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- The true shape of the earth is an oblate spheroid.
- The earth's true shape is most easily confirmed by photographs from space
- The earth appears to be perfectly round
- Compared with its size, the earth's surface appears to be smooth
- To determine the circumference of the earth, you need to measure the altitude of a star above the horizon from two or more locations
- The earth's equatorial circumference is slightly larger than its polar circumference
- The lithosphere is the earth's solid outer layer of rock
- The hydrosphere is the thin layer of water on the earth's surface
- The atmosphere is the thin shell of gases surrounding the earth
- The densest sphere is the lithosphere
- The least dense sphere is the atmosphere
- The thickest sphere is the lithosphere
- The thinnest sphere is the hydrosphere
- Over time, elevations represented on a topographic map change
- The building blocks of rocks are minerals
- Minerals are identified on the basis of well-defined physical and chemical properties
- Minerals are grouped into families according to their chemical composition
- The basic unit of most minerals is the silicon-oxygen tetrahedron (pyramid shape)
- The physical properties of minerals depends upon the arrangement and bonding of their atoms
- Rocks are classified on the basis of their origin (bow they formed)
- Igneous rocks form by the crystallization of molten magma or lava
- Crystal size in igneous rocks depends on rate of cooling
- Intrusive igneous rocks form slowly beneath the earth's surface
- Extrusive igneous rocks form quickly on the earth's surface
- Continents are granitic, Oceans are basaltic
- Sedimentary rocks form from sediments, evaporation of water, and organic remains
- Sedimentary rocks form at or near the surface of the earth
- Fossils are found almost exclusively in sedimentary rocks
- Metamorphic rocks form from other rocks by the action of beat and or pressure
- Contact metamorphism occurs when molten rock comes in contact with surrounding rocks
- Regional metamorphism occurs over large areas and is associated with mountain building
- Earthquakes and volcanoes occur in specific zones (ring of fire, mid atlantic) ·
- The speed of a seismic wave depends on the density of the material thru which it travels
- Richter and Mercalli measure the strength of an earthquake
- The Richter scale gives the power released
- The Mercalli scale gives the damage caused
- Plate tectonics the earth's crust is divided into pieces called plates which move
- The three types of plate boundaries are divergent (moving way, mid ocean ridge), convergent (coming together) and transform (sliding)
- Subduction is when one plate sinks under another forming a trench
- Weathering occurs when rocks are exposed to the hydrosphere, biosphere, and atmosphere
- Moist and warm climates favor chemical weathering
- Moist and cold climates favor physical weathering
- Weathering is slow in dry climates
- As particle size decreases surface area increases and the rate of weathering increases
- Soils develop as a result of weathering and biological activity
- The primary force that drives the agents of erosion is gravity
- The most important agent of erosion is running water
- The amount of stream erosion depends on the velocity of a stream and the volume of water
- Stream velocity depends on gradient and volume of water
- The outside of a meander bend is fast and erodes. The inside of a meander bend is slow and deposits
- As stream velocity increases, the size of the particles that can be transported increases
- Streams carry sediments by solution, suspension, bouncing and rolling
- The particles that settle out first are larger, most dense, and roundest
- Water and wind deposits are sorted by size and layered
- Gravity and glacial deposits are unsorted
- Arid landscapes are angular. Humid landscapes are smooth
- Glacial landscapes show U shaped valleys, depressions, irregular hills, scratched boulders
- In undisturbed sedimentary rocks, the bottom layer is the oldest
- Faults, folds, and intrusions are younger than the rocks they are found in
- Index fossils are found over a wide area and existed for a short period of time
- Geologic time is divided into units based on the fossil record
- An unconformity is a buried erosional surface
- Unconformities represent a gap in the geologic record
- Radioactive isotopes decay at a predictable rate known as half 1ife
- Carbon is used to date recent, organic remains
- Most life forms of the geologic past have become extinct
- As temperature increases, relative humidity decreases
- As altitude increases, air pressure decreases
- Wind is named for the direction it comes from
- The closer air temperature is to the dew point the greater the chance of precipitation
- Air in a low pressure area is warm and moist
- Air in a high pressure area ls cool and dry
- A rising barometer indicates good weather coming. A falling barometer indicates bad weather coming. A steady barometer indicates no change
- Fronts occur where air masses of different temperature and humidity meet
- The most likely areas for precipitation are the leading edges of air masses (fronts)
- The circulation in a low pressure system is counterclockwise, toward the center, where air rise. The circulation in a high pressure system is clockwise, away from the center, where air sinks.
- Weather systems in the U.S. usually move from west to east
- cT warm & dry. cP cool & dry. mT warm & moist. mP cool & moist
- Hurricanes form over warm oceans ln summer and autumn
- Tornadoes form in the spring where very different air masses collide
- Hurricanes lose strength as they move over land or cool water
- The earth rotates west to east, 15 degrees per hour, in 24 hours or in one day
- In the U.S. the sun appears to rise in the east, move through the southern sky and set in the west
- The earth revolves counterclockwise, 1 degree per day, in 365 ¼ days or one year
- As a planet gets closer to the sun the faster it orbits
- The earth’s orbit around the sun is nearly circular
- The moon revolves around the earth, in an elliptical orbit, in approximately one month
- The seasons are caused by the tilting of the earth’s axis and revolution around the sun
- The intensity of sunlight varies with the angle of the sun above the horizon
- The sun is most intense at an angle of 90 degrees
- Shadows get longer as the sun gets lower ln the sky
- Summer solstice: June 21.
- The sun rises north of east.
- The sun sets north of west.
- The sun reaches highest altitude of year.
- Vertical ray hits tropic of cancer.
- NY gets approx. 16 hours of daylight.
- North pole gets 24 hours daylight
- Winter solstice: December 21
- The sun rises south of east
- The sun sets south of west
- The sun reaches lowest altitude of year
- Vertical ray hits Tropic of Capricorn
- NY gets approx. 8 hours daylight
- North pole gets 0 hours daylight
- Equinoxes: Vernal March 21, Autumnal September 22
- The sun rises due east
- The sun sets due west
- Vertical ray hits equator
- The whole earth gets 12 hours daylight
- The equator always receives 12 hours of daylight
- The earth absorbs mostly short wavelength light energy. The earth reradiates mostly longer wavelength heat radiation
- Gases such as carbon dioxide prevent the escape of heat causing the greenhouse effect
- Marine climate cool summers, warm winters. Continental climate cold winters, hot summers
- Leeward side of a mountain dry & warm due to compression
- Windward side of a mountain cool & moist due to expansion
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