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</style><p class="p_CC664AAA"><span class="s_3FE45715">On Wednesday, there were reports of several human triggered size 1 wind slab avalanches. </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/3311db23-7039-4e1f-a51c-f191cd31a022" target="_blank"><span class="s_B5813F7D">Check out this MIN report from Wednesday.</span></a><span class="s_AA239A9B" /></p><p class="p_CC664AAA"><span class="s_3FE45715">There were no avalanches reported Sunday through Tuesday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">On Saturday, a persistent slab avalanche was triggered by a skier on a north aspect on a 30 degree slope. </span><a href="https://www.avalanche.ca/mountain-information-network/submissions/043c732e-fd04-4102-be4c-0004e2dcf9f9" target="_blank"><span class="s_B5813F7D">Check out the MIN report here.</span></a><span class="s_3FE45715"> These sorts of avalanches are becoming less frequent, but they are still possible and the consequences are high.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">There was also evidence of large avalanches (up to size 3) that were triggered by strong wind in the north of the region on Saturday.</span></p><p class="p_CC664AAA"><span class="s_3FE45715">Last Friday, two small to large (size 1 to 2) persistent slab avalanches were triggered by humans. They were 50 to 70 cm deep and released on the mid-January surface hoar layer described in the Snowpack Summary. They occurred at treeline and alpine elevations on north to northwest aspects.</span></p>