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Basic Chemistry• An atom is a basic chemical building block
of matter. An atom consists of protons, neutrons, and electrons.
Particle Charge LocationProton Positive In nucleusNeutron Neutral nucleusElectron negative Orbits the nucleus
• Which particles determine the mass of an atom? The number of protons plus the number of neutrons
• Which particle refers to the atomic number for an element? Protons
4. Identify the atomic number and the atomic mass for this element.
• atomic number _1_
• atomic mass __1.0079_Hydrogen
1H
1.0079
Measuring Matter
1. How is density calculated? Density = mass/volume
2. What is the density of an object with a volume of 15cm3 and a mass of 45g?
• 3.0 g/cm33. What is the density of an object with a
volume of 30cm3 and a mass of 60 g?• 2.0 g/cm34. What is the density of an object with a
volume of 30 cm3 and a mass of 25g?• 0.83 g/cm3
5. Use the densities to describe the placement of each of these objects in a container of water (the density of water is 1.0 g/cm3). The object with a density of 0.83 g/cm3 will float in water; the other two objects will sink in the container.
Structure of the Interior of Earth
The Earth's interior consists of rock and metal. It is made up of four main
layers. Describe each layer in terms of temperature, composition, and
thickness.
Layer of the Earth
Temperature Composition Thickness
Inner Core 6600 C Solid Nickel and iron
5200 – 6400 km
Outer Core 5500 C Liquid nickel and iron
2900 – 5200 km
Mantle 1500 – 5000 C Silicon and oxygen
670 – 2900 km
Crust Surface temperatures –
1000 C
Mostly silicon and oxygen
35 km
• The crust and the mantle can be divided into the lithosphere and asthenosphere. Describe each
of these layers.
Layer Description Crust, Mantle, or
Both
Physical State
Lithosphere outermost layer
Crust and mantle
solid
Asthenosphere Layer beneath the
lithosphere
Part of the lower mantle
Soft solid; has
plasticity
Minerals
• What is a mineral? a solid with a crystalline structure that is naturally occurring, with a defined chemical composition.
1.Use the table below to describe the properties of minerals.
Property Description Examples
Color Most easily observed, but the least useful
Pink, grey, green, blue
Luster The way light is reflected from a newly exposed
surface
Metallic or nonmetallic(glassy, pearly, waxy)
Streak The color of the mineral in the powder form
Pink, grey, dark colored, no streak
Crystal Structure Pattern of a mineral controlled by the
arrangement of atoms
Hexagonal, cubic,
Hardness The ability of one mineral to scratch another; the
softer mineral gets scratched
Talc – 1.0Feldspar – 6.0
Diamond – 10.0
Cleavage or Fracture
The surface displayed when a mineral breaks
Smooth/flat surfaceRough/irregular surface
Acidity The concentration of acid in a mineral
High acidity = calcite
Magnetism The force exerted by a magnetic field
Strong attraction = high iron content
Class Description Example and Formula
Silicates Most common mineral group; contains silicon and oxygen
Talc - (Mg,Fe)3Si4O10(OH)2
Carbonates Contains a carbonate group (CO3).
Calcite (CaCO3)
Oxides consist of oxygen and another element
(H2O) and magnetite (Fe3O4)
Sulfides Contain sulfur ions Pyrite, FeS2 or “fool’s gold”
Sulfates Contain a sulfate group (SO4) Anhydrite CaSO4
Halides Contain a “salt” ion such as Na, Cl, or F
Halite (NaCl)
Native Elements
Minerals that exist in pure elemental form
gold (Au), silver (Ag), and copper (Cu)
1. Minerals can also be classified according to color. Which minerals are silicates that are low in iron and magnesium and light in color? Felsic
2. Give an example of the type of mineral described in number 4 and write the chemical formula. Quartz (SiO2)
3. Which minerals are silicates that contain higher levels of iron and/or magnesium and are dark-colored? Mafic
4. Give an example of the type of mineral described in number 6 and write the chemical formula.
Olivine ((Fe, Mg)2SiO4)
5. According to the table, which mineral is capable of scratching garnet? Corundum
Rock How it Forms
Igneous Melting, cooling, and solidification of magma
Metamorphic Heat, pressure, and crystallization
Sedimentary Compaction and cementation
Draw a diagram of the rock cycle below. Use the terms in #3 in
your diagram to show the processes that form rocks.
Physical Weathering breakdown of rocks and minerals by
a mechanical process.
Freezing and thawing of water, plant
growth, actions of animals, friction
Chemical Weathering chemical change that results in the decomposition of
rocks and minerals.
Chemical reactions: oxygen, water, carbonic acid
3. What is metamorphism? the changes in the composition and/or texture of a rock that result from increasing pressure and/or temperature.
4. What are two types of metamorphism? Describe each. Contact metamorphism occurs when rocks come in contact with a heat source. Regional metamorphism occurs when a large area of rock undergoes increased temperatures and pressure.
3. What type of metamorphism is described in this example?
Marble is created from limestone that has been subjected to heat from an
igneous intrusion.
4. What are factors that increase the rate of weathering? Higher temperatures, increased water flow, increased surface area
3. Sedimentary rocks form from sediment . Explain how sediments are deposited along the bottom of an ocean floor according to size. The largest sediments are deposited near the shore. Increasingly smaller sediments settle out farther from the shore where the water is calmer.
Rock How it Forms
Igneous Melting, cooling, and solidification of magma
Metamorphic Heat, pressure, and crystallization
Sedimentary Compaction and cementation
2. How does the cooling rate of an igneous rock affect its’ texture? Give and example of a rock with slow cooling rate and fast cooling rate.
Quick cooling = fine grains (pumice)/slow cooling = coarse grains (granite)
2. Describe the texture of a foliated and nonfoliated metamorphic rock.
Foliated metamorphic rocks have layers or bands of crystals (gneiss/slate). Nonfoliated metamorphic rocks do not have layers or bands of crystals and are usually more uniform (marble/quartzite)