| Big Chiwaukum | |
| Elevation Ft: | 8098 |
| Elevation Ref: | [1] |
| Prominence Ft: | 3721 |
| Isolation Mi: | 10.43 |
| Parent Peak: | Mount Stuart |
| Range: | Chiwaukum Mountains Wenatchee Mountains Cascade Range |
| Map: | Washington#USA |
| Country: | United States |
| State: | Washington |
| Region: | Chelan |
| Region Type: | County |
| Part Type: | Protected area |
| Part: | Alpine Lakes Wilderness |
| Coordinates: | 47.7024°N -120.9347°W |
| Topo: | USGS Chiwaukum Mountains |
| Rock: | Schist |
| Easiest Route: | Scrambling Class 3[2] |
Big Chiwaukum is a prominent 8098feet mountain in Chelan County, Washington, United States. Big Chiwaukum is located northeast of Frosty Pass, and within the Alpine Lakes Wilderness. Big Chiwaukum is the highest peak in the Chiwaukum Mountains, a subset of the Cascade Range. The nearest higher peak is Cashmere Mountain, 10.35miles to the south-southeast. Precipitation runoff from Big Chiwaukum drains into tributaries of the Wenatchee River. In the Wenatchee dialect, Chiwaukum means many little creeks running into one big one.[3]
Most weather fronts originating in the Pacific Ocean travel east toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the Cascades experience high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.
The Alpine Lakes Wilderness features some of the most rugged topography in the Cascade Range with craggy peaks and ridges, deep glacial valleys, and granite walls spotted with over 700 mountain lakes.[4] Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences.Big Chiwaukum is composed of schist, part of the Nason terrane laid down 210 million years ago.[5] During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.[6] The last glacial retreat in the Alpine Lakes area began about 14,000 years ago and was north of the Canada–US border by 10,000 years ago.[6] The U-shaped cross section of the river valleys is a result of that recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the Alpine Lakes Wilderness area.