Midori is a sweet, bright-green-coloured, muskmelon-flavored liqueur made by Suntory. It is manufactured in Japan, United States, Mexico, and France, although it was made exclusively in Japan until 1987. Midori is usually 20-21% alcohol by volume. Its name is the Japanese word for "green". French-made Midori is sweeter than the original Japanese version.
As it is extremely sweet, Midori is not usually taken "straight"; it is generally used in a mixed drink (i.e., a cocktail), such as a Japanese slipper. It is usually used in a range of long drinks - with lemonade, fresh lemon juice, lime juice, pineapple juice, or orange juice. Sour flavours are often combined with it to balance its sweetness.
Named after the spanish word for lemon, BACARDÍ? LIMÓN is a carefully crafted product that infuses BACARDI rum with the essence of the royal family of citrus fruits: lemon, lime and grapefruit.
Sprite is a colourless, caffeine-free, lemon and lime-flavoured soft drink created by The Coca-Cola Company. It was first developed in West Germany in 1959 as Fanta Klare Zitrone (?Clear Lemon Fanta?) and was introduced in the United States under the current brand name Sprite in 1961 as a competitor to 7 Up. Bottles of Sprite are usually a transparent green colour with a green and yellow label whereas cans are coloured silver, green, and blue and aluminum bottles are coloured a solid lime green.
Ice is water frozen into a solid state. Depending on the presence of impurities such as particles of soil or bubbles of air, it can appear transparent or a more or less opaque bluish-white color.
In the Solar System, ice is abundant and occurs naturally from as close to the Sun as Mercury to as far as away the Oort cloud objects. Beyond the Solar System, it occurs as interstellar ice. It is abundant on Earth's surface - particularly in the polar regions and above the snow line - and, as a common form of precipitation and deposition, plays a key role in Earth's water cycle and climate. It falls as snowflakes and hail or occurs as frost, icicles or ice spikes.
Ice molecules can exhibit up to sixteen different phases (packing geometries) that depend on temperature and pressure. When water is cooled rapidly (quenching), up to three different types of amorphous ice can form depending on the history of its pressure and temperature. When cooled slowly correlated proton tunneling occurs below 20 K giving rise to macroscopic quantum phenomena. Virtually all the ice on Earth's surface and in its atmosphere is of a hexagonal crystalline structure denoted as ice Ih (spoken as "ice one h") with minute traces of cubic ice denoted as ice Ic. The most common phase transition to ice Ih occurs when liquid water is cooled below 0°C (273.15K, 32°F) at standard atmospheric pressure. It may also be deposited directly by water vapor, as happens in the formation of frost. The transition from ice to water is melting and from ice directly to water vapor is sublimation.
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