Effective wastewater planning
requires knowledge of the physical setting as well as the social
environment of the area to be served. To address this need, this chapter
provides a summary of the basic characteristics of the planning area.
The information is organized into four sections.
§
The planning area
definition establishes the service area boundary for a 20-year planning
horizon and presents considerations for long-term planning.
§
The physical
environment section includes descriptions of the study area geography,
geology, climate, air quality and wildlife habitat.
§
The water resources
discussion provides an overview of key surface and groundwater features
in the planning area.
§
The human environment
section summarizes the area's land use, economic activity, historical
population trends, and governmental structure.
The planning area for this
facilities plan consists of two land masses: one located in North
Spokane and one located in the Spokane Valley (see
Drawing 2-1. Planning Area.
The North Spokane section is bounded on the west, north and east by the
Draft Urban Growth Area (Draft UGA) boundary for the greater Spokane
area. On the south, the boundary is established by the City/County
Sewer Service Boundary. The North Spokane section has an area of 8,539
acres and includes the following urban planning areas: Mead, North
Metro 1, North Metro 2 and North Metro 3.
The Spokane Valley section is
bounded on the north and south by the Draft UGA boundary for the greater
Spokane area and on the east by the boundary for Liberty Lake Sewer and
Water District No. 1. The west boundary is generally defined by the
City/County Sewer Service Boundary. The Spokane Valley section has an
area of 31,103 acres and includes the following urban planning areas:
Northwest Valley, Northeast Valley, East Valley and West Valley. It
also includes the Town of Millwood.
The definition of the Draft UGA
boundary is driven by the Growth Management Act (GMA), which provides a
framework for managing growth and land use development, and coordinating
these with infrastructure planning. The UGA defines an area sufficient
to provide housing, facilities, and services for projected growth
through 2020. This boundary, shown in
Drawing 2-1,
was established as part of the
County’s on-going long-range planning, and has yet to be approved by the
Spokane County Board of County Commissioners. If approved, it will
supersede the Interim Urban Growth Area (IUGA) that was adopted in 1997.
In general, urban development is
encouraged within the UGA and discouraged outside the UGA.
Consequently, the GMA requires that the principal planning agencies
within each County allocate the majority of planned growth to the area
within the UGA. To support urban land use densities, municipal services
are required to be provided within the UGA and should be limited outside
the UGA. The major impact of the GMA on wastewater management is that a
facilities plan must demonstrate that adequate wastewater facilities and
capacity will be provided to support the planned level of growth
In addition to the 20-year planning
horizon, this facilities plan will project growth and provide a cursory
examination of wastewater management requirements for a longer (50-year)
planning horizon. Because this is a longer planning horizon than the GMA
requires public agencies to consider, a 50-year planning area has not
been designated. However, it is assumed that only areas contiguous with
the Draft UGA will be served in the future by the County’s wastewater
program.
Since the early 1980s, Spokane
County has been implementing a sewer construction program to eliminate
septic tanks and reduce on-site wastewater disposal above the Spokane
Valley-Rathdrum Prairie Aquifer. To guide these efforts, an Aquifer
Sensitive Area (ASA) was designated to identify locations where on-site
disposal practices could have significant potential to adversely impact
water quality in the aquifer. To prioritize the sewer construction
program, Spokane County worked with State and local health departments
to establish a Priority Sewer Service Area (PSSA). Both the ASA and
PSSA boundaries are shown in
Drawing 2-1.
In the 1996 CWMP, Spokane County
identified a phased sewer construction program within the PSSA, to be
implemented in five-year blocks, reaching completion in 2015.
Drawing 2-2. North Sewer
Priority Areas, and
Drawing 2-3. Valley Sewer Priority Areas
show the phased capital improvement
programs for the North Spokane and Valley planning areas, respectively.
In developing planning projections
for wastewater facilities, it has been assumed that sewers will be
extended to serve the entire Spokane County planning area by 2020. With
the adoption of an UGA Boundary, the PSSA Boundary will no longer exist.
Chapter 3 presents assumptions
regarding extension of service to areas outside the Draft UGA boundary
between 2020 and 2050.
