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Performance Test Review. June 2012. General overview of the test. Three stations 9 minutes per station ALL materials supplied by teacher including pencils, ESRT pages, calculators, etc. DO NOT be late for class on the day of your test! The test will be given in ________________________
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Performance Test Review June 2012
General overview of the test • Three stations • 9 minutes per station • ALL materials supplied by teacher including pencils, ESRT pages, calculators, etc. • DO NOT be late for class on the day of your test! • The test will be given in ________________________ • Leave ALL belongings outside the room • You may only come in with a pen or pencil (no other items are allowed)
General advice • Study these notes before the test! • Make sure to read CAREFULLY all directions on the test • Be careful to round numbers according to the directions tenths place one decimal like 0.2 or 1.6 • Write down your station code numbers as soon as you sit-down at your station • Do not talk during test! • Don’t be nervous, you have seen all this before!
Specific stations on the test • Station #1: Rocks and minerals • Station #2: Ellipses • Station #3: Earthquake epicenter
Station #1: Rocks and minerals (see Mineral PowerPoint for details) • TASKS: (1) Determine the identity of a mineral based on a set of characteristics that you find. You will use a flow chart for this. (2) Determine the identity of a rock based on a set of characteristics that you find. You will use a flow chart for this. • Minerals: Naturally occurring, crystalline solids with well-defined chemical and physical properties
Ways to identify minerals • Hardness (1-10) • Cleavage or fracture • Streak test • Crystal shape • Acid test • Density (specific gravity) • Taste
Cleavage • Results from weaknesses in atomic structure
Fracture • Uneven breakage within minerals
Streak test Streak color Streak plate
Hardness test • Harder or softer than glass • If mineral scratches glass, then object is harder than glass • If does not leave a scratch on the glass, then object is softer than glass
Rocks • Rocks: Composed of two or more minerals (not pure substances) • Three kinds of rocks 1) Igneous: cooling and solidification of magma or lava 2) Sedimentary: compaction and cementation of sediment 3) Metamorphic: changes in heat and pressure
Igneous rocks granite All have interlocking crystals except obsidian which has glassy texture.
Sedimentary rocks Conglomerate Sandstone All are fragmental (clastic) and/or contain fossils. limestone
Metamorphic rocks Gneiss showing banding (type of foliation) Slate showing foliation
Station #2 Ellipses (see Ellipse notes for more details) • TASK: Draw an ellipse and determine the eccentricity • Ellipse: A circle that has been stretched-out (oval) • Formula: e = d/L DEMO • http://vids.myspace.com/index.cfm?fuseaction=vids.individual&videoid=35689164
Station #3: Earthquake epicenter (see Earthquake notes for more details) • TASK: Determine the position of an earthquake epicenter DEMO • http://vids.myspace.com/index.cfm?fuseaction=vids.individual&videoid=57489815