earth history
DESCRIPTION
7th Grade Curriculum Earth HistoryTRANSCRIPT
EARTH HISTORY EARTH HISTORY Review
Created by Beverley SuttonPueblo Gardens PreK-8
Our Changing EarthOur Changing Earth
• Earth is a geologically active planet.
• Huge quantities of energy are always acting on the surface of the Earth and its interior.
• Observable evidence in the present gives information about processes and events that occurred in the past.
How Scientists work:Observation
How Scientists work:Observation
• Using one or more of the five senses
How Scientists work:Inference
How Scientists work:Inference
• Based on what you already know about footprints and the footprints you see …
What happened here?
Layers of the EarthLayers of the Earth
Let’s take them apart …Let’s take them apart …
… and look at them one by one … and look at them one by one
CrustCrust• The outermost “skin” of Earth. Two types:
Oceanic crust (thinner, mostly basalt) and Continental crust (thicker, mostly granite)
LithosphereLithosphere
• The crust and the uppermost part of the mantle – brittle and cool
LithosphereLithosphere
• Like the skin and a little of the white of an apple
MantleMantle
• Molten rock – between the crust and the core
CoreCore• Center of the Earth: Made up of mostly
iron and some nickel.• Outer core (liquid)• Inner Core (solid)
MineralMineral
• a crystalline inorganic solid that occurs naturally in the Earth’s crust.
PHYSICAL properties of mineralsPHYSICAL properties of minerals
RockRock
• inorganic solid that occurs naturally in the Earth’s crust.
Rock Cycle – a process that constantly recycles rock
Rock Cycle – a process that constantly recycles rock
Rock CycleRock Cycle
ErosionErosion• The wearing away of rocks by weather
(wind, water), or chemical means
SedimentsSediments
• small particles of sand, dirt, broken up rocks
Shale
Sedimentary RockSedimentary Rock• Formed by compaction and cementation.
Sediments are compacted (packed down) and glued together (cemented). Grains are in layers sandwiched between a muddy matrix
Limestone
Coal
Sandstone
Metamorphic RocksMetamorphic Rocks
• Rock that was once one type of rock but has changed to another under the influence of heat and pressure. Grains arranged in bands.
Marble – which was once limestone
Slate – which was once shale
Quartzite –which was once sandstone
Igneous RockIgneous Rock
• rocks that form from magma (melted, liquid rock) that cools and crystallizes. The crystals are randomly arranged and interlocking.
Pumice
Granite
Gabbro
Tectonic PlatesTectonic Plates
• Solid plates of lithosphere that float on the mantle
ConvectionConvection
• Convection -- Heat transfer in a gas or liquid by the circulation of currents from one region to another.
Divergent BoundaryDivergent Boundary
• At divergent boundaries new crust is created as plates pull away from each other.
Convergent BoundariesConvergent Boundaries
• Here crust is destroyed and recycled back into the interior of the Earth as one plate dives under another.
These are known as Subduction Zones - mountains and volcanoes are often found where plates converge.
Oceanic-Continental ConvergenceOceanic-Continental Convergence
Oceanic-Oceanic ConvergenceOceanic-Oceanic Convergence
Continental-Continental Convergence
Continental-Continental Convergence
Transform-Fault BoundariesTransform-Fault Boundaries
• Transform-Fault Boundaries are where two plates are sliding past one another.
These are also known as transform boundaries or more commonly as faults.
FaultFault• a crack in the earth's crust resulting from
the displacement of one side with respect to the other
Strike-slip Fault
Normal Fault
Law of SuperpositionLaw of Superposition• In a sequence of
layered rocks, a given bed must be older than any bed on top of it.
In other words, each layer is younger than those underneath it.
Law of Original HorizontalityLaw of Original Horizontality• Most sediments, when originally
formed, were laid down horizontally. In other words, most sediments settle in flat horizontal layers. If the layers are no longer horizontalthen somethinghappened to move them.
How landforms change
Seismologist Seismologist
• scientist who studies earthquakes
Seismograph Seismograph
• an instrument that records the magnitude (size) and duration (how long it lasted) of an earthquake.
Richter scaleRichter scale• the logarithmic scale used to measure
earthquakes.
Epicenter Epicenter
• The point of the earth's surface directly above the focus of an earthquake
Rock ColumnRock Column• A diagram that
shows the sequence of rocks in a particular area.
• Stratigraphy – the science of layered rocks.
Index fossilIndex fossil
• The fossil remains of an organism that lived in a particular geologic age, used to identify or date the rock or rock layer in which it is found. Also called guide fossil.
Our Changing EarthOur Changing Earth
• Earth is a geologically active planet.
• Huge quantities of energy are always acting on the surface of the Earth and its interior.
• Observable evidence in the present gives information about processes and events that occurred in the past.
Serene, still, and peaceful?Serene, still, and peaceful?
Wrong! A dynamic, always changing world!