Science 7
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Transcript of Science 7
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Science 7Discovering Science 7
Unit 4“Earth’s Crust”
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Chapter 10
Earth’s Crust Is Made Up Off Rocks And Mineral.
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Minerals vs. Rocks• Minerals –
A mineral is a pure substanceex. Gold
• Rocks – A rock is a mixture of two or more minerals.ex. Granite
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Mineral/Rock Identification• Lustre – how light is reflected of the material (Dull, Glassy or
metallic).
• Colour – Spectrum of colour.
• Hardness – Moh’s Hardness Scale (1 softest ex. Talc and 10 hardest ex. Diamond).
• Streak – Residue left after a rock is streak across porcelain
(powder,…) • Cleavage – Splitting along smooth, flat surfaces called
planes. Ex. Mica
• Fracture – Splitting along rough jagged edges.
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Families of Rocks
Igneous, Sedimentary and Metamorphic
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Igneous Rock• Intrusive Rock -
Formed when molted rock (magma) cools under the surface of the earth.ex. Granite
• Extrusive Rock – Formed when molted rock (lava) cools on the surface of the earth.ex. Obsidian
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Sedimentary Rock• Formed when loose particles, weathered
and eroded away, are compacted together. The extreme pressure and heat help cement the particles together.
• Cementation – Process by which pieces of sediments are held together by another material.
• Layers of sediments form beds.
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Sedimentary Rock
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Metamorphic Rock• Metamorphic means “changed form”.• Formed when extreme pressure and heat,
or hot fluid changes one type of rock into another.
• The formation of metamorphic rock is a slow process.
• Parent Rock - The type of rock which has been changed into metamorphic rock.
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Metamorphic Rock
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The Rock Cycle
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Many Things Are Made From Minerals and Rocks
• Zippers• Watches• Shirts• Blood• Muscles• Shoes• Detergents
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Mineral and Rock Resources• Petroleum and Coal – made from the remains of
once living things.
• Metals – Copper, Zinc, Nickel, iron, …
• Gems – Sapphires, Diamonds, emerald, Amethyst, …
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Chapter 11Earth’s Crust Is Constantly Changing.
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The Layers of the Earth
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The Earth’s Moving CrustAlfred Wegener (1880-1930)
• Paleogeographic Evidence – Shape of Continent- Pangaea- Theory of Continental Drift
• Biological Evidence – Fossils• Geological Evidence – Rocks and Rock Layer• Meteorological Evidence – Climate Change
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Wegner’s Theory RejectedWhat caused the platesto move?
Without an answer,some scientist rejectedhis theories.
Today we accept theexplanation of convectioncurrents
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Evidence From The Sea Floor• Sonar (Sound Waves)
• Magnetometers (Magnetic Fields)
• Deep Sea Drilling (Core Samples)
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Types of Plate Boundaries• Divergent Boundaries
– Pulling apart
• Convergent Boundaries – Pushing together
• Transform Boundaries – Sliding past (J. Tuzo Wilson)
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Convection Currents• The driving force that possible causes
plates tectonics (movement of the earth’s crust).* The creation of subduction zones – The area of the crust when one plate is push below another plate.
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Earth’s Crust Catastrophe’sEarthquakes
- Seismograph (Seismic Waves)- Bedrock- Richter Scale- Focus and Epicentre
VolcanoesOccur:- areas where plates converge- areas where plates diverge- areas where plates are thin (hotspots)
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Mountain Building• Fold Mountains
• Fault Block Mountains
• Volcanic Eruption
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The Geological Time ScaleThe Fossil Record – The Origin of Man
“Evolution vs. Creation”Precambrian – formation of the Earth and
appearance of simple life forms.Paleozoic – appearance of more complex life
forms .Mesozoic – appearance and extinction of
dinosaurs.Cenozoic – appearance of humans.
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Chapter 12
Soil Is The Living Component Of Earth’s Crust.
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WeatheringWeathering is the mechanical and/or chemical
breakdown of rocks.• Chemical
- Acid rain and ground water-Acid actions of organism (animals and plants)
• Mechanical– Ice/Frost Wedging– Plant roots Wedging– Animal Factor – pathways, burrow, …
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Erosion
Erosion is the process that loosens and moves weathered rock particles over the earth’s surface.
• Water in motion
• Meteorological processes (rain and wind)
• Geological processes (gravity and glaciers)
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Classifying Soil• Soil is a combination of eroded “rocks and
minerals”, “water”, “air”, and “organic material.”
• Humas is material made from breaking down plant And animal remains.
• Texture relates to how soil feels when robbed between fingers.
- Coarse-textured (sandy, gravel).- Medium-textured (loamy).- ne-textured (clay).
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Porosity and Permeability• Porosity
The amount of empty space in soil or a rock.
• PermeabilityThe measure of how easily liquids and gases pass through a soil or a rock
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