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					The Nature of Science

  Earth & Space Science
   Chapter 1, Section 1
   The Scope of Earth Science
• The scope of Earth science is vast.
   – Dinosaur bones on display at museums were once
     embedded in the rocks that make up some of Earth’s
     cliffs and canyons.
   – Mining certain rocks produces some of the gold used
     by jewelers and dentists.
   – Computer models simulate the flow of the blanket of
     air that surrounds Earth so that scientists better
     understand stormy weather.
   – Ocean-floor exploration has led to the discovery of
     bizarre creatures that never see the light of day.
   – The study of objects in space has revealed much
     about our own planet.
   The Scope of Earth Science
• As you can see, there are many different
  areas of Earth science.
• This broad field can be broken into 4 major
  areas of specialization:
  – Astronomy
  – Meteorology
  – Geology
  – Oceanography
                        Astronomy
• Astronomy is the study of
  objects beyond Earth’s
  atmosphere.
• Prior to the invention of
  sophisticated instruments,
  such as the telescope,
  astronomers merely
  described the locations of
  objects in space in relation to
  one another. Today these
  scientists study the universe
  & everything in it, including
  Earth, its neighbors, & other
  bodes in the universe.
                    Meteorology
• The branch of Earth
  science that studies the air
  that surrounds our planet
  is called meteorology.
• Meteorologists study the
  forces & processes that
  cause the atmosphere to
  change to produce
  weather.
• They also try to predict the
  weather & how changes in
  weather might affect
  Earth’s climate.
Geology
    • The study of the materials
      that make up Earth & the
      processes that form &
      change these materials
    • Geologists identify rocks,
      study glacial movements,
      interpret clues to Earth’s
      history, & determine how
      forces change our planet,
      among many other things.
Oceanography
      • The study of Earth’s oceans,
        which cover nearly ¾ of the
        planet
      • Oceanographers study the
        creatures that inhabit salty
        water, measure physical
        properties & observe the
        processes of oceans
      • Some oceanographers study
        the effects of human
        activities on the oceans.
   The Scope of Earth Science
• The study of our planet requires a vast
  amount of knowledge and the study of
  many different things.
• There are many subspecialties of the 4
  major areas of Earth Science
           Climatology
    Subspecialty of Meteorology
• A climatologist studies patterns of weather
  over a long period of time and the effects
  of human activities on weather and
  climate.
           Paleontology
       Subspecialty of Geology
• Paleontologists study the remains of
  organisms that once lived on Earth.
• Paleontologists also study ancient
  environments.
             Hydrology
       Subspecialty of Geology
• Hydrologists study water flow on and
  below Earth’s surface.
• Also interested in the sources of water and
  solutions to water pollution.
             Ecology
       Subspecialty of Biology
• Ecologists study the habitats of organisms
  and how organism interact with each other
  and their environments.
          Geochemistry
     Subspecialty of Geology &
           Chemistry
• Geochemists study Earth’s composition
  and the processes that change it.
                Tectonics
           Specialty of Geology
• A scientist that studies tectonics would also be
  called a geologist. He/she would be more
  knowledgeable in the area of plate tectonics
  than a ―regular‖ geologist.
• These scientists
  study the effects of
  earthquakes, &
  mountain building.
           Earth’s Systems
• Scientists who study Earth have identified
  4 main Earth systems:
  – Lithosphere
  – Hydrosphere
  – Atmosphere
  – Biosphere
• Each system is unique, yet each interacts
  with the others. None of Earth’s systems
  is independent of the others, nor of the
  global system of Earth itself.
The Lithosphere
        • Earth’s lithosphere is
          rigid outer shell and
          includes the crust & the
          solid, uppermost part of
          the layer below the crust,
          the mantle.
        • There are 2 kinds of
          crust: continental crust
          and oceanic crust.
The Lithosphere
        • Earth’s continental crust
          is made mostly of a rock
          called granite.
        • Oceanic crust is mainly
          basalt, a rock that is
          denser than granite.
        • Earth’s mantle is mainly
          composed of a rock
          called peridotite.
The Lithosphere
        • Some of Earth’s upper
          mantle behaves like a
          rigid solid while other
          parts of this layer are
          partially molten and flow
          like a soft plastic.
        • This partially molten
          layer is called the
          asthenosphere.
The Lithosphere
        • Beneath Earth’s mantle is
          the core, which can be
          divided into 2 parts: an outer,
          liquid part & a solid, inner
          part.
        • Earth’s core is thought to be
          made of iron & nickel.
        • While Earth’s core &
          asthenosphere are not parts
          of the lithosphere, they do
          interact with this system of
          Earth to produce many of the
          features at the planet’s
          surface.
            The Hydrosphere
• The water in Earth’s oceans, seas, lakes, rivers
  & glaciers, as well as the water in the
  atmosphere, makes up the hydrosphere.
• About 97% of Earth’s water exists as salt water.
  The other 3% is freshwater contained in glaciers,
  lakes & rivers, and beneath Earth’s surface as
  groundwater.
• About ¾ of all freshwater is contained in glaciers
  and icebergs.
• The rest of freshwater is mainly groundwater.
• Only a fraction of Earth’s total amount of
  freshwater is in lakes & streams.
            The Atmosphere
• The blanket of gases that surrounds our planet
  is called the atmosphere.
• Among other things, Earth’s atmosphere is
  necessary for respiration by most living things,
  protects Earth’s inhabitants from harmful
  radiation from the Sun, and helps to keep the
  planet at a stable temperature.
• Earth’s atmosphere contains about 78%
  nitrogen and 21% oxygen. The remaining 1% of
  gases in the atmosphere include water vapor,
  argon, carbon dioxide, and other trace gases.
             The Biosphere
• The biosphere includes all organisms on Earth
  as well as the environments in which they live.
• Most organisms exist within a few meters of
  Earth’s surface, but some live deep beneath the
  ocean’s surface, and others live high atop
  Earth’s mountains.
• Earth’s biosphere is unique in that scientists
  have not found any confirmed evidence of life on
  other planets or elsewhere in the galaxy.
             The Biosphere
• Earth’s biosphere, lithosphere,
  hydrosphere and atmosphere are
  interdependent systems.
• Earth’s present atmosphere formed
  millions of years ago as a result of
  volcanic activity, respiration and
  transpiration by ancient organisms &
  photosynthesis.
• Today’s organisms, including humans,
  continue to change the atmosphere
  through their life processes and activities.
  Earth Science in Your Everyday
               Life
• You and the billions of other life forms that
  live on Earth are part of the biosphere.
• Together with many of these creatures,
  you live on Earth’s crust, which is part of
  the lithosphere, and breathe the gases in
  Earth’s atmosphere.
• You also depend in many ways on the
  substance that covers nearly ¾ of Earth—
  water, which makes up the hydrosphere.
                 Technology
• While you might not realize it, the study of
  science, including Earth science, has led to the
  discovery of many things that you use every day.
• This application of scientific discoveries is called
  technology.
• Freeze-dried foods, ski goggles, micro-fabrics,
  and the ultra-light materials used to make many
  pieces of sports equipment are just a few
  examples of technological advances developed
  as a result of scientific study.
Mapping Our World