Physical characteristics of the
planning area affect wastewater generation rates by shaping the nature
and pattern of land use, as well as the location and density of
population. The physical environment also affects the location and
design of facilities for conveyance, treatment and disposal or reuse of
wastewater. Local geology, soils, and seismicity affect cost of laying
pipe and siting of treatment systems. Similarly, climate affects choice
of wastewater treatment processes, determines seasonal operating
conditions, and dictates the amount of stormwater runoff generated.
Spokane County is located in northeastern Washington adjacent to the Idaho
border. The County has an array of landscapes ranging from the
mountainous area in the northeast, including Mount Spokane, to the
semiarid basalt plains in the southwest. Between these extremes are the
rolling wheat lands of the Palouse area, the channeled scablands created
by the glacial floods, and the Spokane metropolitan area
[i].
The total County area is approximately 1,760 square miles.
The County’s wastewater planning area is located directly over the Spokane
Valley-Rathdrum Prairie Aquifer, along the Spokane and Little Spokane
Rivers. The principal drainage features within the County are the
Spokane River, Little Spokane River, and Latah Creek.
Drawing 2-4. Surface and Ground
Water Sources shows the major waterways within Spokane
County.
The planning area is nearly all
urban landscape with flat to moderately rolling topography. Elevations
within the planning area range from 1,700 feet above mean sea level
along the Spokane River to 2,300 feet above sea level along the outer
edges of the valley.
Geology
The structural features of the
Spokane Valley are the result of a complex sequence of intense folding
and faulting. Geologic structures within the planning area fall into
two units based on their permeability. The consolidated Precambrian and
Tertiary rocks, composing one unit, are relatively impermeable and allow
delineation of the bottom and the sides of the valley. Unconsolidated
Quaternary deposits compose the second unit and define the extent and
thickness of the valley fill. This unit consists mainly of poorly
sorted, reworked, glaciofluvial deposits of sand and gravel.
Soils
The planning area follows the
Spokane River, resulting in level to gently sloping topography and
consistent soil types. The soils of this area consist of the Garrison
Marble-Springdale soil association, which is excessively drained sandy
and gravelly soils formed in glacial outwash. The soils within the
planning area are very porous in nature with a rapid water-intake rate
and low water-holding capacity. These soils also have moderate
resistance to erosion, high shear strength, and high load-carrying
capacity. The high level of permeability is a concern for aquifer
health, which is located directly under the planning area
[ii].
Soils characteristics in other parts
of the County outside of the planning area may be relevant to some
wastewater management alternatives. These characteristics are described
below.
§
The southwestern part
of the County consists of a broad basalt plateau. Only small remnants
of pre-glacial soils, characterized by deep to shallow, gravelly or
rocky soils with moderate permeability and low water-holding capacity,
remain from the glacial floods.
§
The southeastern part
of the County is described by rolling to hilly topography with deep
soils that formed from wind deposits of silty material. The soils are
characterized as medium to fine-textured soils with moderate to slow
permeability and high to moderate water-holding capacity. Basalt is the
most prominent geologic formation with quartzite, shale, and sandstone
also found in the region. The area consists of rolling loessal uplands,
glacial till plains, and mountain foot slopes.
§
The Okanogan Highlands
makes up the northern part of the County and consists of mountains, foot
slopes, glaciated valleys, broad glacial lake terraces, and outwash
terraces. Soils in the eastern area are characteristically deep,
medium-textured soils of the hilly and mountainous areas with moderately
rapid permeability and moderate water-holding capacity. Soils in the
northwest consist of gravelly and sandy soils with rapid permeability
and moderate water-holding capacity that formed in glacial materials.
Geologic
Hazards
Geologically hazardous areas are
susceptible to earthquakes, erosion, landslides, or other geologic
events. Typically, they are not suited for commercial, residential or
industrial development without mitigation. Geologic hazards are
categorized as critical and sensitive areas under the Critical Areas
Ordinance described later in this chapter.
Drawing 2-5. Geologic Hazards and Constraints
shows the geologic
hazards and constraints including erodible soils, alluvium, landslide
deposits, and Latah formation i. This Drawing shows that geologic hazards
inside the planning area are minimal, with some small areas of erodible
soils.
