Backcheck
The backcheck is an ice hockey defensive transition play made (primarily) in the neutral zone. It is a type of checking. The purpose of the backcheck is to try to limit the opponents options as they head up the ice towards the backchecking team's end zone. The backcheck may be initialized by situations such as having lost the puck in the opponent's half of the ice, the opponents having played through the first line of pressure in their own end zone, or having lost a faceoff in the neutral zone. An important aspect of backchecking is counting the opponent's players. This is so as to make sure that the opponents are not gaining any significant numerical advantages on the ice during transition. Failure to adequately count numbers in particular in the neutral zone by the backchecking team most likely leads to numerical advantages by the opponent when, and if, entering the backchecking team's end zone. A proper backcheck leads to significantly less time and space for the opponents ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
200-foot Game
A 200-foot game is a definition in ice hockey that describes a player's (usually a forward's) ability to have strong presence in all three zones of an ice rink, which is standardized at 200 feet long. Players who can play a 200-foot game are contrasted with players who score a lot of points by avoiding hard forechecking or backchecking, cherry picking their plays perhaps for breakaways, and avoiding fighting for the puck in the corners of the rink, such as Pavel Bure or Brett Hull. Playing a 200-foot game means fighting for each part of the ice, fighting for control of the puck whether it's in one's possession or not, and engaging using your body in traffic. Classic examples of players who exemplify the 200-foot player include Gordie Howe, Bryan Trottier, Jari Kurri, Steve Yzerman, Patrice Bergeron, Doug Gilmour, Pavel Datsyuk, Mike Modano, Bobby Clarke, Sergei Fedorov, Joe Sakic, Anže Kopitar, Bob Gainey, Frank Nighbor and Sidney Crosby. Having players able to play a 200-fo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Ice Hockey
Ice hockey (or simply hockey) is a team sport played on ice skates, usually on an ice skating rink with lines and markings specific to the sport. It belongs to a family of sports called hockey. In ice hockey, two opposing teams use ice hockey sticks to control, advance and shoot a closed, vulcanized, rubber disc called a " puck" into the other team's goal. Each goal is worth one point. The team which scores the most goals is declared the winner. In a formal game, each team has six skaters on the ice at a time, barring any penalties, one of whom is the goaltender. Ice hockey is a full contact sport. Ice hockey is one of the sports featured in the Winter Olympics while its premiere international amateur competition, the IIHF World Championships, are governed by the International Ice Hockey Federation (IIHF) for both men's and women's competitions. Ice hockey is also played as a professional sport. In North America as well as many European countries, the sport is known simply ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Ice Hockey Rink
An ice hockey rink is an ice rink that is specifically designed for ice hockey, a competitive team sport. Alternatively it is used for other sports such as broomball, ringette, rinkball, and rink bandy. It is a rectangle with rounded corners and surrounded by walls approximately high called the ''boards''. Name origins ''Rink'', a Scots word meaning 'course', was used as the name of a place where another game, curling, was played. Early in its history, ice hockey was played mostly on rinks constructed for curling. The name was retained after hockey-specific facilities were built. Dimensions There are two standard sizes for hockey rinks: one used primarily in North America, also known as NHL size, the other used in Europe and international competitions, also known as IIHF or Olympic size. International Hockey rinks in the rest of the world follow the International Ice Hockey Federation (IIHF) specifications, which are with a corner radius of . The two goal lines are fr ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Checking (ice Hockey)
Checking in ice hockey is any of a number of defensive techniques aimed at disrupting an opponent with possession of the puck or separating him from the puck entirely. Most types are not subject to penalty. Types Body checking A player drives the shoulder, upper arm and hip and elbow, equally into the opponent to separate him from the puck, using the body to knock an opponent against the boards or to the ice. This is often referred to as simply ''checking'' or ''hitting'' and is only permitted against an opponent with possession of the puck. Body checking can be penalized when performed recklessly. In women's IIHF ice hockey, body checking is considered an "illegal hit" as well as in non-checking leagues, and is punishable by a minor penalty, major penalty and automatic game misconduct, or match penalty. Body checking was allowed at the first women's world ice hockey championship in 1990 but has been considered illegal since. Hip-checking When a player drops to a near-cro ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Neutral Zone Trap
The neutral zone trap (often referred to as simply the trap) is a defensive strategy used in ice hockey to prevent an opposing team from proceeding through the neutral zone (the area between the blue lines) and to force turnovers. Description The strategy is generally used to level the playing field for teams that are not as offensively talented as their opponents, although the trap can also be used by teams simply looking to protect a lead late in the game. The most recognizable implementation of the trap sees the defense stationing four of their players in the neutral zone and one forechecker in the offensive zone. As the offensive team starts to move up the ice, the forechecker (generally the center) will cut off passing lanes to other offensive players by staying in the middle of the ice, forcing the puck carrier to either sideboard. The defensive wingers—typically placed on or near the red line—will be positioned by the boards to challenge the puck carrier, prevent pa ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Forecheck
The forecheck is an ice hockey defensive coverage play made (primarily) in the offensive zone with the objective of applying pressure to the opposing team to regain control of the puck. It is a type of checking. Forechecking is generally executed in one of three situations: recovery of the puck after a dump in, after the rebound following a scoring attempt, or immediately after a turnover to regain possession. Forechecking can be aggressive or conservative depending on the coaching style and on the skating skills of the players. Aggressive forechecking strategies are more suited for players with good skating mobility, while more conservative plays such as the neutral zone trap The neutral zone trap (often referred to as simply the trap) is a defensive strategy used in ice hockey to prevent an opposing team from proceeding through the neutral zone (the area between the blue lines) and to force turnovers. Description ... are better suited for players with less agility. ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Ice Hockey Strategy
Ice is water frozen into a solid state, typically forming at or below temperatures of 0 degrees Celsius or 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 away as the Oort cloud objects. Beyond the Solar System, it occurs as interstellar ice. It is abundant on Earth's surfaceparticularly in the polar regions and above the snow lineand, 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 and aggregates from snow as glaciers and ice sheets. Ice exhibits at least eighteen phases ( packing geometries), depending on temperature and pressure. When water is cooled rapidly (quenching), up to three types of amorphous ice can form depending on i ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |