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The Clark Fork River Operable Unit. The Milltown Reservoir Sediments Superfund Site is a major Superfund site in Missoula County, Montana, seven miles east of Missoula. It was added to the National Priorities List in 1983 when arsenic groundwater contamination was found in the Milltown area. The contamination resulted from a massive flood three ...
When Higgins was forced to resign as bank president in 1888, the next two presidents also resigned after five and six months respectively. [6] Marcus Daly then became president with Hammond as vice president and Keith as Cashier. [7] Hammond became president of the bank in 1893 and renamed it the First National Bank of Missoula. [6]
The settlement was moved four miles east to the location of today's Downtown Missoula in 1865 and renamed Missoula Mills. In 1873, Higgins organized the Missoula National Bank as one of the first banks in Montana Territory and located it next to his and Worden's store built two years earlier and now called the Worden & Company Store.
The rivers around Missoula provide nesting habitats for bank swallows, northern rough-winged swallows, and belted kingfishers. Killdeer and spotted sandpipers can be seen foraging for insects along the gravel bars. Other species include song sparrows, catbirds, several species of warblers, and the pileated woodpecker.
She’s not worried about the new Starbucks slated to arrive in Two Rivers by the end of 2024. The sign for The High Lift Coffee Shop as seen, Thursday, January 25, 2024, in Two Rivers, Wis.
Cut Bank Pioneer Press - Cut Bank; ... Powder River Examiner - Broadus; ... The Daily Missoulian - Missoula (1904–1961) [1] See also
The rivers around Missoula provide nesting habitats for bank swallows, northern rough-winged swallows and belted kingfishers. Killdeer and spotted sandpipers can be seen foraging insects along the gravel bars. Other species include song sparrows, catbirds, several species of warblers, and the pileated woodpecker.
A cut bank, also known as a river cliff or river-cut cliff, is the outside bank of a curve in a water channel , which is continually undergoing erosion. [1] Cut banks are found in abundance along mature or meandering streams, they are located opposite the slip-off slope on the inside of the stream meander.