Seismicity.
Spokane County is in a region with a
moderate risk of seismic activity. The Uniform Building Code classifies
the area as Seismic Zone 2B.
Erosion.
Spokane County defines erodible soils as those soil associations
which have been found to have severe potential
of erosion according to the U.S. Soil Conservation Service and/or which
have a slope of 30 percent or greater. There are a few small areas of
erodible soils located along the planning area border, primarily
northwest of Mica Peak, east of Millwood, and in the northern portion of
the North Spokane service area. Erodible soil types are found primarily
in the northeastern and southeastern portions of the County. Small
areas with these characteristics can also be found northeast and
southeast of the City of Spokane, north and west of the City of Cheney,
and west of the City of Medical Lake.
Landslide.
Landslide hazard areas have been defined by areas with a history of
landslide deposits, Alluvium, or the Latah formation. Landslide hazard
areas are primarily located in pockets in the northern and central
portions of the County. These areas are associated with the Little
Spokane River and with the foothills and mountainous areas north of the
City of Spokane. Small areas are also present north and west of the City
of Cheney. There are no Latah formations within the planning area
boundaries; however, landslide deposits are found in a few areas
bordering the planning area.
The planning area's location on the
western flank of the Rocky Mountains gives the area a temperate
climate. Summer is mostly warm and dry, interspersed with a few cool,
damp days. Winter weather is often damp and foggy, with below-freezing
temperatures, characteristic of maritime Polar air mass. Generally, the
prime growing season is from mid-April to mid-October.
Annual precipitation in Spokane
County ranges from less than 15 inches in the semiarid western edge of
the County to more than 25 inches in the hills and mountains on the east
side of the County. The annual precipitation in the planning area is
approximately 17 to 21 inches i. Figure 2‑1 presents normal monthly temperature and
precipitation for the planning area (data taken from a USGS gauging
station east of the Spokane International Airport).

Figure
2‑1.
Spokane County Planning Area Average Monthly Temperature and
Precipitation
Several conditions contribute to air pollution in Spokane County. Human
activities, including automobile use, wood stove use, industrial
facilities and agricultural operations, generate airborne substances
that can affect air quality. Furthermore, Spokane has been affected
substantially by windblown dust from the central portion of the State.
The Spokane Valley is a natural basin in which air pollution
occasionally is concentrated by temperature inversions (a
situation in which lighter warm air overlies heavier cool air).
According to the Spokane County Air Pollution Control Agency, significant
air quality problems in Spokane County are limited to particulates (PM10)
and carbon monoxide (CO)
[iii].
PM10
refers to small airborne particles (e.g., smoke and dust), while CO is a
product of incomplete combustion. A nonattainment area for each of
these sources of air pollution has been designated in the Spokane
Metropolitan Area. See
Drawing 2-6. Air Quality Areas
for a summary of air quality concerns.
A variety of air pollution control
strategies have been employed in Spokane
County. The strategies
include auto emission inspections, restrictions on open burning, wood
stove certification and restriction on wood stove use when pollution
levels are high, oxygenated fuels for cars, road paving, and use of
chemical deicers as an alternative to road sanding. These measures,
combined with cleaner-burning cars, have significantly improved air
quality; however, traffic volumes continue to increase which could lead
to degradation of air quality in the future i.
In July 1996, critical areas in
Spokane County were designated, and a Critical Areas Ordinance for the
Protection of Wetlands, Fish and Wildlife Habitats and Geo-Hazard Areas
in Spokane County was adopted. The Critical Areas Ordinance applies to
all unincorporated areas of Spokane County and establishes allowable
uses in wetlands, fish and wildlife habitats, and geo-hazard areas, as
well as buffer areas for wetlands.
Critical areas include the following
natural places: (a) wetlands; (b) areas with a critical recharging
effect on aquifers used for domestic water supply; (c) fish and wildlife
habitat conservation areas; (d) frequently flooded areas; and (e)
geologically hazardous areas. Specific sections within this chapter
contain information concerning the locations and status of each critical
and sensitive area category listed above i.
