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The WECC Region extends from Canada to Mexico and includes the provinces of Alberta and British Columbia, the northern portion of Baja California, Mexico, and all or portions of the 14 Western states between. Membership in WECC is open to all entities who meet the qualifications in the WECC Bylaws.
The 2015 California drought brought pipeline proposals back to the public consciousness, abetted by celebrities Rush Limbaugh and William Shatner, [7] the latter proposing a Kickstarter campaign to raise $30 billion to fund such a pipeline from Washington state. [8] As of 2013, there were no interstate water pipelines to California. [9]
Ice Energy was founded in 2003. The assets of Ice Energy were reformed into Ice Energy Holdings in 2012. [5] In August 2014, Ice Energy revealed a version of the Ice Bear for single-family homes called the Ice Cub. [6] In November, the company won sixteen contracts with Southern California Edison. [7] [8] The contracts totaled 25.6 megawatts. [9]
The Columbia Icefield is the largest ice field in North America's Rocky Mountains. [1] Located within the Canadian Rocky Mountains astride the Continental Divide along the border of British Columbia and Alberta, Canada, the ice field lies partly in the northwestern tip of Banff National Park and partly in the southern end of Jasper National Park.
Pages in category "Ice fields of Alberta" The following 4 pages are in this category, out of 4 total. This list may not reflect recent changes. C. Chaba Icefield;
The Wapta Icefield from Mistaya Mountain. The Wapta Icefield is a series of glaciers located on the Continental Divide in the Waputik Mountains of the Canadian Rockies, in the provinces of British Columbia and Alberta, [1] in Yoho National Park in the Canadian Rockies. [2]
An ice cave is any type of natural cave (most commonly lava tubes or limestone caves) that contains significant amounts of perennial (year-round) ice. At least a portion of the cave must have a temperature below 0 °C (32 °F) all year round, and water must have traveled into the cave’s cold zone.
Unlike the Laurentide Ice Sheet, which may have taken as many as eleven thousand years to fully melt, [3] the Cordilleran ice sheet melted very quickly, probably in four thousand years or less. [4] This rapid melting caused floods such as the overflow of Lake Missoula and shaped the topography of the fertile Inland Empire of Eastern Washington. [5]