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Steps of the Scientific Method
Ask a Question
Do Background Research
Construct a Hypothesis
Test Your Hypothesis by Doing an Experiment
Analyze Your Data and Draw a Conclusion
Communicate Your Results
Percent ocean coverage of Earth
71%
Compare ionic and covalent bonds
- Ionic: electrical charges hold two atoms together due to a gain or loss of one or more electrons (transfer/exchange)
- Covalent: two atoms share one or more pairs of outer shell electrons (share)
5 characteristics used to classify a mineral
- natural
- inorganic
- solid
- posses an orderly internal structure of atoms
- definite chemical composition
Methods to identify minerals
- luster
- color
- streak
- ability to transmit light
The most common mineral group in earth's crust
Feldspar
renewable resources
corn, wind, & water
Non-renewable resources
oil, aluminum, natural gas, & coal
Describe the rock cycle
rocks are broken into sediments... sediments are compacted and form rocks... changed heat, pressure or fluids... magma forms when rock melts beneath surface.. magma cools and forms igneous
What are the 3 types of rocks?
igneous, sedimentary, metamorphic
igneous rocks
formed when magma cools beneath Earth's surface or when lava cools at Earth's surface; forms in or around volcanoes; requires heat (no gas)
sedimentary rock
- A type of rock that forms when particles from other rocks or the remains of plants and animals are pressed and cemented together (75% of the continent)
- used to reconstruct earth's history
metamorphic rock
A type of rock that forms from an existing rock that is changed by heat, pressure, or chemical reactions.
magma and lava difference
- magma has no gas and is underneath the earth's crust
- lava has gas and is above earth's crust
- both molten
early evidence for one continentnt
- fits of South America and Africa
- fossils match across seas
- rock types and structures match
- ancient climates
lithosphere and asthenosphere differences
Lithosphere:
- strong
- formed from the crust/uppermost mantle
- varies in thickness/density
Asthenosphere
- hotter
- the weaker region in the mantle
- solid but never melting temperature
- "flowy" consistency
The 3 types of plate boundaries
Divergent, Convergent, and Transform
divergent boundary
The boundary between two tectonic plates that are moving away from each other
convergent boundary
A tectonic plate boundary where two plates collide, come together, or crash into each other.
transform boundary
A plate boundary where two plates move past each other in opposite directions
3 type of seismic waves
Primary (P) Waves, Secondary (S) Waves, and Surface Waves
Primary Waves (P-Waves)
compression waves that travel through solids and liquids, compressing and expanding the material they pass through, temporarily changing volume
(greatest velocity of all waves)
Secondary Waves (S Waves)
only travel through solids and temporarily change the shape, but not the volume of the material they pass through; move slower than P waves
surface waves
a type of seismic wave that forms when P waves and S waves reach Earth's surface
(slowest velocity of all waves)
Destruction caused by earthquakes
- landslides/ ground subsidence
- fires
- tsunami (bc of displacement of floor)
Preventions of destruction caused by earthquakes
- Earthquake-resistant structures
- tsunami & earthquake warning systems
3 major types of volcanoes
shield, composite, cinder cone
Cinder volcano characteristics
1. largest
2. almost exclusively basalt
3. broad (slight dome shape)
5. mild eruptions- large volumes of lava
6. most begin on the ocean floor
composite volcano
1. built from ejected basaltic lava (mainly cinder sized) fragments
2. small size
3. frequently occur in groups
Shield volcano
1. thousands of feet high
2. several miles wide
3. composed of interbedded lava flows
4. violent eruptions
5. most adjacent to pacific ocean
materials that are ejected during volcanic eruptions
ash/dust, pumice, lapilli, cinders, blocks, bombs, (in form of hot lava)
Ring of Fire
region having the greatest concentration of composite volcanoes
catastrophism
- landscape developed by catastrophes
- James Usher (mid 1600s) concluded earth was only a few thousand years old
Uniformitarianism
James Hutton: the idea that the Earth's natural processes have operated in the same way throughout history
In what ways can an animal or plant be preserved as a fossil
frozen, dry caves, fine-grained sediment, three-dimensional detail, and sticky resin
fossil succession
The principle that the assemblage of fossil species in a given sequence of sedimentary strata differs from that found in older sequences or in younger sequences. a given species appears at a certain level and then disappears (goes extinct) at a higher level
3 types of particles emitted in radioactive decay
alpha, beta, and electron capture
alpha particle
A cluster of 2 protons and 2 neutrons emitted from a nucleus in one type of radioactivity
beta particle
a high-speed electron with a 1- charge that is emitted during radioactive decay
electron capture
the process in which an inner orbital electron is captured by the nucleus of the atom that contains the electron
4 basic units that makeup geologic time
eon: one billion years long
era: hundreds of millions of years
period: tens of millions of years
epoch: tens of millions of years
Cambrain explosion
earliest part of the Paleozoic era, when a huge diversity of animal species evolved
(541 million years ago)
ex): jellyfish, worms, and mullusks
extra credit: Big Bang Theory
- 13.7 billion years ago
- heavier elements created in stars
- universe started to expand from one spot
- hydrogen + helium formed shortly after Big Bang
- supernova event stars exploded and creates heaviest elements
extra credit: Earth Formation
- planetesimals to protoplanets
- solar system = solar nebula
- rotating cloud of gas and substances around the protosun
- remained debris formed a flattered disk
extra credit: Life/Animal Evolution
- prokaryotes + eukaryotes
- single celled bacteria
- DNA segregated from nucleous
- complex multicellular
- dinosaurs to reptiles and birds