Threatened species for Spokane County include the bald eagle (Haliaeetus
leucocephalus), Columbia River population bull trout (Salvelinus
confluentus), Spaldings’s silene (Silene spaldingii), Palouse
goldenweed (Haplopappus liatriformis), Ute ladies’-tresses (Spiranthes
diluvialis), and water howellia (Howellia aquatilis).
Spokane County has one endangered species, the Yellow Lady’s-slipper (Cypripeduim
parviflorum).
Drawing 2-7. Critical Areas shows general habitat locations
for endangered and threatened species. There is no endangered or
threatened species habitat within the planning area; however, small
areas of endangered species habitat are found bordering the planning
area.
In addition to federal- and
state-listed endangered and threatened species, there are state-listed
candidate species and species of concern. The species of concern for
Spokane County are listed in
Error! Reference source not
found.. None of the state-listed species are found in the planning area.
Critical habitats are determined for
species with sensitive, critical, threatened, or endangered
characterizations. These habitats are managed under the Critical Areas
Ordinance described above. Habitat conservation measures seek to
manage land to maintain the species in suitable, natural habitats
without creating isolated subpopulations. Spokane County defines fish
and wildlife habitat conservation areas based upon the presence of
species of concern (i.e., threatened, sensitive and endangered species);
habitats and species of local importance; certain lakes, ponds, streams
and rivers that provide fish or wildlife habitat; and state natural area
preserves and natural resource conservation areas. Fish and Wildlife
Critical Habitat areas are shown in
Drawing 2-7
i.
This section provides an overview of the key water resources within the
planning area or potentially impacted by the County’s wastewater
management activities. For a more thorough discussion of water quality
and water quantity issues associated with the Spokane Valley-Rathdrum
Prairie Aquifer and the Spokane and Little Spokane Rivers, the reader is
referred to Chapter 4.
Principal groundwater aquifers in
the vicinity of the planning area are shown in
Drawing 2-4. By far,
the most significant groundwater resource is the Spokane Valley-Rathdrum
Prairie Aquifer, which serves as a source of drinking water for over
400,000 people. This aquifer commences at Lake Pend Oreille in Idaho
and continues west and southwest through the Spokane Valley. It is part
of the Purcell Trench, a major intermountain valley extending northeast
from Spokane into Canada. The aquifer is the product of continental
glaciers and flood deposits (one of three hydrogeologic regimes found in
the County), and is composed of glaciofluvial sands and gravels over 400
feet thick. The sand and gravel deposits are underlain and laterally
bounded by granite and basalt in most portions of the valley. In some
areas, the aquifer boundaries are comprised of low-permeability lakebed
sediments (clays). In the planning area, the aquifer is recharged along
its margin on all sides and from percolation through porous soils
overlying the aquifer and through seepage from the Spokane River. In
1978, the United States Environmental Protection Agency declared the
Spokane Valley-Rathdrum Prairie Aquifer a “sole source” aquifer under
the provisions of Section 1424(e) of the 1976 Amendments to the Safe
Drinking Water Act.
Additional aquifers located within Spokane County consist of basalt
interbeds, basement granitics, and matasediments, which formed primarily
along fractures
[iv].
These are recharged by precipitation and from interaction with adjacent
streams. Groundwater sources within Spokane County in the vicinity of
the planning area include the following units: the Deer Park Aquifer;
the Little Spokane Aquifer area; the Green Bluff, Peone Prairie and
Orchard-Pleasant Prairie Aquifers; and the East Columbia Plateau Aquifer
area, which includes the West Plains Aquifer i. Like the Spokane Valley-Rathdrum Prairie
Aquifer, the Deer Park and Little Spokane Aquifers were created by
continental glaciers and flood deposits. The East Columbia Plateau
Aquifer in the western portion of the County represents a hydrogeologic
regime consisting of thin aquifers in basalt formations. The third
hydrogeologic regime found in the county is granitic formations which
tend to be located in the northern highlands i.
Soils in the planning area are
highly permeable and gravels are frequently encountered at depths of
seven to eight feet. During implementation of the County’s sewer
extension program, groundwater has been rarely encountered during trench
excavations. Groundwater levels are typically 200 feet below ground
surface.
