front 1 Steady state theory | back 1 neither a beginning nor an end to the universe (matter is constantly destroyed and remade) |
front 2 Contraction-expansion theory | back 2 someday, the universe will contract and expand again |
front 3 light year | back 3 the distance light travels in one year |
front 4 stars are made of - | back 4 hydrogen and helium |
front 5 stars have a - | back 5 finite life span |
front 6 the mass of a star controls its - | back 6 evolution |
front 7 hydrogen - | back 7 burns first |
front 8 helium - | back 8 burns last |
front 9 parallex | back 9 used to measure the distance of stars from earth |
front 10 hydrogen to helium - | back 10 fusion |
front 11 helium to hydrogen - | back 11 fission |
front 12 polaris - | back 12 North star |
front 13 alpha centaur - | back 13 closest star to Earth |
front 14 Nebula - | back 14 dust and gases |
front 15 bright stars - | back 15 top |
front 16 dim stars - | back 16 bottom |
front 17 red shift | back 17 stars moving away |
front 18 blue shift | back 18 stars moving towards |
front 19 sun - | back 19 main sequence star; 70% hydrogen, 28% helium |
front 20 apparent magnitude - | back 20 brightness from earth |
front 21 Absolute magnitude - | back 21 brightness if all stars were the same distance |
front 22 star nebula theory | back 22 the solar system condensed from a cloud of dust and gas |
front 23 asteroid belt is located between - | back 23 Mars and Jupiter |
front 24 Comets | back 24 tail always pointed away from the sun |
front 25 Kuiper belt | back 25 beyond Neptune where comets originate |
front 26 Meteoroid | back 26 small, solid particle |
front 27 Meteor | back 27 streaks of light produced by a solid particle |
front 28 Meteorite | back 28 a meteoroid that passes through earth's atmosphere and hits earth's surface |
front 29 Inner planets - | back 29 Mercury, Venus, Earth and Mars |
front 30 Outer planets - | back 30 Jupiter, Saturn, Uranus ans Neptune |
front 31 Trophosphere - | back 31 layer closest to the ground; temperature drops with altitude; contains all weather |
front 32 Stratosphere - | back 32 three layer oxygen atoms bonded together; protect earth from ultra violet radiation |
front 33 Mesosphere - | back 33 temperature decreases with altitude; meteors burn up |
front 34 Thermosphere - | back 34 largest and outermost layer; contains isosphere( bounces radio waves back to earth |
front 35 Stage 1 of the atmosphere - | back 35 mostly hydrogen and helium; earth's surface was molten; no oxygen present |
front 36 Stage 2 of the atmosphere - | back 36 formation of moon occurs; volcanoes result in carbon; oceans form, carbon dioxide leaves the atmosphere |
front 37 Photosynthesis - | back 37 cynobacteria consumed carbon dioxide and released oxygen |
front 38 Modern atmosphere - | back 38 1% trace gas; 21% oxygen; 78% nitrogen |
front 39 Insolation - | back 39 the amount of solar radiation reaching a given area |
front 40 ITCZ - | back 40 inter-tropical convergence zone; influenced by the sun's radiation; warm air rises |
front 41 STHP - | back 41 sub-tropical high pressure belt; influences the distribution of deserts; cold air sinking |
front 42 SPLP | back 42 sub-polar low pressure belt; warm air rises |
front 43 PH - | back 43 polar high; high to low always |
front 44 Wind flow - | back 44 forces that drive surface winds |
front 45 Coriolis force - | back 45 the influence of the earth's rotation |
front 46 cP | back 46 dry and cold |
front 47 mP | back 47 moist and cold |
front 48 mT | back 48 moist and warm |
front 49 cT | back 49 dry and warm |
front 50 warm front - | back 50 warm air; low pressure system; brings rain |
front 51 cold front - | back 51 cold air sinking; high pressure system; good weather |
front 52 stationary front - | back 52 slow moving |
front 53 occluded front - | back 53 balance each other out ( warm and cold front) |
front 54 dry line - | back 54 dry air |
front 55 cyclone - | back 55 low pressure; tropical storm; counter clockwise; warm air rises |
front 56 anti-cyclone - | back 56 high pressure; clear weather; clockwise; cooling air |
front 57 sling psychrometer - | back 57 measures relative humidity |
front 58 anemometer - | back 58 wind speed |
front 59 ocean uses - | back 59 fresh water. petroleum, minerals, food |
front 60 sea ice formation - | back 60 needle-like crystals become slush |
front 61 iceberg formation - | back 61 icebergs break off of glaciers |
front 62 shelf ice - | back 62 plate-like icebergs |
front 63 wind power - | back 63 uneven solar heating generates winds |
front 64 surface currents - | back 64 wind driven; primarily horizontal |
front 65 deep currents - | back 65 differences in density caused by differences in temperature and salinity |
