Geol 1040 1st Edition Lecture 24Outline of Last Lecture XXVI. Types of stressa. Compressionalb. Tensionc. Shear stressXXVII. Types of faultsa. FractureOutline of Current Lecture XXVIII. Convergent boundariesa. Stressb. Strainc. GeographyXXIX. Divergent Boundariesa. Stressb. Strainc. GeographyXXX. Transform Boundariesa. Stressb. Strainc. GeographyXXXI. Deformation: Foldsa. Causeb. Typesc. PartsCurrent LectureXVIII. Convergent boundariesa. Stressi. Compressionalii. Pushing togetherb. Straini. Reverse faults1. Foot wall goes down, hanging wall moves upc. Geographyi. Alps/ Andes/ CascadesXIX. Divergent Boundariesa. Stressi. TensionalThese 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. Pulling apartb. Straini. Normal Fault1. Foot wall moves up, hanging wall moves downc. Geographyi. Mid Ocean Ridge, Icelandic RidgeXX. Transform Boundariesa. Stressi. Shearii. Opposite directionsb. Straini. Strike-slipii. Hanging wall and foot wall move away from each otherc. Geographyi. San Andreas Fault, Alpine faultXXI. Deformation: Foldsa. Causei. Compressional stress from convergent boundariesb. Typesi. Anticline1. Oldest layer in the middle. 2. Upside down U shapeii. Syncline1. Newest layer in the middle2. U Shapec. Partsi. The crease, or arch, is known as the hingeii. The parts of rock coming from the hinge is the
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