Title: Geology
1Geology
2Layers of the Earth
- Inside the earth this dynamic earth, USGS
- Read this page from the US geological survey and
fill in pages 1 and 2 in your student guide
3How Do We Know?
NOT by drilling holes! (Not that we dont
try) We map the structure of Earth by measuring
seismic waves.
- Holes
- Mohole project
- Ocean drilling program
- Digging from China
4Seismic Wave Pattern
- Patterns of earthquake (seismic) waves as they
arrive at seismograph stations worldwide - P-waves (primary)
- Propagate through solids and liquids, but change
speeds - S-waves (secondary)
- Propagate through solids but not liquids
5Seismic Wave Types
6Mapping Inner Earth
7Review
- T or F In 1999, with NSF funding, a hole was
drilled into the mantle. - T or F Scientists have mapped the interior of
Earth by taking core samples. - Which type of seismic wave dies out when it hits
a liquid boundary? - Give 3 characteristics of a P-wave.
- Give 3 characteristics of an S-wave.
8Field Guide to Rocks and Minerals
- Are rocks and minerals the same thing?
9What Is A Mineral?
- A mineral is a naturally occurring inorganic
solid with definite chemical composition and
crystal structure. - Gypsum CaSO4.2H20.
- A minerals appearance will depend on the
conditions under which it was formed.
10Another Mineral
CaCO3
Limestone
Marble
Calcite
Aragonite
11What Is a Rock?
- A rock is a mixture of minerals
12Types of Rock
- Sedimentary
- Igneous
- Metamorphic
13Sedimentary Rock
14Types Of Sedimentary Rock
- Clastic (cemented) sediments
- 1. Weathering (breaking down) rocks into small
particles - 2. Deposition (laying down) of these particles
- 3. Cementation (consolidation, glue)
- Chemical sediments
- Organic sediments
15Clastic Sediments
- Shales
- Fine grained particles of clay
- Deposited in deep water
- Sandstones
- Larger grained sand particles
- Deposited near shores
- Conglomerates
- Pebbles, large sand grains
Western Kansas
16Organic Sediments
- Limestone
- Consists mainly of animal shells left on ocean
floors, lake bottoms or river beds - Type of limestone depends on minerals in the
water where it was formed - Coal
- Decomposed vegetable matter
17Kansas City Rock Layers
18Chemical Sediments
- Weathered mineral-bearing rock dissolved in water
- Gypsum
- Salt
- Chert
Flint Hills Chert, Limestone
Salt mine Hutchinson, KS
19Student Activity
- Write three examples of sedimentary rock
Castle Rock, Western Kansas (chalk formation)
20Igneous Rock
21Igneous Rocks
- Rocks which form directly from the cooling of
magma - Igneous rock can form deep in the earth, on the
surface of the earth or in the air - The rate of cooling determines the crystal
structure of the rock
22Basalt
- Very common fine-grained volcanic rock
- Rapid cooling forms fine-grained crystal
structure - Basalt is made of the minerals
- Feldspar
- Pyroxene
- Olivine
- Magnetite
- Remember rock is a mixture of minerals!
Devils Tower, Wyoming
23Granite
- Large individual crystals form when the rock
cooled slowly, allowing time for crystal
formation - Granite consists mostly of the minerals
- Quartz
- Feldspar
- Mica
24Pumice
- Magma that cools very quickly in air
- Ejected in pyroclastic flows
- Very fine-grained
- Gas trapped inside
-
25Common Elements in Igneous Rock
- Magma is rock soup composed of the same elements
that make up the crust and mantle of earth - Oxygen, Silicon, Aluminum, Iron, Magnesium,
Calcium, Sodium and Potassium - Small quantities of rarer elements
- These elements combine differently to make
various minerals quartz, feldspar, mica,
amphibole, pyroxene and olivine. - The minerals formed from the magma soup depend on
where and how it is cooled.
26Student Activity
- Write three examples of igneous rocks
27Metamorphic Rock
28Metamorphic Rock
- Formed from igneous or sedimentary rock
- Heat
- Pressure
- Hot mineral solution
- Mineral composition changes
- Limestones gt marble
- Shales gt slate gt schist gt gneiss
- Sandstones gt quartzite
29Progression of Metamorphic Rock
Temperature and Pressure
30Student Guide Activity
- Write two examples of metamorphic rock
- Include the original and the product
marble
31Rock ProcessesWeatheringErosionDeposition
32Weathering, Erosion, Deposition
These three processes form all of the landscape
we have around us.
33Chemical Weathering
- Rainwater combines with CO2 in the atmosphere to
form a weak acid - Limestone layers are dissolved and deposited in
caverns
Lewis Clark Caverns, Missouri
34Mechanical Weathering
- Wind carrying sand particles
- Water freezing/thawing in rock crevices
- Streams carrying abrasive particles, flooding
Concretions Western Kansas
35Biological Weathering
- Lichens
- Plant and tree roots
- Animal burrowing
36Erosion
- The process of moving weathered material from one
location to another - Water
- Wind
- Ice
Red Hills, Western Kansas
37Continental Glaciers
- Ice age continental glaciers scraped and ground
surface rocks - Created rolling hills and valleys, deposited
glacial debris
Glacial Debris, Northwest Kansas
38Alpine Glaciers
- Smaller, year-round streams of ice
- Wears down upper mountain material and carries it
downward into streams and valleys
39Erosion by Water
- Sediment carried by rains into streams
- Fast flowing water scours stream banks
- As the water slows, sediment settles
- Heavy particles first
- Silt and small particles last
40Deposition
- Sediments are deposited where
- Winds die down or are blocked
- Water slows down
- River bends
- Seas
- Glaciers stop or begin to melt
41The End