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Accumulation can take place by snowfall directly over the glacier floor but in addition from avalanches that deposit snow from slopes adjacent to your glacier and from snow currently being blown onto the glacier from bordering spots. In certain locations with the Earth, condensation of h2o vapor on glacier surfaces https://918kiss-apk34555.activosblog.com/34942503/kiss918-things-to-know-before-you-buy

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