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Science Proficiency
Earth Science
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Earth
is between
4
and
5
billion years old
Earth science
is the name for all the sciences that collectively seek to understand earth and it's neighbors in
space.
Earth
Science
includes
geology
,
oceanography
,
meteorology
, and
astronomy
Geology
is the scientific study of the solid parts of the earth (landforms, rocks, minerals)
Oceanography
is the scientific study of oceans and their properties
Meteorology
is the scientific study of weather patterns and atmospheric conditions
Astronomy
is the scientific study of celestial objects such as stars, planets, moons, comets, asteroids, etc.
Law of Superposition
- younger layers are laid down on the older ones
The half-life of Uranium 237 is
4.5 billion
years
Fossils
are remains or traces of organisms preserved from past geologic ages
Sedimentary
rock forms when particles settle to form new rock
Paleontologists
are scientists who study
plant
and
animal
fossils
Igneous
rocks are formed by cooling magma or lava
Metamorphism
is the process that changes one type of rock into another without
melting
Minerals
are naturally occurring substances with definite chemical compositions and crystal structures
Amber
is the hardened resin formed by
coniferous
trees
Precambrian
era - all geologic time up to
600
million years ago
Paleozoic
-
ancient
life
Cenozoic
-
recent
life
Mesozoic
-
intermediate
life
Cenozoic
era are divided into
epochs
The earth's crust is composed of two types of rocks,
sedimentary
rock and
igneous
rock.
Epochs
are further subdivided into ages
Precambrian
rocks are
igneous
or
metamorphic
Igneous
rocks are formed from the solidification of molten material either below the surface (
intrusive
) or on the surface (
extrusive
)
Paleozoic era is divided into 7 periods:
•
Marine
invertebrates
•
Shells
•
Amphibians
•
Devonian Period
•
Marine life
•
Reptiles
Mesozoic
era - formation of several continents
Cenozoic
Era - mammals evolved
Mesozoic
- largest creatures existed during this era such as
dinosaurs
Pythagoras
- Greek philosopher and mathematician who thought that the earth had a
spherical
shape
Aristotle
- believed that the universe was composed of concentric spheres, with the earth at its center.
Eratosthenes
- Greek astronomer who made a measurement of the Earth's circumference
Isaac
Newton
- English mathematician and physicist who predicted that earth was not a perfect sphere
Henry Cavendish
- English scienctist, was the first one to determine the mass of the Earth
Latitude
Lines drawn east to west around the Earth, numbered from 0° at the equator to 90° at the North and South Poles
Longitude
North-south lines drawn from the North Pole to the South Pole, with the prime meridian at 0° passing through Greenwich, England
Longitudes
or
meridians
are not parallel, they are farthest apart at the equator and get closer together as they reach the poles where they meet</b>
International Date Line
The 180° meridian where east and west longitude lines meet, crossing this line going west adds one day
The
International Date Line
is directly opposite Greenwich on the other side of the Earth
Map
A drawing of the Earth, or part of the Earth, on a flat surface
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