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  • Polarized light photograph of ice crystals. Under polarized light the ice appears to have many colors within it. The colors are due to the ice crystals being birefringent in polarized light.
    K17Polarized-ice_0302.jpg
  • Polarized light photograph of ice crystals. Under polarized light the ice appears to have many colors within it. The colors are due to the ice crystals being birefringent in polarized light.
    K17Polarized-ice_0292.jpg
  • Regular water is frozen in an ice cube tray.  In a dark room the ice cube tray is twisted to release the cubes.  When ice breaks it releases light in a physical process known as triboluminescence.  This image was photographed at 409,000 ISO at F1.8 and is the first ever recorded image showing this common effect.  To observe this affect for yourself, twist an ice cube tray to release the cubes in a totally black room with your eyes adjusted to the dark for at least 5 minutes.  To observe this affect the colder the ice the better when it is broken.  This light is emitted from ice when it breaks, but is rarely seen due to the extremely low levels of light produced.
    K16-icebreaking0165.jpg
  • Regular water is frozen in an ice cube tray.  In a dark room the ice cube tray is twisted to release the cubes.  When ice breaks it releases light in a physical process known as triboluminescence.  This image was photographed at 409,000 ISO at F1.8 and is the first ever recorded image showing this common effect.  To observe this affect for yourself, twist an ice cube tray to release the cubes in a totally black room with your eyes adjusted to the dark for at least 5 minutes.  To observe this affect the colder the ice the better when it is broken.  This light is emitted from ice when it breaks, but is rarely seen due to the extremely low levels of light produced.
    K16ice-breaking0156.jpg
  • The vacuum chamber setup to boil ice water in a vacuum.  Ice water is placed in a beaker and the air is removed in a vacuum chamber.  Then the air pressure is lower that the waters vapor pressure the liquid will boil.
    K12vac-boil-icewater001.JPG
  • Ice water is placed in a beaker and the air is removed in a vacuum chamber.  Then the air pressure is lower that the waters vapor pressure the liquid will boil.
    K12vac-boil-icewater004.JPG
  • Thermogram of two ice skaters.  The different colors represent different temperatures on the object. The lightest colors are the hottest temperatures, while the darker colors represent a cooler temperature.  Thermography uses special cameras that can detect light in the far-infrared range of the electromagnetic spectrum (900?14,000 nanometers or 0.9?14 µm) and creates an  image of the objects temperature..
    ir07-273.jpg
  • Ice water is placed in a beaker and the air is removed in a vacuum chamber.  Then the air pressure is lower that the waters vapor pressure the liquid will boil.
    K12vac-boil-icewater002.JPG
  • An X-ray of an ice skate.
    x07iceskateablue.jpg
  • Thermogram of a woman ice skating.  The different colors represent different temperatures on the object. The lightest colors are the hottest temperatures, while the darker colors represent a cooler temperature.  Thermography uses special cameras that can detect light in the far-infrared range of the electromagnetic spectrum (900?14,000 nanometers or 0.9?14 µm) and creates an  image of the objects temperature..
    ir07-286.jpg
  • Thermogram of an ice skate.  The different colors represent different temperatures on the object. The lightest colors are the hottest temperatures, while the darker colors represent a cooler temperature.  Thermography uses special cameras that can detect light in the far-infrared range of the electromagnetic spectrum (900?14,000 nanometers or 0.9?14 µm) and creates an  image of the objects temperature..
    ir07-281.jpg
  • An ice cube is dropped in water, creating a splash.
    K09watersplash5407.jpg
  • Thermogram of a woman ice skating.  The different colors represent different temperatures on the object. The lightest colors are the hottest temperatures, while the darker colors represent a cooler temperature.  Thermography uses special cameras that can detect light in the far-infrared range of the electromagnetic spectrum (900?14,000 nanometers or 0.9?14 µm) and creates an  image of the objects temperature..
    ir07-343.jpg
  • An ice cube is dropped in water, creating a splash.
    K09watersplash5414.jpg
  • Scanning Electron Micrograph (SEM) of a sample if ice water hash or hashish. Shown in the image is a pile of glandular trichomes that have been concentrated in a unique process. Leaves with very high concentrations of stalked glandular trichomes are cooled in ice water then agitated. The agitation breaks off the trichomes, which in turn sink, to the bottom of the water.  Once separated from the water and dried, the ice water hash has some of the highest concentrations of THC of any physical separation process.  Since the stalked glandular trichomes are the location of the highest concentration of THC this technique in recent years has become very popular. The marijuana (Cannabis sativa) plant contains tetrahydrocannabinol (THC), the active component of cannabis when used as a drug. The spherical cells in this sample are 60 um in diameter.
    K170403hashish01.jpg
  • X-Ray of a speed skate.  Ice skate.
    x07-speed-skate1blue.jpg
  • A cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-ice-8520.jpg
  • A cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-ice-8505.jpg
  • A cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-ice-8563.jpg
  • A cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-ice-8558.jpg
  • A cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-ice-8545.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    070214frost0006.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5795.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5649.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5450.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5287.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_4648.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_9862PR-cropped.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_9738PR.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5855.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_4829.jpg
  • A cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-icicle-8626.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6817.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6794.jpg
  • Snowflake with a platelet crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6528.jpg
  • Snowflake with a platelet crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6525.jpg
  • Snowflake with a platelet crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6511.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11-snow6840.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11-snow6743.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5107.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_4206.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    fantastic2003.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    bIMG_4779.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    2100300012_RT8PR.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    Snowflake05-1936.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K14-snowflake9024A.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K13Snow011A.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K13snow006A.jpg
  • A cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-icicle-8632.jpg
  • Snowflake with a platelet crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11snowflake6501.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6779.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11-snow6824B.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5804.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5429.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_4967.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    coin_5128.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    2130300134_rt8PR.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    2130300089_RT8PR.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    k11-snowflake0058.jpg
  • Snowflake with a platelet crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6507.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_9604PR.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    snowKINSMAN5287.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6846.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    K11Snowflake6819.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5329.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5221.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_5194.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_4961.jpg
  • Snowflake with a stellar (or dendritic) crystal form, made in a cloud when water freezes at negative fifteen degrees Celsius. When crystallization occurs slowly, in calm air and in temperatures near the freezing point, snowflakes will exhibit hexagonal symmetry.
    IMG_4604.jpg
  • A lengthwise cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-icicle-8574.jpg
  • A lengthwise cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-icicle-8784.jpg
  • A lengthwise cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-icicle-8607.jpg
  • A lengthwise cross section of an icicle that is three days old. In this case the icicle grows rings similar to a tree. The age of an icicle can be determined by the number of heating and cooling cycles the icicle has gone through. This cross section is 2 mm thick and is photographed in polarized light.
    K12-icicle-8584.jpg
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