Mother Lode (Methow Mountains)

{{short description|Mountain in Washington (state), United States}}

{{Infobox mountain

| name = Mother Lode

| photo = Mother Lode Peak.jpg

| photo_caption = North aspect, from Wallaby Peak

| elevation_ft = 7905

| elevation_ref = {{cite peakbagger|1936|Mother Lode Peak, Washington}}

| prominence_ft = 1585

| prominence_ref =

| isolation_mi = 3.03

| isolation_ref = {{cite web |url = https://listsofjohn.com/peak/48940|title = Mother Lode WA - 7,905'|website = Lists of John |access-date = 2021-09-27}}

| parent_peak = Gilbert Mountain (8,023 ft)

| etymology = Mother lode

| country = United States

| state = Washington

| region = Okanogan

| region_type = County

| part_type = Protected area

| part = Lake Chelan-Sawtooth Wilderness

| range = Cascade Range
North Cascades
Methow Mountains

| map = Washington#USA

| map_size = 270

| map_caption = Location in Washington

| label_position = right

| mapframe = yes

| mapframe-zoom = 8

| mapframe-caption = Interactive map of Mother Lode

| coordinates = {{coord|48.443559|N|120.615132|W|type:mountain_region:US-WA_scale:100000_source:ngs|format=dms|display=inline,title}}

| coordinates_ref =

| topo = USGS Gilbert

| rock =

| first_ascent =

| easiest_route = {{YDS|4}} scrambling North Ridge

}}

Mother Lode is a {{convert|7,905|ft|meter|adj=mid|-elevation|abbr=off|sp=us}} mountain summit located in the North Cascades, in Okanogan County, Washington.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Volume 3, 2nd Edition, Mountaineers Books, 2000, page 281. It is situated in the Lake Chelan-Sawtooth Wilderness, on land managed by Okanogan–Wenatchee National Forest. The mountain is part of the Methow Mountains, which are a subset of the Cascade Range, and the peak is approximately two miles east of the crest of the range. Mother Lode is set approximately six miles south of Washington Pass, and the nearest higher neighbor is Gilbert Mountain, three miles to the northeast. Topographic relief is significant as the north aspect rises {{convert|3,500|ft|m|abbr=off|sp=us}} above the South Fork Twisp River in one mile. The peak was climbed in 1983 by Rick La Belle and Glen Sterr via the north ridge, and the northeast ridge was climbed in 1985 by Carl and Gordon Skoog. Precipitation runoff from the peak drains into tributaries of Twisp River, which in turn is a tributary of the Methow River.

Climate

Weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, 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 west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall.Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. 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.

Geology

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, ridges, and deep glacial valleys. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences. These climate differences lead to vegetation variety defining the ecoregions in this area. The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.{{cite book|last=Kruckeberg|first=Arthur|title=The Natural History of Puget Sound Country|publisher=University of Washington Press|year=1991}} With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. The U-shaped cross section of the river valleys is a result of 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 North Cascades area.

Gallery

File:MotherLode Mountain.jpg|Mother Lode Peak

References

External links

Mother Lode weather forecast: [https://www.mountain-forecast.com/peaks/Mother-Lode/forecasts/2409 Mountain-forecast.com]
Mother Lode photo: [https://www.flickr.com/photos/johnwporter/51203117702/in/dateposted/ Flickr]

{{Geographic Location 2

| Center = Mother Lode

| North = Wallaby Peak

| Northeast = Gilbert Mountain

| East = Crescent Mountain

| Southeast =

| South = South Creek Butte

| Southwest =

| West = Hock Mountain

| WNW = Twisp Mountain

| Northwest = Lincoln Butte

}}