pws 4100548 0 drinking water intake -surface water drinking water protection area for watersheds...

Figure 1: Winston-Dillard Water System's Drinking Water Protection Area

PWS 4100957

9 Drinking Water Intake - Surface Water

Drinking Water Protection Area

For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the Winston-Dillard Water District's drinking water protection area. Activities and impacts in the Winston-Dillard Water District"s drinking water protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:24,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Mt Gurney (1g90), Reston (1987), Winston (1987), Roseburg West (1987),Tenmile (1990), Camas Valley (1990), Chipmunk Ridge (1990), Live Oak Mtn (1990), and Nickel Mtn. (1986) are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

StataolOregan Oepilrtmenl of Envll'

Figure 2: Sensitive Areas within Winston-Dillard Water District's Drinking Water Protection Area PWS 4100957

• Drinking Water Intake - Surface Water


Sources of Information: High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Solis derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGO Layer Table. K factor displayed is a weighted average (of only the surface layer) for the map unit. High Runoff Potential: Hydrology Group D (very slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified. High Permeability Soils: Alluvial deposits (Oal), dune sand (Od) and landslide and debris-flow deposits (Ols) from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

j ffi1!ilJ'.J.1e on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, rcDEO used existing GIS layers and other natural resource agency data sets. Not all areas of the state have

been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEO has sought to obtain the best available information for this composite.

Printed January, 2003 Oregon Department of Environmental Quality GIS

Kilometert

0 10

-·-'···~I ?~/I"* l'-"I'"~ 012345878 Mlle•

Sensitive Areas in Watershed

High Soil Erosion Potential (Slope > = 30 Percent and Soil Erodibility Factor > =.251

Figure 1: Roseburg Forest Prod-Dillard's Drinking Water Protection Area

PWS 4194300

Drinking Water Intake - Surface Water


For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the Roseburg Forest Products-Dillard's drinking water protection area. Activities and impacts in the

·Roseburg Forest Products-Dillard's drinking water protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:24,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Nickel Mtn (1986). Canyonville (1986). Live Oak Mtn (1990), Winston (1987), Roseburg East (1987), Roseburg West(1987l. Reston (1990). Myrtle Creek (1987), and Tenmile (1990) are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

S!ateolO~ D

Figure 2: Sensitive Areas within Roseburg Forest Prod-Dillard's Drinking Water Protection Area PWS 4194300 • Drinking Water A.• Intake - Surface Water "T Drinking Water

Protection Area

Sources of Information: High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained '1n the SSURGO Layer Table. K factor displayed is a weighted average (of only the surface layer) for the map unit. High Runoff Potential: Hydrology Group D Ivery slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified. High Permeability Soils: Alluvial deposits (Qal), dune sand IOdl and landslide and debris-flow deposits (Qls) from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, DEO used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEQ has sought to obtain the best available information for this composite.

~ [!!;[!] ;,;:-; Printed December, 2002 Oregon Department of Environmental Quality GIS

Composite of Sensitive Areas 0

Kilometers

2 3 4

Mile•

6


High Soil Erosion Potential (High Sediment Yield Potential)

High Permeability Soils !Alluvial Deposits, Dune Sand, Landslide and Debris-flow Deposits)

Figure 1: Clarks Branch Water Assoc.'s Drinking Water Protection Area PWS 4100548



For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the Clarks Branch Water Association's drinking water protection area. Activities and impacts in the Clarks Branch Water Association's drinking protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:24,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Myrtle Creek (1987). Canyonville (1986), Roseburg East (1987), Lane Mtn (1987), Dixonville (1987), Red Butte (1989). Deadman Mtn (1989), White Rock (1987), Dodson Butte (1987), Days Creek (1986), Milo (1986). and Tiller (1989) are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

SlateofOreg:in --· EnVlronmantal Qllilllly

' ' ' I I ' '

' I •

' ' '

Kiiometer•

0 , z 3 4 6

~ 0 2 3

Mlle• Printed February, 2003

Oregon Department of Environmental Quality GIS

Figure 2: Sensitive Areas within Clarks Branch Water Association's Drinking Water Protection Area PWS 4100548

• Drinking Water Intake - Surface Water


Sources of Information: High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGD Layer Table. K factor displayed is a weighted average (of only the surface layer) for the map unit. High Runoff Potential: Hydrology Group D (very slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified. High Permeability Soils: Alluvial deposits (Oal), dune sand (Qd) and landslide and debris-flow deposits (Qls) from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, DEQ used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEQ has sought to obtain the best available information for this composite.

Kilometer•

Printed February, 2003 Oregon Oepairtment of Environmental Quality GIS


Mile•


High Permeability Soils (Alluvial Deposits)

Figure 1: City of Myrtle Creek's Drinking Water Protection Area PWS 4100550



For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the City of Myrtle Creek's drinking water protection area. Activities and impacts in the City of Myrtle Creek's drinking protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:24,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Myrtle Creek (1987) and Canyonville [1986) are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

Stat!l o!Oreg:in Oept1nrneo1 of Envlfonmental Qu~ucy

Kiiometer•

~ ~ 0

Miles Printed January, 2003

Oregon Departman1 of Environmental Quality GIS

Figure 2: Sensitive Areas within the City of Myrtle Creek's Drinking Water Protection Area PWS 4100550 8 Drinking Water

Intake - Surface Water


Sources of Information: High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGO Layer Table. K factor displayed is a weighted average {of only the surface layer) for the map unit. High Runoff Potential: Hydrology Group D {very slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified. High Permeability Soils: Alluvial deposits (Dal), dune sand {Qd) and landslide and debris-flow deposits {Qlsl from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir,

Note on Sensitive Areas: In determining the most sensitive areas withih this Drinking Water Protection Area, DEQ used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEQ has sought to obtain the best available information for this composita

Kilometer•

Printed January, 2003 Oregon Department of Environmental Quality G1S

Composite of Sensitive Areas

Mile•

~ I

~1 . I I ~-~\ ~ \

I


High Soil Erosion Potential {Slope > = 30 Percent and Soil Erodibility Factor > =.25) High Permeability Soils (Alluvial Deposits)

Sensitive Area Setbacks Adjacent to Streams and Reservoirs (1000 feet)

I' ~7

) I /

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Figure 1: Tri-City Water District's Drinking Water Protection Area PWS 4100549



For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the Tri-City Water District's drinking water protection area. Activities and impacts in the Tri-City Water District's drinking protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:24,000 scale U.S. Geological Survey Digital Raster Graphics IDRGs) for Winston 11987), Myrtle Creek (1987), Dodson Butte 11987), White Rock (1987), Deadman Mtn 11989), Nickel Mtn (1986), Red Butte (1989), Days Creek 11986), Milo (1986), Tiller (1989), McCullough Creek (1986), Ouines (1986), Starvout Creek 11986), Cedar Springs Mtn 11986), Richter Mtn (1989), Roseburg West (1987), Roseburg East (1987), Dixonville (1987), Lane Mtn (1987), and Canyonville (1986), are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

State of Oregon Departmen1 of Environmental Oua~ty

. "

' ' '

. i i

' '

Kiiometers

; I '

0 1 2 3 4 6

~ 0 ' 3

Miies Printed January, 2003


Figure 2: Sensitive Areas within Tri-City Water District's Drinking Water Protection Area PWS 4100549 8 Drinking Water



Sources of Information: High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGO Layer Table. K factor displayed is a weighted average (of only the surface layer) for the map unit. High Runoff Potential: Hydrology Group D (very slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified. High Permeability Soils: Alluvial deposits (Qal), dune sand (Qd) and landslide and debris-flow deposits (Qls) from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, DEQ used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEQ has sought to obtain the best available information for this composite.

Kilometer•

Printed January, 2003 0 10 Oregon Department of Environmental Quality GIS


Mlle•

\


High Soil Erosion Potential (Slope > = 30 Percent and Soil Erodibility Factor > =.25)

J High Runoff Potential (Hydro logic Group D - slow infiltration rates)

10 .g

Figure 1: Milo Academy's Drinking Water Protection Area

PWS 4100250



For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the watersystem's intake are included in the Milo Academy's drinking water protection area. Activities and impacts in the Milo Academy's drinking protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:24,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Tiller (1989), Deadman Mtn (1989). White Rock (1987), Richter Mtn (1989), Milo (1986). and Cedar Springs Mtn (1986) are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

State of Oregon Oepartmeot or En'llronmanlnl Quaity

' ,, '

' ' '

Kllomet11rs

; I '

0 1 2 3 4

_.,/ 21 ·~·!;!:··;1~ 0 2

Miles Printed December, 2002


Figure 2: Sensitive Areas within Milo Academny's Drinking Water Protection Area PWS 4100250 • Drinking Water



Sources of Information: (Douglas County)

High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGO Layer Table. K factor displayed is a weighted average(of only the surface layer) for the map unit. High Runoff Potential: Hydrologic Group D (very slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified.

(Umpqua National Forest) High Soil Erodibility: Defined by high sedimentation yield potential of the dominant soil. High Runoff Potential: Hydrologic Group Din the dominant soil. These data are extracted from the Soil Resource Inventory.

(Entire Watershed) High Permeability Soils: Alluvial deposits (Oal) from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, DEO used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEO has sought to obtain the best available information for this composite.

Kilometers

Printed December, 2002 Oregon Department of Environmental Quality GlS

Composite of Sensitive Areas 0 2 3 4 5

Mile•

) v

~ ~

N


High Soil Erosion Potential (Slope > = 30 Percent and Soil Erodibility Factor > =.25) High Permeability Soils (Alluvial Deposits)

'~ I

( (

" High Runoff Potential (Hydrologic Group D - slow infiltration rates)

~ ' d

71 1

(r I

Figure 1: Tiller Elementary, SD #15's Drinking Water Protection Area

PWS 4192139

• IV



For watersheds with more than one intake, Oregon compl.etes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the. water system's intake are. included in the Tiller Elementary, School District #15's drinking water protection area. Activities and impacts in the Tiller Elementary, School District #15'.s drinking protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:24,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Richter Mtn (1989), Tiller (1989), Pickett Butte (1989), Ragsdale Butte (1989), Cedar Springs Mtn (1986), and Milo (1986) are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

StataofOregoh Department of Environmental QU"ft!Y

0

r I 0

I , !

. . '

Kilometers , 2 3 I " I '.I

I

'i I 2

Miles Printed February, 2003


Figure 2: Sensitive Areas within Tiller Elementary, SD #15's Drinking Water Protection Area PWS 4192139 8 Drinking Water

lritake - Surface Water


Sources of Information: (Douglas/Jackson County Areas)

High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,QdO, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGO Layer Table. K factor displayed is a weighted average(of only the surface layer) for the map unit. High Runoff Potential: Hydro logic Group D (very slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified.

IUmpqua National Forest) High Soil Erodibility: Defined by high s.edimentation yield potential of the dominant soil. High Runoff Potential: Hydrologic Group Din the dominant sbil. These data are extracted from the Soil Resource Inventory.

(Entire Watershed) High Permeability Soils: Alluvial deposits (Qal) from the U.S. Geologi¢al Survey Geologic Map of Or~gon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir. ,

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, DEQ used existing GIS layers and other-natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEQ has sought to obtain the best available information for this composite.

Printed February, 2003 , Oregon Department af Environmental Quality GIS


Kilameter•

2 3

Milel

4 5


High Soil Erosion Potential (Slope > = 30 Percent and Soil Erodibility Factor > =.25)

(

High Runoff Potential.(Hydrologic Group D - slow infiltration rates)

Figure 1: USFS Tiller Ranger Station's Drinking Water Protection Area

PWS 4101092



For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the · USFS Tiller Ranger Station's drinking water protection area. Activities and impacts in the USFS Tiller Ranger Station's drinking protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:100,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Diamond Lake (1978), and Crater Lake (1989) are displayed. DR Gs are scanned images of topographic sheets. Where the DR Gs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen .

SMaolOragon ililpartme111 of Env~onrnantiU QuaUty

I

'' f

\

.,...,... I - I I

I

I

I

I

i i I

~ ~ 0 2 ' 4

"\ I

I

\

I

MllH Printed February, 2003

Oregon Departmen1 of Environmental Quallty GJS

Figure 2: Sensitive Areas within the USFS Tiller Ranger Station's Drinking Water Protection Area PWS 4101092 9 Drinking Water



Sources of Information: (Douglas County)

High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unil. K factor is contained in the SSURGO Layer Table. K factor displayed is a weighted average(of only the surface layer) for the map unit. High Runoff Potential: Hydrologic Group D (very slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified.


(Entire Watershed I . High Permeability Soils: Alluvial deposits !Dall from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, DEO used existing GIS layers and other natural resource agency data Sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEO has sought to obtain the best available information for this composite.

Kilometer•

Printed February, 2003 0 10 Oregon Department of Environmentcll Quality GlS


Miles

10


High Soil Erosion Potential (Slope > ~ 30 Percent and Soil Erodibility Factor > ~.25)

Figure 1: City of Canyonville's Drinking Water Protection Area PWS 4100169



Note on Base Map: 1:24.000 scale U.S. Geological Survey Digital Raster Graphics (DRGsl for Canyonville (1986). Days Creek (1986). Quines Creek (1986) and Starvout Creek (1986) are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join. seams and/or gaps may be visible. Between DRGs, variations in information displayed also maybe seen.

.. ........ 0 1 2

~ 0

Printed February. 2001 Oregon Department of Envimnmental Quality GIS

Figure 2: Sensitive Areas within The City of Canyonville's Drinking Water Protection Area PWS 4100169

• if



Sources of Information: High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained_ in the SSURGO Layer Table. K factor displayed is a weighted average {of only the surface layer} for the map unit. High Runoff Potential: Hydrology Group D (very slow infiltration rates} from the SSURGO Component Table. SSURGO data have been certrried. High Permeability Soils: Alluvial deposits (Qal) from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Arear DEQ used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEQ has sought to obtain the best available information for this composite.

"""' ~ lllE Printed August.. 2000 0 ,..,.,.,... -· Oregon Department of Environmental Quality GIS Composite of Sensitive Areas

0

2

1

Kilometers

3

2

M ...