Spokane County has many surface water bodies that provide a variety of
economic, recreational and aesthetic benefits and uses.
Drawing 2-4 shows the location of surface water features in
and surrounding the planning area.
Principal rivers and streams in the planning area are the Spokane River,
Little Spokane River, and Latah Creek. The Spokane River begins in Idaho
at Lake Coeur d’Alene and flows west into Washington, through the
planning area. Wide flow fluctuations are common, ranging from a
minimum of 800 cubic feet per second (cfs) to a maximum of 30,000 cfs.
More typically, the river flow varies from 2000 to 7000 cfs. The wide
fluctuation of flow levels is dependent upon season, precipitation,
water use, and operating strategies of the Post Falls Dam in Idaho. As
described in Chapter 4, the Spokane River and Spokane Valley-Rathdrum
Prairie Aquifer are highly interactive with the river, losing or gaining
large volumes of water depending on the location along its reach. The
Spokane River is dammed at several locations along its course. The Post
Falls Dam controls the water level in Lake Coeur d’Alene and regulates
release of water to the river. The Upriver Dam, located within the
planning area, creates a 4.5-mile long backwater used for recreational
purposes. Downstream of Spokane, the Long Lake Dam creates 22-mile long
Long Lake, a major recreational resource in the region.
The Little Spokane River and its tributaries originate just north of
Spokane County and flow south, discharging to Long Lake at the border of
Stephens and Spokane Counties. Typically, Little Spokane River flows
fluctuate between 300 and 700 cfs. Flows in the lower segment of the
river are augmented by discharge from the Spokane Valley-Rathdrum
Prairie Aquifer
[v].
Latah Creek originates in Benewah County, Idaho and flows north to a
confluence with the Spokane River at the west side of the City of
Spokane. Flow fluctuates between an average summer flow of 30 cfs to
periodic winter flows reaching up to 2000 cfs
[vi].
Major lakes surrounding the planning area include Newman Lake and
Liberty Lake on the east side of the planning area and a cluster of
lakes including Medical Lake, Clear Lake, and Silver Lake to the
southwest.
There are no federally designated wild and scenic rivers within Spokane
County. The Little Spokane River is designated as a State-listed wild
and scenic river from its confluence with the Spokane River to
approximately River Mile 5; however, the state designation does not
carry the same regulatory significance as a federal designation. Along
the lower stretch of the river, the 1,353-acre Little Spokane River
Natural Area has been established.
Frequently flooded areas, or Flood
Hazard Areas, are lands which have a 1-percent or greater chance of
flooding in any given year. They are commonly referred to as 100-year
floodplains. These lands are found near streams, rivers, lakes, sink
areas, major drainage areas and wetlands i.
Major flood plains in the area are
located along the shores of lakes, the Spokane River, and Little Spokane
River.
Drawing 2-8. Flood Hazard
shows flood hazard locations in the County.
The major stormwater problem areas
are located in Glenrose/Central Park, Eaglewood, Five Mile Prairie, West
Plains and the Saltese area (including the Ridgemont, Morningside
and Bella Vista areas). These areas are underlain by geology that does
not readily absorb water; therefore, they tend to experience acute
stormwater problems just after a heavy rain or rapid snowmelt. The City
of Spokane’s combined sewer system is susceptible to surcharge due to
runoff from storm events. Spokane County has a separated sewer system,
in which stormwater inflow and infiltration has little influence.
Spokane County has adopted the
definition of wetlands specified in the Growth Management Act (GMA).
This definition includes “areas that are inundated or saturated by
surface water or groundwater at a frequency and duration sufficient to
support, and that under normal circumstances do support, a prevalence of
vegetation typically adapted for life in saturated soil conditions”.
Wetlands are regulated under the Critical Areas Ordinance as described
in the Critical and Sensitive Areas section of this chapter.
According to a wetland inventory
conducted for Spokane County in 1991, wetlands are distributed
throughout Spokane County, with the majority of wetlands located in the
west and southwest as shown in
Drawing 2-9. Wetlands.
