Lab Practical Information Regents Earth Science

When? Wednesday 5/31/2011 –Everyone

Where? All classes report to room (here) as normal.

Some Simple Rules ON TIMEBe ON TIME Do not be absent!Do not be absent! Pen AND Pencil!Pen AND Pencil! READ DIRECTIONSREAD DIRECTIONS NO TALKINGThere is to be absolutely NO TALKING –If you choose to talk, your exam booklet will be taken from you 0 –You will receive a 0 for the Regents grade –You will have to re-take the Regents Exam in August & possibly have to go to Summer School 

What is the Lab Practical? First part of the Regents Exam Test divided into 3 stations Students are given 9 minutes per station

Station 1: Mineral and Rock Identification Using a mineral identification kit, the student will determine the properties of a mineral and will use those properties to identify that mineral from a flowchart. Using rock identification charts from the Earth Science Reference Tables and the characteristics observed in two rock samples, the student will classify each rock as igneous, sedimentary, or metamorphic.Using a mineral identification kit, the student will determine the properties of a mineral and will use those properties to identify that mineral from a flowchart. Using rock identification charts from the Earth Science Reference Tables and the characteristics observed in two rock samples, the student will classify each rock as igneous, sedimentary, or metamorphic.

Mineral Properties Luster –metallic or nonmetallic—glassy, dull, pearly Cleavage or Fracture –are the broken sides of the mineral semi-smooth surfaces, or non-smooth broken surfaces? Streak –using white streak plate to see color of powdered mineral Hardness –using glass scratch plate

Luster? Cleavage? Streak? Hardness? Mineral Name? Luster? Cleavage? Streak? Hardness? Mineral Name?

Metallic Luster

Rock Properties and Classification Classify 2 different rock samples –Sedimentary, Igneous, Metamorphic State a reason for your classification

Igneous Rocks Granite Basalt Pumice Obsidian

Igneous Rocks: –Multiple-mineral composition –Crystalline texture –Interconnected mineral crystals with NO layering –Glassy texture –Rounded gas pores or spaces

Sedimentary Rocks Limestone Layered sediments Fossil

Sedimentary Rocks: –Bedding or layering of sediments –Rounded grains, clasts, fragments or sediments –Fossils –Cemented sediments with visible pores or openings –Contain fragments of other rocks

Metamorphic Rocks Gneiss Quartzite Schist Slate

Metamorphic Rocks: –Multiple-mineral composition –Interconnected mineral crystals WITH layering (foliation) –Slaty, schistose or gneissic foliation –Distorted or wavy rock structure –Stretched pebbles –A high percent of mica minerals

Station 2: Locating an Epicenter Using seismic data, the Earthquake P- wave and S-wave Travel Time graph from the Earth Science Reference Tables, a safe drawing compass, and a map, the student will determine the location of an earthquake epicenter

2:33:002:35:30 00:02:302:35:30 – 2:33:00 =

Station 3: Constructing and Analyzing an Asteriod’s Elliptical Orbit Using two pins, a looped string, a metric ruler, and a calculator, the student will construct an ellipse, determine its eccentricity, and apply this information to our solar system.

Eccentricity A number indicating the roundness of an ellipse. Eccentricity = Distance Between Foci Length of Major Axis e=d/L Page 1 in your BEST FRIEND

Measure to the nearest tenth! 0.1 Calculate e to the nearest thousandth! Please Remember

e = 0 e = 1 Perfect circle Straight line Please Remember

Planets change orbital speed as they revolve around the Sun.

Please Remember As distance from the Sun increases, a planet’s period of revolution increases.

ACCURATELYBe sure to Read & Measure ACCURATELY Remember: NO TALKING Be on time! Do not be absent!