| Tillamook’s Water History
The
original diversion of Fawcett Creek began prior to the turn of the 20th
century by a private company. In 1895, the City of Tillamook took over
the Fawcett Creek supply.
In 1905,
the Tillamook Water Commission was chartered. Five years later,
diversion of Killam Creek began. Wood stave pipe was used to transport
water from each creek intake into town. In the 1920s, diversion dams
and 200,000-gallon impoundments were constructed at each intake. The
low dam structures divert a portion of the creek flows into the
impoundments, which provide settling prior to the water entering the
screened concrete intakes.
In order to
supplement the flows of Fawcett Creek, Skookum Reservoir was
constructed in 1965, three miles upstream of the intake. The
700-acre-foot impoundment has a 37-foot-high earth-fill dam and a
concrete spillway. The drainage area to the impoundment is
approximately 2.2 square miles or 1,408 acres. Water is collected in
the reservoir during the rainy months and released during the summer
via a slide gate over the outlet pipe at the bottom of the dam.
In 1994, a
2-million-gallons-per-day package filtration plant was completed that
allows the city to treat, disinfect and store the surface water prior
to delivering it to town. Treated water is then stored in 3 million
gallons of on-site storage. This provides adequate chlorine contact
time and reserve capacity.
From the
water treatment plant site, water flows by gravity to the city limits
through six miles of parallel transmission mains. The original wood
stave pipes were replaced with steel between 1937 and 1959. In 1994, a
24-inch iron main was constructed to replace old lines. It extends from
the reservoirs to the old chlorination building site located south of
town just off South Prairie Road. That site today is the location of a
pump station that delivers water to Pleasant Valley.
Starting in
the late 1950s, efforts were made to supplement the surface water with
groundwater. In 1958, the first well, known now as Well No. 1, was
drilled. It is located two miles south of town just northeast of the
Highway 101 bridge over the Trask River. A second well was drilled in
1960 on Gienger Road, about 1.5 miles south of town. Both wells have
high iron content and are not used for household water.
Beginning
in 1980, efforts to develop an alternate groundwater supply began.
Drilling focused on the east side of town, where wells of proven
quality existed. In 1981, a well was drilled on the southwest corner of
the East Elementary School property just east of Maple Street and
Williams Avenue. It is now known as Well No. 2. Another well, Well No.
3., was completed at the Junior High School in 1993. |