Palustrine wetlands are scattered throughout the southwest portion of
the county and are characterized as inland wetlands, which lack
flowing water. Lacustrine
unvegetated wetlands occur along streams, rivers, and lakes especially
along the Spokane River outside of the Spokane City limits. The Spokane
Valley
has few wetlands, due to the
permeable nature of the soils. There are a few small areas of wetlands
scattered throughout the planning area, with the majority focused in
small clumps in the western section.
Spokane County depends almost
entirely on groundwater for its domestic water supply. Several thousand
homes rely on private wells and approximately 400,000 people utilize the
Spokane Valley-Rathdrum Prairie Aquifer for drinking water.
The City of Spokane supplies
drinking water from eight well fields located within the City’s limits.
The well fields have a pumping capacity of 220 million gallons per day
which equates to 24 billion gallons of water per year
[vii].
Chapter 4 present further discussion of potable water usage from the
Spokane Aquifer. Detailed information on well locations, types, depth,
capacity and year of construction may be found in the
City of Spokane’s Wellhead
Protection Program Phase I Report
vii and in Spokane County’s 1996 Report on Water
Quality and Water Quantity[viii].
Due to the permeability of the soils overlying the Spokane
Valley-Rathdrum Prairie Aquifer, potential for aquifer contamination by
surface and subsurface activities is high.
A key regional concern has been the proliferation of septic tank leach
fields and other on-site disposal systems over the aquifer. This
activity has resulted in increased nitrate levels in groundwater down
gradient from the disposal fields, which is an indicator of potential
groundwater pollution from human wastewater. In 1983, the State Board
of Health adopted regulations establishing minimum lot sizes to be
served by on-site wastewater disposal systems with soil conditions that
could contribute to aquifer contamination. The same year, the County
began construction of a regional sewer system to serve unincorporated
parts of the County. As described earlier, the County focused efforts on
the Priority Sewer Service Area, encompassing high-density developments
that exceeded the Board of Health’s density standards. Through 1995, a
total of 15,595 Equivalent Residential Units (ERUs) had been connected
to the County’s sewer system
[ix].
From 1995 through 1999, approximately 6,900 additional on-site disposal
systems have been replaced by connections to the sewer. Water quality
monitoring has demonstrated that where sewers have been installed, the
trend toward increased nitrate levels has been reversed
[x].
Completion of the County’s sewer program will further protect and
improve groundwater quality.
As on-site wastewater disposal systems are eliminated, the primary focus
of concern has now turned towards accidental spills of chemicals and
toxins
[xi].
Petroleum products, which are transported or stored over the aquifer,
are of particular concern. In addition, there is concern of
contamination due to manufacturing chemicals, chemical storage, and
illegal dumping
[xii].
To address these issues, the City of Spokane recently prepared a
wellhead protection program
[xiii].
This section provides information on historical population, land use,
economic development, historical and archaeological resources and
governmental structures. Much of the source material used for this
section addresses countywide characteristics, and is not specific to the
wastewater planning area. Where possible, more localized information is
presented.
As shown in
Figure 2‑2, the
population in Spokane County increased from 37,500 people in 1890 to
more than 414,000 people in 1999. With the exception of the early
portion of the 20th century (1910 through 1930), growth in
the County has steadily increased.
The estimated 1999 population within
the Spokane County wastewater planning area is 121,000, of which 54,000
people are currently served by the County’s sewer system.

Figure 2‑2.
Spokane County Historical Population Trends
The City of Spokane and surrounding
urban areas are an economic and cultural center for much of eastern
Washington and northern Idaho. The metropolitan center has traditionally
been connected closely with the resource economy of the surrounding
rural areas. Agriculture, forestry and mining remain important economic
activities that shape the rural character of Spokane County. Spokane
County is approximately 1,760 square miles in area, of which
approximately 95 percent is unincorporated.
A general zoning map for the region,
including the wastewater planning area is shown in
Drawing 2-10. Zoning Area.
Within the planning area, the dominant land use category is urban
residential. The main business corridor in the planning area is located
along Sprague, with other smaller business and industrial areas
scattered throughout the planning area.
Median household and per capita
incomes in Spokane County rose through the 1970s, then declined or were
stagnant through the 1980s. However, recent increases in both income and
retail sales indicate a strong local economy.
Figure 2‑3 shows the
increase in both median household income and per capita personal income
since 1994
[xiv].

