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BGSU GEOL 1040 - Base levels
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Geol 1040 1st Edition Lecture 30Outline of Last Lecture II. Stream Profilesa. Definitionb. Creating onec. DischargeIII. Factors that control stream profilesa. Rock typeb. Plate tectonicsc. Sea leveld. ClimateOutline of Current Lecture IV. Two Types of Base levelsa. Ultimateb. Local or temporaryc. ExampleV. Changes in levelsa. Base levels b. Sea levelCurrent LectureIV. Two Types of Base levelsa. Ultimatei. Sea/ oceanb. Local or temporaryi. Lakec. Examplei. Local base level: Waterfallii. Resistance: Rockiii. Moves from high gradient to low gradientiv. Stream will eventually erode wall away until local base level and ultimate base level differentiation disappears *** erodes until local base is at sea level**V. Changes in levelsa. Base levelsi. Raising causes erosionThese notes represent a detailed interpretation of the professor’s lecture. GradeBuddy is best used as a supplement to your own notes, not as a substitute.ii. Lowering causes depositions b. Sea leveli. Drops = more erosionii. Raises = more


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BGSU GEOL 1040 - Base levels

Type: Lecture Note
Pages: 2
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