front 66 Eutrophication - | back 66 fertilizer carried by run-off causes algae blooms; causes dead zones in oceans |
front 67 sedimentation - | back 67 too much sediment stops sunlight from reaching plants; carried from land to water through storm drains |
front 68 ocean acidification | back 68 excess carbon dioxide dissolved into ocean by waves; animals' shells are thinner |
front 69 carbonates - | back 69 organisms that make their own carbonate shells; build-up of material such as limestone and dolomite |
front 70 estuary - | back 70 a semi-enclosed area where fresh water and salt water mix |
front 71 salinity - | back 71 higher salinity closer to oceans; lower salinity in rivers higher salinity during droughts; lower salinity after rainfall |
front 72 Tsunami - | back 72 waves generated by sudden movements of the seafloor |
front 73 tides - | back 73 waves generated by the gravitational pull of the moon |
front 74 wind driven waves - | back 74 created by the transfer of wind energy to the ocean surface |
front 75 density driven waves - | back 75 located at the pycnocline (area in which water density increases at a rapid pace |
front 76 geologic driven waves - | back 76 created by sudden movements of the seafloor; mostly occur in the Pacific ocean |
front 77 tidal range - | back 77 the difference in height between high tides and low tides |
front 78 sonar - | back 78 works by transmitting sound waves towards the ocean bottom |
front 79 continental margin - | back 79 the zone of transition between ocean basin floor |
front 80 continental shelf - | back 80 the gently sloping submerged surface extending from the shoreline |
front 81 continental slope - | back 81 the steep gradient that leads to the deep ocean floor |
front 82 turbidity current - | back 82 the downslope movement of dense, sediment-laden water |
front 83 continental rise - | back 83 the gently sloping surface at the base of the continental slope |
front 84 ocean basin floor - | back 84 the area of the deep ocean floor between the continental margin and the oceanic ridge |
front 85 abyssal plain - | back 85 the very level area of the deep ocean floor |
front 86 seamount - | back 86 an isolated volcanic peak that rises at least 1000 meters above the deep ocean floor |
front 87 seafloor spreading - | back 87 the process by which plate tectonics produces at new oceanic ridges |
front 88 hydrothermal vents - | back 88 form along mid-ocean ridges; where mineral rich water escapes through cracks in the oceanic crust |
front 89 terrigenous sediments - | back 89 consist primarily of mineral grains that were eroded from continental rocks |
front 90 biogenous sediments | back 90 consists of shells and skeleton marine animals |
front 91 calcareous ooze | back 91 a thick, common biogenous sediment produced by dissolving calcium carbonate shells |
front 92 siliceous ooze | back 92 biogenous sediment composed of silica-based shells of single-celled animals |
front 93 hydrogenous sediment - | back 93 consists of minerals that crystallize directly from ocean water through various chemical reactions |
front 94 gas hydrates - | back 94 compact chemical structures made of water and natural gas |
front 95 manganese nodules - | back 95 hard lumps of manganese and other metals |
front 96 thermocline - | back 96 the layer of ocean water between about 300 meters and 100 meters |
front 97 relative humidity | back 97 is a ratio of the air's actual water-vapor content compared with the amount of water vapor |
front 98 dew point - | back 98 the temperature to which a parcel of air would need to be cooled to reach saturation |
front 99 cirrus - | back 99 clouds that are high, white, and thin |
front 100 cumulus - | back 100 clouds that consist of rounded individual cloud masses |
front 101 stratus - | back 101 clouds best described as sheets or layers that cover much or all of the sky |
front 102 solar eclipse - | back 102 occur when the moon moves in a line directly between earth and the sun |
front 103 lunar eclipse - | back 103 occur when the moon passes through the earth's shadow |
front 104 red giant - | back 104 a large, cool star of high luminosity; occupies the upper right portion of the HR diagram |
front 105 supergiant - | back 105 a very large, very bright red giant star |
front 106 protostar - | back 106 a collapsing cloud of gas and dust destined to become a star |
front 107 supernova - | back 107 an exploding massive star that increases in brightness many thousands of times |
front 108 white dwarf - | back 108 a star that has exhausted most or all of its nuclear fuel and has collapsed |
front 109 spiral galaxies - | back 109 about 30% of all galaxies; diameters of 20,000 to 125,000 light years |
front 110 elliptical galaxies - | back 110 about 60% of galaxies; range in shape from round to oval |