Liqueurs are alcoholic beverages that are bottled with added sugar and have added flavors that are usually derived from fruits, herbs, or nuts. Liqueurs are distinct from eaux-de-vie, fruit brandy, and flavored liquors, which contain no added sugar. Most liqueurs range between 15% and 55% alcohol by volume.
Orange juice is the liquid extract of the fruit of the orange tree, made by squeezing the fresh orange. Some commercial orange juice with a long shelf life are made by drying and later re-hydrating the juice, or by concentrating the juice and later adding water to the concentrate. Others are made by pasteurizing the juice and removing oxygen from it, necessitating the later addition of a flavor pack, generally made from orange products. It is known for its health benefits, particularly its high concentration of vitamin C. It comes in several different varieties, including blood orange. In American English, the beverage name may be abbreviated as "OJ".
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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