Curaçao (/?kj??r?sa?/ KYUR-uh-sao) is a liqueur flavored with the dried peel of the laraha citrus fruit, grown on the island of Curaçao.
A non-native plant similar to an orange, the laraha developed from the sweet Valencia orange transplanted by Spanish explorers in 1527. The nutrient-poor soil and arid climate of Curaçao proved unsuitable to Valencia cultivation, resulting in small, bitter fruit of the trees. Although the bitter flesh of the laraha is hardly edible, the peels are aromatic and flavorful, maintaining much of the essence of the Valencia orange.
To create the liqueur the laraha peel is dried, bringing out the sweetly fragranced oils. After soaking in a still with alcohol and water for several days, the peel is removed and other spices are added. The liqueur has an orange-like flavor with varying degrees of bitterness. It is naturally colorless, but is often given artificial coloring, most commonly blue or orange, which confers an exotic appearance to cocktails and other mixed drinks. Blue color is achieved by adding a food colorant, most often E133 Brilliant Blue.
Some other liqueurs are also sold as Curaçaos with different flavors added, such as coffee, chocolate, and rum and raisin.
Bitter lemon (Dry Lemon in South Africa) is a carbonated soft drink flavoured with quinine and lemon.
The signature bitter taste is produced by a combination of the quinine and the lemon pith used in manufacturing the drink. The principal difference between tonic water and bitter lemon is the addition of lemon juice and rind. Bitter lemon is drunk both by itself and as a mixer, and is sold across the world.
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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