Basics of Weather and Climate</i> The Earth in space; the importance of its orbital characteristics; the ellipticity of the orbit; eccentricity, obliquity, cold poles and warm equator. <i>The Atmosphere</i> Basic properties of the troposphere, stratosphere, mesosphere; the friction layer; temperature; pressure and density in the vertical; the lapse-rate; mean sea-level; distributions of pressure, temperature, rainfall.]
Different SEMESTER
Source=[First semester,]
Xref = [First semester.]
Differences in Earth Sciences, Faculty of Arts (v3, p50)
Different CONTENT
Source=[The Earth The origin of the Earth in a planetary system; the physical and chemical structure of the Earth; the geosphere; hydrosphere; and atmosphere; origin and composition of the atmosphere. Geological Materials Minerals: the nature of crystalline substances; the relationship between crystalline structure, chemical composition and physical properties of common minerals; rocks as aggregates of minerals; an introduction to igneous, sedimentary and metamorphic rocks. Plate Tectonics Why plate tectonics; where plates collide: volcanoes, earthquakes, continental collision and mountain building; where plates part: continental drift, sea-floor spreading, mid-oceanic ridges; within plates: uplift, weathering and erosion, transport of sediment, subsidence and sedimentation, volcanism. The Basics of Weather and Climate The Earth in space; the importance of its orbital characteristics; the ellipticity of the orbit; eccentricity, obliquity, cold poles and warm equator. The Atmosphere Basic properties of the troposphere, stratosphere, mesosphere; the friction layer; temperature; pressure and density in the vertical; the lapse-rate; mean sea-level; distributions of pressure, temperature, rainfall.]
Xref = [<i>The Earth</i> The origin of the Earth in a planetary system; the physical and chemical structure of the Earth; the geosphere; hydrosphere; and atmosphere; origin and composition of the atmosphere. <i> Geological Materials </i>Minerals: the nature of crystalline substances; the relationship between crystalline structure, chemical composition and physical properties of common minerals; rocks as aggregates of minerals; an introduction to igneous, sedimentary and metamorphic rocks. <i>Plate Tectonics</i> Why plate tectonics; where plates collide: volcanoes, earthquakes, continental collision and mountain building; where plates part: continental drift, sea-floor spreading, mid-oceanic ridges; within plates: uplift, weathering and erosion, transport of sediment, subsidence and sedimentation, vulcanism. <i>The Basics of Weather and Climate </i>The Earth in space; the importance of its orbital characteristics; the ellipticity of the orbit; eccentricity, obliquity, cold poles and warm equator. <i>The Atmosphere</i> Basic properties of the troposphere, stratosphere, mesosphere; the friction layer; temperature; pressure and density in the vertical; the lapse-rate; mean sea-level; distributions of pressure, temperature, rainfall.]
Different OBJECTIVES
Source=[On completion of this subject, students should:
<p><i>Comprehend:</i></p>
<ul>
<li>the materials that the Earth is made of -- rocks, minerals and fossils;
<li>the diverse processes from continent-scale to microscopic-scale which shape the Earth;
<li>the mode of formation of the rocks which make up the geological record;
<li>the structure of the Earth's atmosphere;
</ul>
<p><i>Have developed:</i></p>
<ul>
<li>the skills to observe, in the laboratory and the field, basic properties of the global environment.
</ul>]
Xref = [On completion of this subject, students should:
<p>Comprehend:</p>
<ul>
<li>the materials that the Earth is made of - rocks, minerals and fossils;
<li>the diverse processes from continent-scale to microscopic-scale which shape the Earth;
<li>the mode of formation of the rocks which make up the geological record;
<li>the structure of the Earth's atmosphere;
<li>Have developed:
<li>the skills to observe, in the laboratory and the field, basic properties of the global environment.
</ul>]
Different POINTS
Source=[12.5]
Xref = [12.5 1st year]
Mon Oct 9 16:30:34 1995
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