Vätterstads IK
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Vätterstads IK
Vätterstads IK is a former Swedish ice hockey club from Jönköping. The club was formed in mid 1967 as a merger of IK Stefa and Vättersnäs IF. The club played its home games in Rosenlundshallen, which later was HV71's arena for a period. The club played in the Swedish second division in the seasons of 1967-1968 and 1968-1969 In 1971 the club was merged with Husqvarna IF's ice hockey Ice hockey (or simply hockey in North America) is a team sport played on ice skates, usually on an Ice rink, ice skating rink with Ice hockey rink, lines and markings specific to the sport. It belongs to a family of sports called hockey. Tw ... section forming the still active HV71. References Ice hockey teams in Jönköping County Ice hockey clubs established in 1967 Ice hockey clubs disestablished in 1971 Sport in Jönköping HV71 1967 establishments in Sweden 1971 disestablishments in Sweden Sport in Huskvarna 20th-century establishments in Jönköping County 20th-cent ...
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Ice Hockey
Ice hockey (or simply hockey in North America) is a team sport played on ice skates, usually on an Ice rink, ice skating rink with Ice hockey rink, lines and markings specific to the sport. It belongs to a family of sports called hockey. Two opposing teams use ice hockey sticks to control, advance, and Shot (ice hockey), shoot a vulcanized rubber hockey puck into the other team's net. Each Goal (ice hockey), goal is worth one point. The team with the highest score after an hour of playing time is declared the winner; ties are broken in Overtime (ice hockey), overtime or a Shootout (ice hockey), shootout. In a formal game, each team has six Ice skating, skaters on the ice at a time, barring any penalties, including a goaltender. It is a contact sport#Grades, full contact game and one of the more physically demanding team sports. The modern sport of ice hockey was developed in Canada, most notably in Montreal, where the first indoor ice hockey game, first indoor game was play ...
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Ice Hockey Teams In Jönköping County
Ice is water that is freezing, frozen into a solid state, typically forming at or below temperatures of 0 °Celsius, C, 32 °Fahrenheit, F, or 273.15 Kelvin, K. It occurs naturally on Earth, on other planets, in Oort cloud objects, and as interstellar ice. As a naturally occurring crystalline inorganic solid with an ordered structure, ice is considered to be a mineral. Depending on the presence of Impurity, impurities such as particles of soil or bubbles of air, it can appear transparent or a more or less Opacity (optics), opaque bluish-white color. Virtually all of the ice on Earth is of a Hexagonal crystal system, hexagonal Crystal structure, crystalline structure denoted as ''ice Ih'' (spoken as "ice one h"). Depending on temperature and pressure, at least nineteen phases of ice, phases (Sphere packing, packing geometries) can exist. The most common phase transition to ice Ih occurs when liquid water is cooled below (, ) at standard atmospheric pressure. When water is coo ...
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