Mapping Earth Review Note Cards

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Transcription:

Review Note Cards

Spheres of Earth Atmosphere- Layer of gases Hydrosphere- All liquid water Lithosphere- Solid surface Biosphere-Living Portion Cryosphere-Ice Portion

Evidence that the Earth is Round The Sinking Ship Lunar Eclipses Sun and Star Path Across Sky Altitude of Polaris Photos from space (best evidence)

Model of Earth Apparent Shape of the Earth The best model of the Earth is a perfect sphere (pool ball, ping-pong ball)-round and smooth Scale Model Drawn to Scale

Oblate Spheroid The ACTUAL shape of the Earth True Shape of the Earth Slightly flattened at the Poles Slightly bulging at the Equator Caused by Rotation of Earth

Gravity Measurements If Perfect Sphere-Same Weight Weigh more at Poles Closer to the Center of Planet Weigh less at Equator Farther away from Center

Latitude A measure of how far north or south of the equator you are Equal to the altitude of Polaris (in the Northern hemisphere) FLAT-ITUDE Equator = 0 N.Pole = 90 N S.Pole = 90 S

Determining Latitude ALTITUDE of POLARIS = LATITUDE Only true in the northern hemisphere This angle is equal to your latitude

Longitude A measure of how far east or west of the Prime Meridian you are LONG-itude Prime Meridian = 0 International Dateline = 180 Locations on the same longitude share the same solar time

Longitude Each time zone is 15 degrees apart Earth rotates 15 degrees per hour U.S. has 4 major time zones Travel vertically through zone, time does not change Travel horizontally from one time zone to the next, time changes

Determining Longitude You MUST know the following: The time where you are The time at the Prime Meridian Find the difference between the time where you are and the time at the Prime Meridian Multiply it by 15 /hr (this gives you your longitude) If your time is less, you are west If your time did increase, you are east

Fields Region of Space A map displaying pressure, temperature or elevation data

Drawing Isolines Lines can never intersect Either complete circles OR run off the edge of the map Separate higher values from lower values

Interval (Contour Interval) The difference in value between two adjacent isolines Difference is an equal interval...by 4 s, 10 s, 100 s

Isolines Iso = Same Lines that connect points of equal elevation, pressure or temperature

Contour Lines Lines that connect points of equal elevation Index Contour Lines show distinct elevations Darker in Color

Isotherms Lines that connect points of equal air temperature

Isobars Lines that connect points of equal air pressure

Contour Map (topographic map) Map that shows the 3-d landscape of an area (mountains, valleys, etc)

Gradient Page 1 in ESRT G = Change in Field Value Distance

Steepest Slope?? Where the contour lines are closest together Also known as the steepest gradient

Stream flow direction? Streams flow OPPOSITE where the v s are pointing Streams ALWAYS flow downhill (high elevation to low elevation) Streams flow out of the V

Highest Elevation? First, find the highest contour line on the map... Highest possible elevation is one value less than next contour line

Lowest Elevation? First, find the lowest contour line on the map... Lowest possible elevation is one value greater than next contour line

Depressions Crater or hole in the ground Look for Hachure Lines

Profile A side view, or cross-section, of a landscape Use scrap paper to record the elevations of the contour lines crossing the profile line Transfer those markings to a graph to draw the profile PRACTICE THIS!!!!