I. Our Dynamic Earth: It's Systems and Formation
Earth - our home - is a unique and beautiful
entity. It is also a complex entity because it is not static.
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It is a dynamic place with many interacting parts that form a complex and
continuously interacting whole - "Earth System".
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a change in one part of the Earth System can produce changes in one or
any of all of the other parts.
A. The Earth's Subsystems (Spheres):
Earth's Subsystems (Four
Spheres)
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biotic - living; abiotic - nonliving; all four spheres
are interconnected
(1) Atmosphere - a thin layer of gases (below 480 km) surrounding
the Earth, and held to the Earth by gravity; it forms a protective boundary
between outer space and the biosphere
(2) Hydrosphere - an abiotic open system that includes all of
the Earth's waters (surface, atmosphere, & crustal; & gaseous,
solid, & liquid)
(3) Lithosphere - the Earth's crust and that portion of the upper
mantle directly below the crust that extends downward to 70 kilometers
(km) (45 miles)
(4) Biosphere (ecosphere) - that area where the atmosphere, hydrosphere,
and lithosphere function together to form the context within which life
exists.
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it is an interconnected web that links all organisms with their physical
environment
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just as the other three spheres impact and shape life, life itself impacts
and shapes the other three spheres
C. Scientific Inquiry (The Scientific Method)
(1). The Goal of Science
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The job of the scientist is to learn about the natural world that surrounds
them; to attempt to discover how and why it works the way it does.
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This task is made easier because the universe is a regular and predictable
place.
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It is the job of the scientist to discern the predictable patterns, and
discover the "simple laws" that are responsible for them.
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Science thus operates under the following assumption: natural laws that
control our universe exist, and can be understood by the human mind.
(2). How Our Present Way of Conducting Science Came to Be
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The first science was astronomy. It came about out of a practical need
for a reliable calender that could be used to assist farmers.
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In the early 17th century, men like Galileo first began to make careful
and systematic observations of natural phenomenon and to try explaining
them.
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Galileo made many careful measurements.
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He and some of his contemporaries introduced the concept that a theory
was valid only insofar as it predicted and explained the observations on
which it was based.
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They thus established a close connection between observations and
theory,
which is the essence of the scientific method (scientific inquiry).
(3). The Scientific Method
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The term scientific method refers to the principles and processes
that guide scientific investigation.
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It provides the framework within which scientists try to discover the laws
governing the natural (observable) world.
Steps Involved in the Scientific Method:
1) Observation
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A scientist begins by making an observation about some system.
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It can involve the making of measurements of the properties of the system
that is being observed.
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These measurements can range, for example, from finding the size of some
object, to finding the length of time it takes for some process to occur.
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An important characteristic of measurement is that its accuracy is always
limited: in part from inaccuracies inherent in any measuring device.
2) The Hypothesis/Theory
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The scientist then comes up with a hypothesis to answer his/her question
and explain his/her observations.
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After a hypothesis has been formulated, it must be tested. It must
predict the observations; if it doesn't, it must be discarded and another
found.
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In order for a hypothesis to be considered valid, it must be (experimentally)
verified. (One way of testing a hypothesis is to conduct a controlled
experiment).
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If a hypothesis has survived extensive scrutiny, and competing hypotheses
have been eliminated, a hypothesis is elevated to the status of a scientific
theory.
3) The Scientific Law
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After a theory has survived many years of experimental investigation, it
is frequently accorded the status of a scientific law.
Summary: The Scientific Method
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Observation
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Hypothesis/Theory
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Testing (perhaps via a controlled experiment)
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Law
D. Our Galaxy (the "Milky Way") and Solar System
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Our sun & solar system is within the Milky Way Galaxy - just
one of millions within the universe
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Our sun is just one of billions within the Milky Way Galaxy
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The Milky Way Galaxy is a "Spiral Galaxy", and we are located far
out from the center of the galaxy on one of the spiral arms - the "Orion
Arm"
Structure of the Milky Way Galaxy
(1) Galactic Dimensions
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speed of light: 299,792 km/sec
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at this speed, the distance that light can travel in one year is
more than 9 trillion km
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this distance is called a "light year"
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we use the "light year" as a distance unit
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1 light year = 9,454,000,000,000 km
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our moon = 1.28 seconds away in light speed
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our solar system's diameter = 11 hours in light speed
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our entire galaxy ~ 100,000 light years
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the entire known universe ~ 12 billion light years
(2) Formation of our Solar System: "nebula
hypothesis"
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our solar system formed from a rotating, cloud of gas, dust,and ice - a
"nebula" (4.6 billion years ago)
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a proto-Sun formed at the center of the nebula where the most mass
existed
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the rotating cloud of gas and dust flattened out an assumed a disk shape
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mass accumulated by "accretion" away from the center of the nebula - protoplanets
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the protoplanets grew in size - "planetesimals"
as the proto-Sun grew in size it became hotter due to intense pressures;
and eventually thermonuclear reactions within the sun occurred - fusion
- the conversion of hydrogen to helium - which releases tremendous amounts
of energy
Nebular Hypothesis
(3) Our Solar System
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Is comprised of nine planets: Mercury, Venus, Earth, Mars [the terrestrial
(Earth-like) planets]; and Jupiter, Saturn, Uranus, Neptune [the Jovian
(Jupiter-like) planets], and Pluto.
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The terrestrial, or inner planets, are small, dense (5 times that
of water), rocky, and metalic, with minor amounts of gases (i.o.w., a meager
atmosphere).
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The Jovian, or outer planets, are large, not very dense (only 1.5
times that of water), and contain a large percentage of gases (i.o.w.,
a thick atmosphere -- of mainly hydrogen and helium).
Orbits and Relative Positions
of the Planets
Relative Sizes of the Planets