Layers
near the surface of the Earth (lithosphere, hydrosphere, biosphere, atmosphere)
What do the 4
prefixes mean? (litho-rock hydro-water bio-life atmos-air)
Rock cycle: how to read the rock cycle diagram
Rock cycle: how to read the rock cycle diagram
Describe two ways a
sedimentary rock can form. an igneous rock weathers into sediment, erodes away, settles somewhere else, then is cemented and compacted into a sedimentary rock
Explain what turns an
igneous rock into a metamorphic rock. heat and pressure
What are sediments? broken bits of rock that have been weathered
Formation of types of rocks (sedimentary, igneous, metamorphic)
Formation of types of rocks (sedimentary, igneous, metamorphic)
Explain how each type
of rock is formed.
sedimentary: broken bits of rocks are pressed together and glued by minerals or other bits of rock
metamorphic: existing rocks are squeezed and heated, melting partially and morphing (changing) formigneous: magma or lava cools, hardening into rock
What do sedimentary
rocks contain that other types of rock do not? fossils
Properties of minerals: cleavage/fracture, luster, hardness, color, streak
Properties of minerals: cleavage/fracture, luster, hardness, color, streak
Identify a mineral
that has a green streak. pyrite
Identify a mineral
that has cubic cleavage and tastes salty. halite
What properties would
you need to observe to identify a mineral as calcite? bubbling with acid
Erosion – transportation of sediment after it is broken down by weathering
Erosion – transportation of sediment after it is broken down by weathering
The forces that carry
sediment (4 forces; 3 of them were demonstrated by sand in class) water, wind, glaciers, and gravity
Weathering (chemical and mechanical)
Weathering (chemical and mechanical)
Explain how a pothole
is formed. A pothole is formed by ice wedging, which means that water seeps into a crack, then freezes and expands, wedging the rock apart.
Is the formation of a
pothole mechanical or chemical weathering? physical
What is chemical
weathering? Chemical weathering is the breaking down of rocks where the composition of the rock is changed in the process. This is different from physical weathering because physical weathering just makes rocks into smaller rocks.
Where fossils are found
Where fossils are found
In which type of rock
are fossils mostly found? Sedimentary
Relative ages of rocks
Relative ages of rocks
How does the age of
fossils in the bottom layer of sedimentary rocks compare to the ages of fossils
in the top layer? The bottom layer is older than the top layer.
What the fossil record tells us
What the fossil record tells us
What can scientists
infer by studying fossils of organisms that lived long ago? Scientists can infer what the characteristics of the climates and environments were.
Theory of Plate Tectonics
Theory of Plate Tectonics
Alfred Wegener’s
hypothesis: The continents used to be connected and then have slowly moved apart to their current locations.
What fossils show
about continental drift: Fossils of some plants and animals can be found on more than one continent, showing that the continents used to be connected.
Convection Currents – movement that is created in a fluid when it is heated unevenly
Convection Currents – movement that is created in a fluid when it is heated unevenly
Draw two convection
currents in the mantle that are helping tectonic plates move.
Why one plate sinks under the other at a subduction zone
Why one plate sinks under the other at a subduction zone
Draw a picture of one
plate subducting under the other.
Label the plate that
is more dense. The more dense plate is sinking under the continental plate.
Seafloor spreading
Who is Harry
Hess? What did he do to provide evidence
for Wegener’s hypothesis?
Harry Hess used sonar to map the ocean floor. He showed that there were ridges (mountains) and volcanoes on the seafloor, which provided evidence that new rock material was being created at the ridges, pushing the continents apart.
Measuring mass with a triple beam balance
Measuring mass with a triple beam balance
Be able to measure
mass to the nearest tenth of a gram.
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