Car audio kennewick wa
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It is located along the southwest bank of the Columbia River , just southeast of the confluence of the Columbia and Yakima rivers and across from the confluence of the Columbia and Snake rivers.
It is the most populous of the three cities collectively referred to as the Tri-Cities the others being Pasco and Richland. The population was 73, at the census ; the Census Bureau estimates the city's population to be 84, as of July 1, [update]. The discovery of Kennewick Man along the banks of the Columbia River provides evidence of Native Americans ' settlement of the area for at least 9, years.
The construction of the Hanford Site at Richland accelerated the city's growth in the s as workers from around the country came to participate in the Manhattan Project. While Hanford and Pacific Northwest National Laboratory continue to be major sources of employment, [10] the city's economy has diversified over time and Kennewick today hosts offices for Amazon and Lamb Weston.
Native Americans populated the area around modern-day Kennewick for millennia before being discovered and settled by European descendants. Kennewick's low elevation helped to moderate winter temperatures. On top of this, the riverside location made salmon and other river fish easily accessible. By the 19th century, people lived in and between two major camps in the area. Lewis and Clark noted that there were many people living in the area when they passed through in and These had approximate populations of 2, and 3, respectively.
There are conflicting stories on how Kennewick gained its name, but these narratives attribute it to the Native Americans living in the area. Some reports claim that the name comes from a native word meaning "grassy place". In the past, Kennewick has also been known by other names. The area was known as Tehe from to , and this name appears on early letters sent to the area with the city listed as Tehe, Washington.
Ainsworth became the first non-Native settlement in the area—where U. Route 12 now crosses the Snake River between Pasco and Burbank. Some Ainsworth residents would commute to what is now Kennewick via small boats for work. All that remains of Ainsworth is a marker placed by the Washington State Department of Transportation near the site.
During the s, steamboats and railroads connected what would become known as Kennewick to the other settlements along the Columbia River. That bridge could not endure the winter ice on the Columbia and was partially swept away in the first winter. A new, more permanent bridge was built in its place in It was around this time that a town plan was first laid out, centered around the needs of the railroad. A school was constructed using donated funds, but this burned soon after it was finished.
This initial boom only lasted briefly, as most of the people who came to Kennewick left after the bridge was finished. In the s, the Northern Pacific Irrigation Company installed pumps and ditches to bring water for agriculture into the Kennewick Highlands. Once there was a reliable water source, orchards and vineyards were planted all over the Kennewick area.
Strawberries were another successful crop. Kennewick was officially incorporated on February 5, There have been other unsuccessful attempts to make this move throughout the city's history, most recently in City residents hoped to capitalize on this new infrastructure by forming the Port of Kennewick, making the city an inland seaport. Freight and passenger ship traffic began that same year. The port also developed rail facilities in the area. This bridge connected the two cities by vehicle traffic for the first time.
Like many other agricultural communities, the Great Depression had an impact in Kennewick. Despite lowered prices for crops grown in the region, the city continued to experience growth, gaining another people during the s.
Growth was aided by federal projects that improved the Columbia River. Grand Coulee Dam , located upstream of Kennewick, fostered irrigation across the Columbia Basin north of Pasco, sending more raw material through Kennewick. In , the United States opened the Hanford nuclear site in and north of Richland. Its purpose originally was to help produce nuclear weaponry, which the US was trying to develop.
People came from across the United States to work at Hanford, who were unaware of what they were actually producing. They were only told that their work would help the war effort.
The plutonium refined at the Hanford Site was used in the Fat Man bomb, which was dropped in Nagasaki in in the decisive final blow of the war. As the Hanford Site's purpose has evolved, there has continually been a tremendous influence from the site on the workforce and economy of Kennewick.
From to , the population of Richland grew from residents to 21, residents, while Pasco gained from 3, to 10,, and Kennewick increased from 1, to 10, An effort to build a new bridge began in and was funded in The two-lane Green Bridge was the only one for automobiles across the Columbia River in the Tri-Cities at the time, and the 10, cars crossing it daily had created traffic problems.
A new four-lane divided highway bridge, dubbed the Blue Bridge , opened in less than 2 miles 3. However, demolishing the Green Bridge proved to be controversial. Those seeking to preserve the bridge for historical reasons were able to stall the demolition, but it was eventually torn down in Racial discrimination against African Americans was common in Kennewick before the civil rights movement.
