Mappa topografica Mabel Lake

Vancouver, British Columbia, is situated on the Burrard Peninsula, bordered by Burrard Inlet to the north and the Fraser River to the south. The city's topography is a blend of flat and hilly terrains, with elevations ranging from sea level to approximately 152 meters (500 feet) above sea level. The North…

Altitudine media: 34 m

The area has a humid continental climate (Köppen climate classification Dfb, Trewartha Dclo), but is close to (and once had) a subarctic climate (Dfc) as May and September averages are both close to the 10 °C (50 °F) threshold. Winters are milder than the latitude and elevation might suggest: the January…

Altitudine media: 685 m

Kelowna is classified as a humid continental climate or an inland oceanic climate per the Köppen climate classification system due to its coldest month having an average temperature slightly above −3.0 °C (26.6 °F) and below 0 °C (32 °F), with dry, hot, sunny summers and cool, cloudy winters, and four…

Altitudine media: 704 m

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Burnaby occupies 98.6 square kilometres (38.1 sq mi) and is located at the geographic centre of the Metro Vancouver Regional District. The regional district's government is located in Burnaby's Metrotown area. Situated between the city of Vancouver on the west and Port Moody, Coquitlam, and New Westminster on…

Altitudine media: 59 m

Altitudine media: 833 m

Victoria, British Columbia, is situated on the southern tip of Vancouver Island, Canada, and boasts a diverse and varied topography. The city is characterized by rolling hills, rugged coastal cliffs, and lush valleys, providing a striking contrast between mountainous terrain and flatland areas. To the north…

Altitudine media: 17 m

The rain shadow effect of the island's mountains, as well as the mountains of Washington's Olympic Peninsula, creates wide variation in precipitation. The west coast is considerably wetter than the east coast. Average annual precipitation ranges from 6,650 mm (262 in) at Hucuktlis Lake on the west coast…

Altitudine media: 411 m

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The western part of the district, the Stave Valley, is largely rural and forested but its watercourse is home to what was the largest hydroelectric project in British Columbia until the Bridge River Power Project opened in 1961. It was built by the British Columbia Electric Railway (BCER) to provide power to…

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The Williams Lake Airport weather station is at an elevation of 939.7 m (3,083 ft) while the Williams Lake River weather station is at 585.2 m (1,920 ft), a difference of 354.5 m (1,163 ft). Thus the average temperature is significantly warmer in the city proper than the airport.

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The rain shadow effect of the island's mountains, as well as the mountains of Washington's Olympic Peninsula, creates wide variation in precipitation. The west coast is considerably wetter than the east coast. Average annual precipitation ranges from 6,650 mm (262 in) at Hucuktlis Lake on the west coast…

Altitudine media: 411 m

Altitudine media: 12 m

Like much of Metro Vancouver, Coquitlam has an oceanic climate (Köppen climate type Cfb), experiencing mild temperatures and high precipitation; warm, dry summers and cool, wet winters. However, compared to most other cities in the area, precipitation is especially heavy in Coquitlam due to its proximity to…

Altitudine media: 190 m

Kimberley has a continental climate with semi-arid influences and heavy moderation from the nearby mountains which tend to block arctic air masses, and produce a rain shadow. Its fairly high elevation counters this effect slightly, as temperatures are somewhat cooler and the town slightly more rainy than it…

Altitudine media: 1’216 m

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Carved out of an ancient floodplain, the small terrace upon which Chetwynd is situated lies in the northern foothills of the Rocky Mountains. Once used as a grazing spot by nomadic Aboriginals, the terrace was farmed by settlers until it was developed into a town. Two types of soil—namely, the Widmark and…

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A small ski resort featuring a single short lift has operated on Mount MacKenzie since the 1960s, and snowcat skiing was offered for higher altitudes. A strong movement pushed to expand the entire mountain into a single resort, and construction started in the early 2000s (decade).

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Snowfalls are also more common than many parts of the City of Vancouver because of the area's higher altitude and the lack of an urban heat island due to less terrestrial development.

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