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During the Pleistocene and on into the Holocene epoch Leavenworth would have been a cold place to live. An alpine glacier originating from the southwest in the Mt. Stuart range made its way to where the town is today. Leavenworth actually sits on the terminal moraine of that glacier. A drive through the residential parts of town display many glacier erratic's that originated 20 miles away up the Icicle valley near Mt. About 19, years ago a large rock slide dammed the Columbia River near Rock Island just south of Wenatchee. The temporary dam, in conjunction with one of the Lake Missoula floods, caused the water to flow back up the Wenatchee valley where it was stopped by the glacier at Leavenworth.

As the leading edge of the glacier interacted with the flood, ice rafts formed carrying granite erratics from the Stuart batholith ending up in the town of Dryden about 15 miles down valley from Leavenworth.

As the glacier retreated, the south side of Leavenworth was a lake dammed up by the dtaing. The bridge on daging east side of town is a good vantage point to see where the Wenatchee River cuts through the moraine today. During the summer, the weather is typically anticyclonic due to Leavenworth wa dating presence of the North Pacific anticyclone, with resultant clear skies and large diurnal temperature ranges. Rainfall is limited by the Cascade rain shadow as well as by the anticyclone, and all months from May to October have recorded zero precipitation on occasions: However, on cooler, stiller days, summer nights can still be cold and frosts have been recorded as early as August 29 of The fall months see steady cooling and a gradual increase in the frequency of frontal storms producing rainfall, whilst winter weather is typically cold and snowy, with an annual mean snowfall of The snowiest season has been from July to June with On occasions, as in January and Februaryand Januaries, andvery cold and dry Arctic air from western Canada can invade the basin, turning the weather much colder and frequently clearer:

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