Monday, February 27, 2012
Chemistry Retest
Any chemistry student wishing to retest "Balancing Equations" please see me and I will enroll you in e2020.
Sunday, February 26, 2012
Week of 2/27/12
Chemistry
Monday- pH lecture, watch pH lecture
Tuesday- review problems/ possible lab
Wednesday- moodle pH, radioactivity simulations
Thursday- finish pH, lab
Friday - 'critical reading activity'
Physical Science
Monday- positive choices talk, watch divergent/convergent boundary lectures on moodle for Thursday
Tuesday- boundary activity
Wednesday- computer lab (google Earth), finish group work/activity sheet/Alution Trence activity
Thursday- boundary activity
Thursday- Boxer Day Tsunami, google Earth
Monday, February 20, 2012
Week of 2/20/12
Chemistry
Monday- off
Tuesday - Friday - juniors ACT prep, seniors bring work to do.
Physical Science
Monday- off
Tuesday-Plate Tectonics review
Wednesday-computer lab start "google Earth" lab
Thursday-Plate Tectonics
Friday-Finish Plate Tectonics Lab
Monday- off
Tuesday - Friday - juniors ACT prep, seniors bring work to do.
Physical Science
Monday- off
Tuesday-Plate Tectonics review
Wednesday-computer lab start "google Earth" lab
Thursday-Plate Tectonics
Friday-Finish Plate Tectonics Lab
Thursday, February 9, 2012
Sedimentary and Metamorphic Rocks
Let's finish-up talking about rocks.
Sedimentary Rocks:
Sedimentary Rocks:
- form from the weathering and erosion of previous rocks
- the process is- weathering, erosion, deposition, compaction, cementation
- clastic rocks form from fragments of material ex; conglomerate and sandstone
- chemical rocks form from the precipitation of minerals from water (oceans) ex; rock salt and rock gypsum
- fossils are found in sedimentary rocks, the other rock processes would destroy the fossils. Interesting fact, even ripple marks from streams or beaches can be fossilized.
- these rocks form from extreme heat and pressure placed upon pre-existing rocks.
- heat is the primary agent for contact metamorphism, this heat is supplied by nearby magma.
- during metamorphism minerals may recrystallize, crystals can grow larger and the rock will become more compact.
- running water is NOT an agent of metamorphism.
Igneous Rocks
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Pictures courtesy of Univ of Texas Geology Dept.
Let's review some terms on Igneous Rocks:
- Intrusive rocks- those that form from cooling magma beneath the Earth's surface (ex. granite, picture on left), they will have a course-grained texture.
- Extrusive rocks- those that form from magma that has reached the Earth's surface, lava, they will have a fine- grained texture ( ex. basalt, picture on right).
- Granitic- light colored rocks contain greater amounts of feldspar (felsic).
- Basaltic- dark colored rocks contain greater amounts of magnesium (mafic).
- Porphyritic- type of rock that has two different crystal sizes.
- Remember, igneous rocks are characterized by composition and texture.
The Rock Cycle
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Important- the energy that drives the Rock Cycle comes from the Earth's interior (igneous and metamorphic rocks) and from the Sun (weathering for sedimentary rocks).
- When magma cools igneous rocks can form intrusive (below ground) or extrusive (above ground).
- Compaction and cementation (lithification) from the weathering of surface rocks for sedimentary rocks.
- Metamorphic rocks occur deep in the ground from the processes of high temperatures and high pressures.
Recap on Minerals
A few more facts on minerals:
- composition and structure determines the properties of a mineral.
- density of a mineral is determined by dividing the mass by the volume
- density is a very important property of a mineral, ex: to tell if a sample of gold is gold check the density of the sample.
Mineral Identification
Physical properties of minerals include:
- crystal form- shape, arrangement of atoms
- cleavage- tendency to break with a smooth plane
- fracture-uneven breakage of a mineral
- luster- how light is reflected from the surface
- color- obvious, but not very reliable
- streak- color of a mineral in powder form
- density- ratio of mass/volume
- hardness- resistance to abrasion, using Moh's scale of hardness
Mineral Formation
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Minerals are formed in the Earth's crust by four major processes:
- magma- molten rock in the crust, as it cools this magma crystallizes to form minerals.
- precipitation- as water evaporates, the dissolved minerals are left behind (ex. limestone, gypsum).
- high pressure/high temperature- these minerals can recrystallize deep within the Earth's crust.
- hydrothermal solutions- hot water and dissolved substances can come into contact with existing minerals, and react to form new minerals.
Mineral Composition
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Minerals are classified by their composition, the elements that they are made of. As seen by the graph ( left) the most abundant element in the Earth's crust (by weight) is oxygen.
The major mineral groups are:
- silicates- (above right) this is the most common mineral group as it contains oxygen and silicon. ex. feldspar
- carbonates-contain carbon and oxygen, ex. limestone
- oxides- contain oxygen and a metal element, ex. TiO2, rutile
- sulfates/sufides- contain sulfur, hint-all minerals in this group contain sulfur. ex. pyrite
- halides- contain a halogen (salt formers) ex. halite-table salt.
- native - minerals of only one element, ex. gold
Minerals
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Minerals typically are composed of two or more elements and have the following properties:
- inorganic- not derived from living things
- naturally occuring- not "fake"
- solids- cannot be a liquid or gas
- crystalline shape- orderly arrangement of atoms
- chemical composition- definite composition
Thanks to Philip Staublin for pointing out that there are some minerals that are considered "native minerals" composed of only one element. This is for Philip- good catch- we did cover native minerals in class but it is not going to be a test question- so I did not blog it, Mr. V.
Sunday, February 5, 2012
Week of 2/6/12
A reminder to all classes. Unless instructed otherwise email me all work as a PDF attachment.
Chemistry
Monday- Lincoln Tech, watch "Kahn" lecture Balancing
Tuesday - balancing equations Ch 11
Wednesday- Ch 11, computer lab
Thursday- Ch 11
Friday- computer lab writing assignment
Physical Science
Monday- Wise choices, watch Rock lecture
Tuesday- rock samples, rock cycle
Wednesday- computer lab,
Thursday- rock reinforcement
Friday- rock ID
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