 Earth & Space Science
  Chapter 2, Section 1
        Latitude & Longitude
• For thousands of years people have used
  maps. We still rely on maps for a variety
  of purposes.
• The science of mapmaking is called
  cartography.
• Cartographers use an imaginary grid of
  parallel lines and vertical lines to locate
  points on Earth exactly.
• In this grid, the equator separates Earth
  into two equal halves called the northern
  hemisphere and the southern hemisphere.
                   Latitude
• Lines running parallel to the equator are called
  lines of latitude
• Latitude is the distance in degrees north or
  south of the equator.
• The equator, which serves as the reference
  point for latitude, is numbered 0° latitude.
• The poles are each numbered 90° latitude.
• Latitude is thus measured from 0° at the equator
  to 90° at the poles.
• Locations north of the equator are referred to by
  degrees north latitude (N). Locations south of
  the equator are referred to by degrees south
  latitude (S).
Latitude
    • Syracuse, New York
      is located at 43° north
      latitude (43°N).
Latitude
    • Christchurch, New
      Zealand is located at
      43° south latitude
      (43°S).
                 Longitude
• To locate positions in east and west directions,
  cartographers use lines of longitude (also known
  as meridians).
• Longitude is the distance in degrees east or
  west of the prime meridian, which is the
  reference point for longitude.
• The prime meridian represents 0° longitude.
• In 1884, astronomers decided that the prime
  meridian should go through Greenwich,
  England, home of the Royal Navy Observatory.
• Points west of the prime meridian are numbered
  from 0° to 180° west longitude (W); points east
  of the prime meridian are numbered from 0° to
  180° east longitude (E).
 Locating Places with Coordinates
• Both latitude and longitude are needed to
  precisely locate positions on Earth.
• For example, it is not sufficient to say that
  New Orleans, Louisiana, is located at
  29°N latitude. That measurement includes
  any place on Earth located along that line
  of latitude.
• New Orleans, LA is located at 29°N 90°W.

				
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posted:10/14/2011
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