Leavenworth, Washington

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Leavenworth
City
Leavenworth's main street reflects its modelling on a Bavarian village
Location of Leavenworth, Washington
Coordinates: 47°35′47″N 120°39′55″W / 47.59639°N 120.66528°W / 47.59639; -120.66528Coordinates: 47°35′47″N 120°39′55″W / 47.59639°N 120.66528°W / 47.59639; -120.66528
Country	United States
State	Washington
County	Chelan
Established	1885
Incorporated	September 5, 1906
Government
• Mayor	Carl Florea[1]
Area [2]
• Total	1.47 sq mi (3.81 km2)
• Land	1.45 sq mi (3.76 km2)
• Water	0.02 sq mi (0.05 km2)
Elevation	1,171 ft (357 m)
Population  (2010)[4]
• Total	1,965
• Estimate  (2019)[3]	2,029
• Density	1,396.42/sq mi (539.20/km2)
Time zone	UTC-8 (PST)
• Summer (DST)	UTC-7 (PDT)
ZIP code	98826
Area code	509
FIPS code	53-38845
GNIS feature ID	1521981[5]
Website	City of Leavenworth

Leavenworth is a city in Chelan County, Washington, United States. It is part of the Wenatchee−East Wenatchee Metropolitan Statistical Area. The population was 1,965 at the 2010 census.^[6] The entire town center is modeled on a Bavarian village as part of a civic initiative that began in the 1960s. The area is a major, four-season tourist destination with festivals nearly every month and a multitude of events year round.

History[]

The construction of the Great Northern Railway through Tumwater Canyon in 1892 brought settlers to a townsite that was named "Leavenworth". Lafayette Lamb arrived in 1903 from Clinton, Iowa, to build the second largest sawmill in Washington state.

Leavenworth was officially incorporated on September 5, 1906. A small timber community, it became a regional office of the Great Northern Railway in the early 1900s. The railroad relocated to Wenatchee in 1925, greatly affecting Leavenworth's economy. The city's population declined well into the 1950s as the lumber mills closed and stores relocated.^[7]

The city looked to tourism and recreation as a major economy as early as 1929, when they opened a ski jump.^[8] In 1962, the Project LIFE (Leavenworth Improvement For Everyone) Committee was formed in partnership with the University of Washington to investigate strategies to revitalize the struggling logging town. The theme town idea was created by two Seattle businessmen, Ted Price and Bob Rodgers, who had bought a failing cafe on Highway 2 in 1960.^[9] Price was chair of the Project LIFE tourism subcommittee, and in 1965 the pair led a trip to a Danish-themed town, Solvang, California, to build support for the idea. The first building to be remodeled in the Bavarian style was the Chikamin Hotel, which owner LaVerne Peterson^[10] renamed the Edelweiss after the state flower of Bavaria.^[11][12]

Leavenworth is home to the Leavenworth Nutcracker Museum, which opened in 1995 and contains more than 5,000 nutcrackers dating from prehistoric to modern.^[13] Leavenworth hosts an annual Oktoberfest celebration.^[14] Leavenworth's transformation into a theme town was inspired, and assisted, by Solvang, California. Later, the Washington town of Winthrop followed Leavenworth's example and adopted a Western town theme.^[15]

In November 2007, Good Morning America went to Leavenworth for Holiday Gifts for the Globe where GMA helped light up the town for the Christmas Holiday. Leavenworth was named the Ultimate Holiday Town USA by A&E Network.^[16]

Geography[]

Bavarian Ritz Hotel

Downtown Leavenworth, 1,500 feet (460 m) below, as viewed from the adjacent Tumwater Mountain on an August afternoon

According to the United States Census Bureau, the city has a total area of 1.25 square miles (3.24 km²), of which, 1.23 square miles (3.19 km²) is land and 0.02 square miles (0.05 km²) is water.^[17]

Geology[]

Leavenworth sits on the southeast side of the North Cascades collage, which is a group of terranes that accreted to North America all about the same time. Marine fossils indicate that the terranes were probably a group of islands originating in the South Pacific hundreds of million years ago. The terranes arrived at North America about 90 million years ago in the middle of the Cretaceous period. When they smashed into their new home, they were a puzzle of north–south slices. As accretion continued, they were cut into horizontal (east-west) slices.

During the Eocene epoch, about 50 million years ago, the area was once again cut into vertical slices, creating among others, the Leavenworth fault and the Entiat fault. In between these two faults the Chiwaukum graben was created. This graben is about 12 miles wide and trends northwest from Wenatchee for about 50 miles. As the graben dropped, it began to fill with clastic sediment from the surrounding hills, creating the Chumstick formation. About 30 million years ago in the Oligocene epoch, the Chiwaukum graben underwent compressional deformation creating several folds in the region that are visible today. Leavenworth is on the western edge of the graben; in fact, the Leavenworth fault runs through the western edge of town. The area to the west and southwest of Leavenworth was created in the middle Cretaceous period with the uplift of the Mt. Stuart batholith, forming the granite rock seen today in Icicle Ridge and .

During the Pleistocene and into the Holocene epochs, an alpine glacier originating from the southwest in the Mount Stuart range made its way to where the town is today. Leavenworth sits on the terminal moraine of that glacier. The residential parts of town display many glacial erratics that originated 20 miles up the Icicle Valley near Mount Stuart.

