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  1. Missoula, Montana - Wikipedia

    en.wikipedia.org/wiki/Missoula,_Montana

    Missoula / mɪˈzuːlə / (listen) is a city in the U.S. state of Montana; it is the county seat of Missoula County. It is located along the Clark Fork River near its confluence with the Bitterroot and Blackfoot Rivers in western Montana and at the convergence of five mountain ranges, thus it is often described as the "hub of five valleys".

  2. Missoula, Montana - Simple English Wikipedia, the free ...

    simple.wikipedia.org/wiki/Missoula,_Montana

    From Simple English Wikipedia, the free encyclopedia Missoula is a city in the U.S. state of Montana and is the county seat of Missoula County. In 2014, the United States Census Bureau estimated the city's population at 69,821 and the population of the Missoula Metropolitan Area at 112,684.

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  4. www.wikipedia.org

    www.wikipedia.org/wiki/Missoula

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  5. Missoula - Wikipedia

    sco.wikipedia.org/wiki/Missoula

    Missoula is a ceety o the U.S. state o Montana an the coonty seat o Missoula Coonty. Wi a population o 66,788 at the 2010 census, it is the second maist populous ceety in the state.

  6. Lake Missoula - Wikipedia

    en.wikipedia.org/wiki/Lake_Missoula
    • Overview
    • Geology
    • Basins of Lake Missoula

    Lake Missoula was a prehistoric proglacial lake in western Montana that existed periodically at the end of the last ice age between 15,000 and 13,000 years ago. The lake measured about 7,770 square kilometres and contained about 2,100 cubic kilometres of water, half the volume of Lake Michigan. The Glacial Lake Missoula National Natural Landmark is located about 110 kilometres northwest of Missoula, Montana, at the north end of the Camas Prairie Valley, just east of Montana Highway 382 and Macfa

    The Cordilleran ice sheet originating in British Columbia expanded out of the mountains and southward. A tongue of ice pushed down the Purcell Valley or Purcell Trench, reaching south beyond Lake Pend Oreille. This Purcell Lobe blocked the natural outlet of the Clark Fork River.

    The Clark Fork's drainage is a network of valleys among high mountain ranges. Lake Missoula formed through this region of western Montana. It is named for the Missoula in the upper reaches of the Clark Fork watershed. The mountains surrounding the city show the strandlines from t

    This reach follows Montana Route 200 up the Clark Fork River canyon, 92 miles to Paradise, then following the Clark Fork, then 49 miles through the Paradise-St. Regis Canyon along Montana Route 135. At St. Regis, the canyon opens out and continues to the east 49 miles with the ri

    The Flathead basin abutted the south face of the ice sheet. For most of this period, the glacial ice reached south to Polson, covering the entirety of Flathead Lake. The basin drains from the Polson Moraine at the south end of Flathead Lake, south to Ravalii with a major lobe up

    The basin extends from Missoula, west to Ninemile and up the Ninemile Creek valley. This 39 miles long valley broadens from 5 miles at Ninemile and to 10 miles at Missoula. The central part of this basin around Missoula is 8 miles wide E-W and 10 miles N-S. The basin is bordered

    • 1966
    • Western Montana
  7. Downtown Missoula - Wikipedia

    en.wikipedia.org/wiki/Downtown_Missoula

    Downtown Missoula is the central business district in Missoula, Montana, and West-Central Montana.Downtown Missoula's rough boundaries are the Clark Fork River to its south, Madison St. to its east, the old U.S 93 highway/ North Orange St. to its west, and West Alder St. to its north, though parts south of the Clark Fork River are also at times mentioned.

  8. Fort Missoula - Wikipedia

    en.wikipedia.org/wiki/Fort_Missoula

    Fort Missoula From Wikipedia, the free encyclopedia Fort Missoula was established by the United States Army in 1877 on land that is now part of the city of Missoula, Montana, to protect settlers in Western Montana from possible threats from the Native American Indians, such as the Nez Perce.

  9. Missoula floods - Wikipedia

    en.wikipedia.org/wiki/Missoula_Floods
    • Overview
    • Flood hypothesis proposed
    • Flood initiation
    • Flood events

    The Missoula floods were cataclysmic glacial lake outburst floods that swept periodically across eastern Washington and down the Columbia River Gorge at the end of the last ice age. These events have been researched since the 1920s. These were the result of periodic sudden ruptures of the ice dam on the Clark Fork River that created Glacial Lake Missoula. After each ice dam rupture, the waters of the lake would rush down the Clark Fork and the Columbia River, flooding much of eastern Washington

    Geologist J Harlen Bretz first recognized evidence of the catastrophic floods, which he called the Spokane floods, in the 1920s. He was researching the Channeled Scablands in Eastern Washington, the Columbia Gorge, and the Willamette Valley of Oregon. In the summer of 1922, and for the next seven years, Bretz conducted field research of the Columbia River Plateau. He had been interested in unusual erosion features in the area since 1910 after seeing a newly published topographic map of the Potho

    As the depth of the water in Lake Missoula increased, the pressure at the bottom of the ice dam increased enough to lower the freezing point of water below the temperature of the ice forming the dam. This allowed liquid water to seep into minuscule cracks present in the ice dam. Over a period of time, the friction from water flowing through these cracks generated enough heat to melt the ice walls and enlarge the cracks. This allowed more water to flow through the cracks, generating more heat, al

    As the water emerged from the Columbia River gorge, it backed up again at the 1 mile wide narrows near Kalama, Washington. Some temporary lakes rose to an elevation of more than 400 ft, flooding the Willamette Valley to Eugene, Oregon and beyond. Iceberg rafted glacial erratics and erosion features are evidence of these events. Lake-bottom sediments deposited by the floods have contributed to the agricultural richness of the Willamette and Columbia Valleys. Glacial deposits overlaid with centuri

    • Between 15,000 and 13,000 years ago
  10. Missoula PaddleHeads - Wikipedia

    en.wikipedia.org/wiki/Missoula_PaddleHeads

    From Wikipedia, the free encyclopedia The Missoula PaddleHeads are an independent baseball team of the Pioneer League, which is not affiliated with Major League Baseball (MLB) but is an MLB Partner League. They are located in Missoula, Montana, and play their home games at Ogren Park at Allegiance Field.

    • Independent (from 2021)
    • TBD
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