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DrDaveEarthSciCh2
Earth Science Chapter 2
| Question | Answer |
|---|---|
| model | a way of representing the properties of an object or system |
| sphere | a round object in 3-D space, like an orange |
| atmosphere | layer of gases that surround the earth |
| hydrosphere | the layer of liquid water on the surface of the earth |
| lithosphere | layer of rock that forms the outer shell of the surface of the earth, like the rind of a orange |
| Earth's interior | the region extending from the lithospere to the center of the earth, like the delicious part of the orange |
| field | region of space that has a meaurable value at every point |
| coordinate system | system of measurement used to locate points on a 2-D surface |
| latitude-longitude | the angular coordinate coordinate system for the earth's surface |
| latitude | the angular distance north or south of the equator |
| Polaris | is at 0 degrees altitude at the equator, 90 degrees altitude at the North Pole, which is the same number of degrees as the latitude |
| longitude | lines running from pole to pole which are the widest at the equator and touching at the poles |
| prime meridian | the half-circle of 0 degrees longitude in Greenwich, England (the other half circle on the other side of the earth is 180 degrees!) |
| longitude | the angular distance east or west of the prime meridian |
| lat_long direction identifier | uses N S E W to make the choice of direction for the number |
| hour | time it takes for the earth to turn 15 degrees |
| isolines | points of equal value that are connected to form a line on a map |
| isobars | lines of equal pressure |
| isotherms | lines of equal temperature |
| contours | line of equal elevation |
| elevation | height of a point above sea level |
| gradient | change in value divided by change in distance |
| topographic map | contour map |