Figure 2‑3.
Spokane County Median Household and Per Capita Income
Businesses within Spokane County
employ workers from within the County and from nearby Kootenai County,
Idaho. According to the U.S. Bureau of Census 1997 Economic Census, the
highest employment in the County is provided by the manufacturing
industry, retail trade, and health care/social assistance. The total
number of establishments and employment by industry are shown in
Table 2‑1.
Table
2‑1. 1997
Spokane County Economic Census Results
|
Industry Description |
Number of Establishments |
Number of Employees |
|
Manufacturing |
572 |
20,892 |
|
Wholesale trade |
788 |
11,268 |
|
Retail trade |
1,730 |
22,246 |
|
Broadcasting & telecommunications |
83 |
1,900 |
|
Information services & data processing services |
29 |
204 |
|
Real estate & rental & leasing |
503 |
2,674 |
|
Rental & leasing services |
105 |
725 |
|
Professional, scientific, & technical services |
894 |
5,806 |
|
Administrative & support |
422 |
9,644 |
|
Educational services |
77 |
480 |
|
Ambulatory health care services |
719 |
7,195 |
|
Nursing & residential care facilities |
138 |
2,784 |
|
Social assistance |
134 |
1,158 |
|
Non-taxable health care & social assistance |
207 |
14,014 |
|
Arts, entertainment, & recreation |
140 |
1,919 |
|
Accommodation & foodservices |
906 |
14,490 |
|
Other services (except public administration) |
842 |
5,158 |
The County is home to many top
employers such as Hewlett Packard, Honeywell, the Boeing Company, the
United States Air Force, Key Tronic, BF Goodrich Aerospace, Principal
Financial Group, and Travelers Property Casualty xiv.
Urban uses have replaced farms in
much of Spokane County; however, 560 square miles of the County remain
designated as agricultural land. Urbanization is particularly evident in
the County’s wastewater planning area. Sixty years ago, the entire
Spokane Valley area was irrigated and devoted to raising fruits and
vegetables; however, gradual urbanization has displaced nearly all
agricultural activities. The conversion of land use resulted from
accessibility to roads, a dependable supply of water, and level land
characteristics with few physical constraints to development.
Prime farmland consists of rural land with excellent physical and
chemical characteristics for the production of food, feed, forage,
fiber, and oilseed crops. There is prime farmland located directly
north of the planning area, and on the western and southeastern
boundaries of the County (see
Drawing 2-10).
Much of the best agricultural land
in Spokane County was protected from development when the 1980
Comprehensive Plan was adopted. The 1980 plan designated approximately
one-third of the County as agricultural land, with restrictions placed
on nonagricultural development in these areas. Spokane County
agriculture consists of 32% livestock (not including dairy, poultry and
animal specialties), 21% grain, 16% forage crops, and 13% animal
specialties. The remaining uses include vegetables, melons, fruits,
nuts horticultural specialties, dairy, poultry, eggs, and general farms
i.
The area which is now Spokane County
shows evidence of habitation reaching back at least 13,000 years.
Within Spokane County there were as many as six aboriginal groups, which
now compose three main tribes: the Spokanes, the Coeur d’Alenes and the
Kalispels. Each of these groups harvested vegetation, hunted game stock
and traded with each other.
In 1810, British traders built a
trading post (the Spokane House) near the confluence of the Spokane and
Little Spokane Rivers. The U.S. Government and the Spokane area tribes
fought over land throughout the early to mid-1800s, until the tribes
were eventually defeated, after which European immigrants began moving
into the area in larger numbers. The territorial legislature created
Spokane County in 1858. The county included all of Washington State east
of the Cascade Mountains, as well as northern Idaho and western Montana:
about 75,000 square miles
[xv].
In these early days of Spokane’s
history, only a few farms dotted the countryside spaced many miles
apart. By the early Twentieth Century, Spokane County was the rapidly
growing center of the Inland Northwest, an area that encompassed the
mining district of northern Idaho and southern British Columbia as well
as the rich timber and farmlands of eastern Washington. By 1903, the
region was served by several transcontinental rail lines and was the hub
of a growing system of electric interurban lines managed by the Spokane
and Inland Empire Railroad System Company
[xvi].
