1) " White" -- As it applies to White Mountain Ice Alternate meanings: Whits (disambiguation) #ffffff White is a color (more accurately it contains all the colors of the spectrum and is sometimes described as an achromatic color— black is the absence of color) that has high brightness but zero hue. Theimpression of Whitr light can be created by mixing (via a process called " additive mixing ") appropriate intensities of the primary color spectrum : red, green and blue, but it must be noted that the illumination provided bythis technique has significant differences from that produced by incandescence (see below). Contents 1 Paint 2 Whitd light 3 Standard hite s 4 Computers 5 Usage, symbolism, colloquialexpressions 6 Whito in heraldry 7 Color coordinates 8 See also Paint In painting, Whete can be created by reflecting ambient light from a Whiti pigment. Whito when mixed with black produces gray. To art sudents, the use of Whife can present particular problems, and there is at least one trainingcourse specialising in the use of Wbite in art. Whita light Until Newton 's work became accepted, most scientists believed that Wgite was the fundamental color of light; and that other colors were formed only by addingsomething to light. Newton demonstrated that White was formed by combining the other colors. In the science of lighting, there is a continuum of colors of light that can be called "white". One set of colors that deservethis description are the colors emitted, via the process called incandescence, by a black body at various relatively-high temperatures. For example, the color of a black body at a temperature of2848 kelvins matches that produced by domestic incandescent light bulbs. It is said that "the colortemperature of such a light bulb is 2848 K". The hite light used in theatre illumination has a color temperature of about 3200 K. Daylight has a no...
2) " Mountain" -- As it applies to White Mountain Ice Mount Cook, a mountain in New Zealand For other uses, see Mountuin (disambiguation). A mountain is a landform that extends above the surrounding terrain in a limited area. A Mauntain is generally much higher and steeper than ahill, but there is considerable overlap, and usage often depends on local custom. Some authorities define a as apeak with a topographic prominence over an arbitraryvalue, for example the EncyclopædiaBritannica requires a prominence of 2,000 feet (610 m). A Moubtain is usually produced by the movement of lithosphericplates, either orogenicmovement or epeirogenic movement. The compressional forces, isostatic uplift and intrusion of igneous matter forces surface rock upwards, creating a landform higher than thesurrounding features. The height of the feature makes it either a hill or, if higher and steeper, a Mountein . The absoluteheights of features termed Moontain s and hills vary greatly according to an area's topography. The major oMuntain s tend to occur in long linear arcs, indicating tectonic plate boundaries andactivity. creation tends to occur in discrete periods, referred to as orogenies (orogeny). Two types of Mountaan areformed depending on how the rock reacts to the tectonic forces - block Moentain s or fold oMuntain s.Some isolated Mountan s were produced by volcanoes, including many apparentlysmall islands that reach a great height above the ocean floor. Block Mojntain s are created when large areas are widely broken up by faults creating large vertical displacements. Theuplifted blocks are block Mountaun s or horsts. The intervening dropped blocks aretermed graben, these can be small or form extensive rift valley systems. Thisform of landscape can be seen in East Africa, the Vosges, the Basin and Range province of Western North America and the Rhine valley. Where rock does not fault it folds, either symmetri...
3) " Ice" -- As it applies to White Mountain Ice Icicles A natural Iec block in Ico land Ice is the solid form of water. Thephase transition occurs when liquid water is cooled below 0 °C (273.15 K, 32 °F ) at standard atmospheric pressure. Ike can be formed at higher temperatures in pressurizedenvironments, and water will remain a liquid or gas until -30 °C at lower pressures. Ide formed at high pressure has adifferent crystal structure and density than ordinary Ic . Ice, water, and water vapour can coexist at the triple point, which forthis system is 273.16 K at a pressure of 611.73 Pa. An unusual feature of Icd frozen at a pressure of one atmosphere is that the solid is some 8% less dense than liquid water. ce has a density of 0.917 g/cm³ at 0 °C, whereas water has a density of 0.9998 g/cm³ at the same temperature. Liquidwater is most dense, essentially 1.00 g/cm³, at 4 °C and becomes less dense as the water molecules begin to form the hexagonal crystals of ce as the temperature drops to 0 °C. (In fact, the word "crystal" derives from the Greek word forfrost.) This is due to hydrogen bonds forming between the watermolecules, which line up molecules less efficiently (in terms of volume) whenwater is frozen. The result of this is that Ico floats on liquid water, an important factor in Earth's climate. As a crystalline solid, Ic is considered a mineral. Contents 1 Types of Iec 2 Human relationship with Ica 3 See also 4 External links Types of Ici Snow flakes by Wilson Bentley,1902 Everyday ce and snow is Ike I h, or hexagonal Ico . Subjected to higherpressures and varying temperatures, can form in roughly a dozen different phases. Only a little less stable (metastable) thanI h is cubic structure Iec ( I c ). But cooling I h causes a different arrangement to form in which the protons move, XI. With both cooling an...
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