Calumet Hotel | |
The Calumet Hotel from the northwest | |
Location | 104 W. Main St., Pipestone, Minnesota |
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Coordinates | 44°0′1″N96°19′4″W / 44.00028°N 96.31778°W Coordinates: 44°0′1″N96°19′4″W / 44.00028°N 96.31778°W |
Area | less than one acre |
Built | 1888 |
Architect | Smith,C.; Frost,William |
Architectural style | Richardsonian Romanesque |
Part of | Pipestone Commercial Historic District (#77000761) |
MPS | Pipestone County MRA (AD) |
NRHP reference # | 76001066 [1] |
Added to NRHP | March 16, 1976 |
The Calumet Hotel, also known as the Calumet Inn, anchors the historic district of downtown Pipestone, Minnesota, United States. The three-story Richardsonian Romanesque hotel was built with light pink jasper quartzite as opposed to the red Sioux quartzite used in most other downtown buildings. The present hotel was built to replace a previous hotel, also three-stories, which was destroyed in an 1886 fire. [2]
Pipestone is a city in Minnesota, United States, and the county seat of Pipestone County. The population was 4,317 at the 2010 census. The city is also the site of the Pipestone National Monument.
Richardsonian Romanesque is a style of Romanesque Revival architecture named after architect Henry Hobson Richardson (1838–1886), whose masterpiece is Trinity Church, Boston (1872–1877), designated a National Historic Landmark. Richardson first used elements of the style in his Buffalo State Asylum for the Insane in Buffalo, New York, designed in 1870.
Quartzite is a hard, non-foliated metamorphic rock which was originally pure quartz sandstone. Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of iron oxide (Fe2O3). Other colors, such as yellow, green, blue and orange, are due to other minerals.
Like its predecessor, the Calumet Hotel was built to meet a demand which was growing as a result of increased railroad traffic. It opened on Thanksgiving Day, 1888 with a guest capacity of 50. It has been enlarged twice, a three-story addition to the south in 1899 differentiated by round rather than square window caps, and fourth story built in 1913, bringing the total number of rooms to 90. Among the various businesses to occupy the first floor and basement of the building were First National Bank and a 14-hole miniature golf course. A fire in 1944 destroyed the floors in the south section, but the hotel was able to reopen the following April. By 1978 had declined to the point that it was condemned by the State Fire Marshall. After two years of thorough renovation the hotel was again able to open for business. [2]
Miniature golf, also known as minigolf, crazy golf, or putt-putt, is an offshoot of the sport of golf focusing solely on the putting aspect of its parent game. It is played on courses consisting of a series of holes similar to its parent, but characterized by their short length.
Architectural details include the oriel window, a replica of the original which was removed along with the balcony in 1912, a large quartzite arch, the corner door, and a crenelated cornice. [2]
An oriel window is a form of bay window which protrudes from the main wall of a building but does not reach to the ground. Supported by corbels, brackets, or similar, an oriel window is most commonly found projecting from an upper floor but is also sometimes used on the ground floor.
Hotel Hell covered the hotel in an episode of the series, broadcast on August 18, 2014, on the U.S. Fox television network. [3]
Hotel Hell is an American reality television series created, hosted and narrated by Gordon Ramsay, which ran on the Fox network for three seasons from 2012 to 2016. It aired on Monday nights at 8 pm ET/PT. It was Ramsay's fourth series for the Fox network.
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The Sioux Quartzite is a Proterozoic quartzite that is found in the region around the intersection of Minnesota, South Dakota, and Iowa, and correlates with other rock units throughout the upper midwestern and southwestern United States. It was formed by braided river deposits, and its correlative units are thought to possibly define a large sedimentary wedge that once covered the passive margin on the then-southern side of the North American craton. In human history, it provided the catlinite, or pipestone, that was used by the Plains Indians to carve ceremonial pipes. With the arrival of Europeans, it was heavily quarried for building stone, and was used in many prominent structures in Sioux Falls, South Dakota and shipped to construction sites around the Midwest. Sioux Quartzite has been and continues to be quarried in Jasper, Minnesota at the Jasper Stone Company and Quarry, which itself was posted to the National Register of Historic Places on January 5, 1978. Jasper, Minnesota contains many turn-of-the-century quartzite buildings, including the school, churches and several other public and private structures, mostly abandoned.
This is a list of the National Register of Historic Places listings in Pipestone County, Minnesota. It is intended to be a complete list of the properties and districts on the National Register of Historic Places in Pipestone County, Minnesota, United States. The locations of National Register properties and districts for which the latitude and longitude coordinates are included below, may be seen in an online map.
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