The cultural resources inventory
includes both archeological and historical sites. The inventory includes
about 100 archeological sites, which are not available to the public
because of past abuse of such sites. They include Indian-related
locations which have been identified. These are fishing sites, trading
grounds, village sites, pictographs and burial grounds. Archeological
sites tend to be found near rivers and lakes at places of note such as
waterfalls, points of river crossing, the confluence of streams or just
along the shore. These sites tend to be buried and are discovered only
when the ground is broken, as for construction.
A wide range of governmental agencies has interest in wastewater
management issues in Spokane County. These agencies span many
jurisdictional levels: local, regional, state and federal. For the
purpose of this discussion, the agencies are divided into two groups:
The first group, “Local Wastewater Service Providers,” include those
agencies that either contribute wastewater to the County collection
system or receive flow from the County for treatment and disposal. The
second group, “Other Interested Agencies,” is those agencies having an
interest in the plan. Authorities and responsibilities of the local
wastewater service providers are described below, along with a listing
of other interested agencies and governments.
Local Wastewater Service Providers
Spokane County. Spokane County provides wastewater collection
service to residential, commercial and industrial customers
within its designated service area. The County also operates and
maintains several small wastewater treatment facilities that serve small
developments to which the centralized sewer system has yet to be
extended (see discussion in Chapter 5).
City of Spokane. The City of Spokane owns and operates the
Spokane Advanced Wastewater Treatment Plant (SAWTP) which processes
wastewater generated in the City of Spokane, Spokane County, Airway
Heights and Fairchild Air Force Base. Wastewater generated in Spokane
County is conveyed through City-owned interceptor sewers to the SAWTP.
In 1980, an interlocal agreement between the City and County of Spokane
resulted in the County purchasing treatment and conveyance capacity in
the City’s system. The agreement addresses a variety of wastewater
management issues, however, at the heart of the contract is the County’s
procurement of 10 million gallons per day of dry weather treatment
capacity at the SAWTP. Since 1980, four amendments to the original
agreement have been executed to refine issues associated with cost
sharing, wet-weather conveyance capacity, pretreatment responsibilities
and other issues.
Town of Millwood. The Town of Millwood operates a wastewater
collection system. Wastewater generated in Millwood is discharged to
Spokane County’s interceptor system for ultimate conveyance to the
SAWTP.
Liberty Lake Sewer and Water District. Liberty Lake Sewer and
Water District provides wastewater collection, treatment and disposal
services for residential, commercial and industrial customers in the
east Spokane Valley near the Idaho State line. In 1993, the District
entered into an agreement with Spokane County to allow “excess” flow
from the District to be conveyed through the County’s interceptor to the
SAWTP on an interim basis should the capacity of the District’s
treatment plant be exceeded, and contingent upon available capacity in
the County wastewater system. To date, no District flows have been sent
through the County system.
Other Interested Agencies
The following is a partial list of other agencies, which share an
interest in water quality and wastewater management issues in the
region, and may be involved in Spokane County’s facilities plan. These
agencies have an interest in the plan because of their regulatory
functions, responsibility for facilities located within the watershed,
interest in the surface and groundwater resources, or ability to impact
development or implementation of the plan.
Federal
§
Bureau of Reclamation
§
Department of Agriculture
§
Department of Energy
§
District Corps of Engineers
§
Environmental Protection Agency
§
Federal Emergency Management Administration
§
Fish and Wildlife Service
§
National Marine Fisheries Service
§
Soil Conservation Service
State of Washington
§
Department of Agriculture
§
Department of Ecology
§
Department of Health
§
Department of Natural Resources
§
Fish and Wildlife
State of Idaho
§
Department of Environmental Quality
Regional Agencies, Governments and Entities
§
City of Airway Heights
§
City of Coeur d’Alene, Idaho
§
City of Post Falls, Idaho
§
Fairchild Air Force Base
§
Hayden Area Regional Sewerage Board, Idaho
§
Spokane River Phosphorus Technical Advisory Committee
§
Spokane County Air Pollution Control Agency
§
Spokane County Health District