About 19,000 years ago, a large rock slide dammed the Columbia River near Rock Island, just south of Wenatchee. The temporary dam, in conjunction with one of the Lake Missoula floods, caused the water to flow back up the Wenatchee Valley, where it was stopped by the glacier at Leavenworth. As the leading edge of the glacier interacted with the flood, ice rafts formed carrying granite erratics from the Stuart batholith, which ended up in the town of Dryden about 15 miles down the valley from Leavenworth. As the glacier retreated, the south side of Leavenworth was a lake dammed up by the moraine. The bridge on the east side of town is a good vantage point to see where the Wenatchee River cuts through the moraine today.

Climate[]

Leavenworth has a continental Mediterranean climate (Köppen Dsb) with summers characterized by hot, sunny days and chilly nights, and cold, snowy winters.

During the summer, the weather is typically anticyclonic due to the presence of the North Pacific anticyclone, with resultant clear skies and large diurnal temperature ranges. Rainfall is limited by the Cascade rain shadow as well as by the anticyclone, and all months from May to October have recorded zero precipitation on occasions, including 114 consecutive days without precipitation from June to October 2003. When a continental flow enters the Columbia Basin, the temperature can be very hot during the day, with the hottest temperature being 110 °F or 43.3 °C during the heatwave of July 1941. However, on cooler, stiller days, summer nights can still be cold and frosts have been recorded as early as August 29 in 1980.

The fall months have steady cooling and a gradual increase in the frequency of frontal storms producing rainfall, whilst winter weather is typically cold and snowy, with an annual mean snowfall of 90.1 inches or 2.29 metres and a maximum monthly total of 92.3 inches (2.34 m) recorded in December 1996. The snowiest season has been from July 1968 to June 1969 with 217.2 inches (5.52 m) and the least snowy from July 1962 to June 1963 when just 19.4 inches (0.49 m) of snow fell. The lowest temperature recorded in Leavenworth was −36 °F (−37.8 °C) on December 30, 1968, but typically five mornings per year will fall at or below 0 °F or −17.8 °C.

The wettest "rain year" was recorded from July 1955 to June 1956 with a total of 41.13 inches (1,044.7 mm) and the driest was from July 1929 to June 1930 with 11.77 inches (299.0 mm). The spring months see gradual warming and drying, though frosts remain frequent well into the start of April. During an average year, over 168 mornings see temperatures fall to freezing or below. May 16 is the average date of last freeze; 2016 was the first year to record a last frost in March.

Demographics[]

As of the 2010 U.S. Census,^[4] there were 1,965 people, 908 households, and 500 families residing in the city. The population density was about 1,598 inhabitants per square mile (617.0/km²). There were 1,241 housing units at an average density of about 1,009 per square mile (389.6/km²). The racial makeup of the city was 92.9% White, 0.4% Black, 0.5% Native American, 0.6% Asian, 0.2% Pacific Islander, 3.9% from other races, and 1.6% from two or more races. Hispanic or Latino of any race were 10.8% of the population.

There were 908 households, of which about 24% had children under the age of 18 living with them, about 42% were married couples living together, about 10% had a female householder with no husband present, 3% had a male householder with no wife present, and about 45% were non-families. About 37% of all households were made up of individuals, and about 20% had someone living alone who was 65 years of age or older. The average household size was 2.16 and the average family size was 2.84.

The median age in the city was about 42 years. About 20% of residents were under the age of 18; about 8% were between the ages of 18 and 24; 25% were from 25 to 44; about 27% were from 45 to 64; and about 20% were 65 years of age or older. The gender makeup of the city was 46.7% male and 53.3% female.

Education[]

Public schools in Leavenworth and the surrounding area are operated by the Cascade School District, which has over 1,300 students.^[22] The district has one high school, located in Leavenworth, that was rebuilt in 2019.^[23]

Leavenworth is home to the Upper Valley Christian School, which is a private, K-12 school operated by the Leavenworth Church of the Nazarene.

Infrastructure[]

Transportation[]

Leavenworth is located on U.S. Route 2, which continues west across Stevens Pass to Snohomish County and east towards Wenatchee.^[24] The Chumstick Highway, formerly known as State Route 209, travels north from Leavenworth to Plain and Lake Wenatchee State Park.

The city is served by Amtrak's Empire Builder train, which stops daily at Icicle Station near downtown.^[24] Link Transit provides local and inter-city public transit services that connect Leavenworth to Wenatchee, as well as local paratransit and a downtown shuttle.^[25] The city also has several private taxi companies and inter-city bus operators, including stops for Northwestern Trailways and Amtrak Thruway Motorcoach.^[26]

See also[]

• Tudorbethan architecture
• Helen, Georgia
• Frankenmuth, Michigan
• Solvang, California

References[]

Further reading[]

• Generalized geologic map of the Chelan 1:100,000 quadrangle
• Swauk Formation (Caroline J. Cloudas, 1998)
• Field Trip Guide: Geology and Art
• Chiwaukum Schist in the Nason Terrane (Jessy Ryan)
• A geological trip along Snoqualmie, Swauk, and Stevens Pass Highways. Washington state geology department, 1963
• Northwest Exposures. David Alt and Donald W. Hyndman
• Roadside Geology of Washington. David Alt and Donald W. Hyndman
• Genealogy of Chelan County. Wayne and Linda McGahuey

External links[]

Wikimedia Commons has media related to Leavenworth, Washington.

• Leavenworth, Washington travel guide from Wikivoyage
• City of Leavenworth website
• Leavenworth Chamber of Commerce
• Leavenworth, Washington at Curlie