The city had been a sundown town , which required African Americans to be out of the city after nightfall. The only place they could live in the Tri-Cities at the time was east Pasco. Even during the day, African Americans would experience harassment by the general public and police. In the s, covenants restricted African Americans from owning property in the city.
After the U. Supreme Court ruled in Shelley v. Kraemer that racially restrictive covenants could not be enforced in state courts, these were replaced by informal agreements between homeowners and realtors to refuse to sell to African Americans.
The eruption of Mount St. Helens caused several inches of volcanic ash to fall on Kennewick. Higher accumulations were recorded in Yakima and Ritzville , but the ash plume was thick enough to trigger street lamps to turn on at noon. Cars that didn't have external filters stopped functioning during the eruption, and it took several months to completely clean all the ash.
Helens since. The s also brought the two most serious attempts to merge Kennewick with the other cities in the Tri-Cities, both of which failed. This resulted from an economic down turn in the area caused by the cancellation of two proposed nuclear power plants on the Hanford Site. The first proposal was to consolidate all three cities Kennewick, Pasco, and Richland into one, while the second only included Kennewick and Richland.
Support for both of these attempts was strong in Richland, but voters in Kennewick and Pasco were not on board. The Toyota Center was used as a venue for ice hockey and figure skating during the Goodwill Games.
Most of the events were held in the host city, Seattle , but were also staged in other areas of the state, including Tacoma and Spokane. In , an ancient human skeleton was found on a bank of the Columbia River. Known as Kennewick Man , the remains are notable for their age some 9, years. Ownership of the bones has been a matter of controversy with Native American tribes in the Inland Northwest claiming the bones to be from an ancestor of theirs and wanting them to be reburied.
After a court litigation, a group of researchers were allowed to study the remains and perform various tests and analyses. They published their results in a book in A genetic analysis confirmed the ancient skeleton's ancestry to the Native Americans of the area some observers contended that the remains were of European origin.
The genetic analysis has notably contributed to knowledge about the peopling of the Americas. Kennewick fared better than most of the state during the Great Recession , primarily due to consistent job growth in the metro area during that time. This was largely driven by the Hanford Site, which only had one significant period of layoffs which briefly caused economic uncertainty.
Home sales experienced a small decline from to , but rebounded in While growth has been experienced throughout the city, new development has been strongest in the Southridge area along U. Route US and in the west part of the city thanks to their access to major roads and the ample land available in those areas when development started.
Kennewick is located in Eastern Washington along the south side of the Columbia River and is one of three cities in the Tri-Cities. The other two cities are Richland, which is upstream of Kennewick on the same side of the river, and Pasco, which is across the river.
The elevation within the city rises from the river to a line of ridges on the south side of town that are a result of the same anticline that created Badger Mountain and Rattlesnake Mountain. The city overlies basalt laid down by the Columbia River Basalt Group , which was a type of volcanic eruption known as a flood basalt. This erupted from fissures that were geographically spread throughout eastern Washington, eastern Oregon, and far western Idaho.
Most of the lava erupted between 17 and 14 million years ago, with smaller eruptions lasting as late as 6 million years ago. While outcroppings from the basalt flows can be seen throughout Kennewick, they are mostly buried by sediments. The first major sediment deposit following the eruptions is the Ringold Formation , which was placed by the Columbia River between 8 and 3 million years ago.
Further deposition came as a result of the Missoula Floods. The pressure from the resulting lake would periodically build to the point that the dam would fail, sending massive amounts of water cascading to the Pacific Ocean.
This abrupt halt in flow allowed the floodwater to drop a significant amount of sediment before passing through Wallula Gap toward Hermiston. During the largest floods, the water's surface reached 1, feet m above sea level. This completely covered all of the land within Kennewick's city limits. Earthquakes are a hazard in Kennewick, though not to the same extent or frequency as areas west of the Cascade Range like the Puget Sound Region.
The entire Pacific Northwest is threatened with subduction zone earthquakes that can exceed magnitudes of 9 on the moment magnitude scale. These subduction zone earthquakes will be centered on the boundary between the North American Plate and the Juan de Fuca Plate , which is located offshore. While these are weaker, they can still cause damage.

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