1764 map showing western part of the island of Montreal (Isle de Mont Real), with the growing town centred on Fort Ville Marie in the upper right and the Cedars (overlooking Rapide du coteau des Cedres) in the map's lower left corner.

The Battle of the Cedars (French: Bataille des Cèdres) was a series of military confrontations in the early stages of the American Revolutionary War that occurred during the Continental Army's invasion of Quebec, which began in September 1775. These skirmishes, which involved limited combat, occurred in May 1776 at and around the Cedars, 45 km (28 mi) west of Montreal, Quebec. Continental Army units were opposed by a small British Army detachment leading a larger force of Haudenosaunee warriors and Canadian Militia.

Brigadier General Benedict Arnold, commanding the American garrison at Montreal, had placed a detachment of his troops at the Cedars in April 1776, after hearing of rumors of British and Indian military preparations to the west of Montreal. The detachment surrendered on May 19 after a confrontation with a combined British-Haudenosaunee force led by Captain George Forster. American reinforcements on their way to the Cedars were also captured after a brief skirmish on May 20. All of the prisoners were eventually released after negotiations between Forster and Arnold, who brought a sizable force into the area. The terms of the agreement required the Americans to release an equal number of British prisoners, but the deal was repudiated by the Second Continental Congress and no British prisoners were freed. (Full article...)

Joseph Georges Gonzague Vézina (/ˈvɛzɪnə/; French: [ʒɔʁʒ vezina]; January 21, 1887 – March 27, 1926) was a Canadian professional ice hockey goaltender who played seven seasons in the National Hockey Association (NHA) and nine in the National Hockey League (NHL), all with the Montreal Canadiens. After being signed by the Canadiens in 1910, Vézina played in 327 consecutive regular season games and a further 39 playoff games, before leaving early during a game in 1925 due to illness. Vézina was diagnosed with tuberculosis, and died on March 27, 1926.

The only goaltender to play for the Canadiens between 1910 and 1925, Vézina helped the team win the Stanley Cup in 1916 and 1924, while reaching the Stanley Cup Finals three more times. Nicknamed the "Chicoutimi Cucumber" for his calm composure while in goal, Vézina allowed the fewest goals in the league seven times in his career: four times in the NHA and three times in the NHL. In 1918, Vézina became the first NHL goaltender to both record a shutout and earn an assist on a goal. At the start of the 1926–27 NHL season, the Canadiens donated the Vezina Trophy to the NHL as an award to the goaltender who allowed the fewest goals during the season. Since 1981, the award has been given to the most outstanding goaltender as determined by a vote of NHL general managers. In Vézina's hometown of Chicoutimi, the sports arena is named the Centre Georges-Vézina in his honour. When the Hockey Hall of Fame opened in 1945, Vézina was one of the original nine inductees, and in 2017 the NHL included him on their list of the 100 greatest players in league history. (Full article...)

West face of Mount Garibaldi

Mount Garibaldi (Squamish: Nch'ḵay̓, pronounced [n̩.ʧʼqɛˀj̰]) is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of 2,678 metres (8,786 feet) and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks. Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome. Both were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is a landslide feature that formed in a series of collapses between 12,800 and 11,500 years ago. These collapses resulted in the formation of a large debris flow deposit that fans out into the Squamish Valley.

Mount Garibaldi has been the focus of intermittent volcanic activity over the last 260,000 years. This activity produced mostly dacite, the main type of volcanic rock forming Mount Garibaldi. Volcanism between 260,000 and 220,000 years ago constructed an ancestral cone that was subsequently destroyed. Another growth period began with the eruption of Atwell Peak about 13,000 years ago when Mount Garibaldi was surrounded by an ice sheet during the last glacial period. The latest period of volcanic activity took place about 10,000 years ago with eruptions from Dalton Dome and Opal Cone after the ice sheet retreated. Although the mountain is not known to have been volcanically active since that time, it could erupt again, which could endanger the nearby populace. If this were to happen, relief efforts could be organized by teams such as the Interagency Volcanic Event Notification Plan who are prepared to notify people threatened by volcanic eruptions in Canada. (Full article...)