4

3



6

Sensitive Area Setbacks Adjacent to Streams and Reservoirs {1000_ feet)

Figure 1: Lawson Acres Water Association's Drinking Water Protection Area

PWS 4100707



For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the , LawsonAcres Water Association's drinking water protection area. Activities and impacts in the Lawson Acres Water Association's drinking water protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:24,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Canyonville (1986), and Nickel Mtn (1986) are displayed. DRGs are scanned images of topographic sheets. Where the DR Gs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

StateofOregon Ollpertment ITT Env!ronrnental Quality

Kllom1tere

~ ~ 0

Mlh111 Printed January, 2003


Figure 2: Sensitive Areas within Lawson Acres Water Association's Drinking Water Protection Area PWS 4100707 • Drinking Water



Sources of Information: High Soil Erodibility: Defined by slope~ greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGO Layer Table. K factor displayed is a weighted average (of only the surface layer) for the map unit. High Runoff Potential: Hydrology Group D (very slow infiltration rates) from the SSURGO Component ll!ble. SSURGO data have been certified. High Permeability Soils: Alluvial deposits (OalJ, dune sand (OdJ and landslide and debris-flow deposits (OlsJ from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining.the most sensitive areas within this Drinking Water P.rotectioii Area, DEO used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEQ has sought to obtain the best available information for this composite.

~ l![!!I Printed January, 2003 ~ Oregon Department of Environmente! Quality GIS

Kilometer•

3 4 '"I ,,,,

' I ~ Composite of Sensitive Areas 0 2

Mile•



(

Figure 1: City of Riddle's Drinking Water Protection Area

PWS 4100706


brin king Water Protection Area

For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the City al Riddle's drinking water protection area. Activities and impacts in the City of Riddle's drinking protection area also have the potential to impact downstream water users. Ses Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:100,000 scale U.S. Geological Survey Digital Raster Graphic (DRG) for Canyonville (1979) is displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen .

......... l _,... I"\

f

I

-~ .•. -i,- .

I

\ I !

I I

Kiiometers

~ StalllofOregan Depertmenl of Envlronman!QI aua~fy

I~ 0 2 3 •

Mile• Printed January, 2003

Oregon Department of Environmental Quallty GlS

i

I

• I

i

Figure 2: Sensitive Areas within the City of Riddle's Drinking Water Protection Area PWS 4100706

• Drinking Water Intake - Surface Water Drinking Water Protection Area

Sources of Information: High Soil Erodibility: Defined by slopes greater than 30 percent and K factor greater than .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGO Layer Table. K factor displayed is a weighted average (of only the surface layer) for the map unit. High Runoff Potential: Hydrology Group D (very slow infiltration rates) from the SSURGD Component Table. SSURGO data have been certified. High Permeability Soils: Alluvial. deposits (Call, dune sand (Qd) and landslide and debris-flow deposits (Gisi from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, DEQ used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEC has sought to obtain the best available information for this composite.

Kilometer•

Printed Jzinuary, 2003 0 10 Oregon Department of Environmental Quality G!S

0

Miles


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Figure 1: City of Glendale's Drinking Water Protection Area

PWS 4100323



For watersheds with more than one intake, Oregon completes the assessments by segment and each source water assessment represents the area from the public water system's intake to the next intake upstream. All protection areas for intakes upstream of the water system's intake are included in the City of Glendale's drinkingwater protection area. Activities and impacts in the City of Glendale's drinking water protection area also have the potential to impact downstream water users. See Attachment B for a schematic of upstream and downstream water providers in the South Umpqua Sub-Basin.

Note on Base Map: 1:100,000 scale U.S. Geological Survey Digital Raster Graphics (DRGs) for Crater Lake (1989) and Canyonville (1989) are displayed. DRGs are scanned images of topographic sheets. Where the DRGs join, seams and/or gaps may be visible. Between DRGs, variations in information displayed also may be seen.

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Figure 2: Sensitive Areas within the City of Glendale's Drinking Water Protection Area PWS 4100323

• Drinking Water Intake - Surface Water Drinking Water Protection Area

Sources of Information: (Douglas/Jackson/Josephine County Areas)

High Soil Erodibility: Defined by slopes greater than 30 percent and K factol greaterthan .25. Soils derived from 1:24,000, USDA, NRCS, SSURGO certified data. Slope is in the SSURGO database Component Table. Slope displayed is a weighted average of the average slope for the map unit. K factor is contained in the SSURGO Layer Tabla K factor displayed "1s a weighted average(of only the surface layer) for the map unit. High Runoff Potential: Hydrologic Group D (very slow infiltration rates) from the SSURGO Component Table. SSURGO data have been certified.


(Entire Watershed) High Permeability Soils: Alluvial deposits (Qal) from the U.S. Geological Survey Geologic Map of Oregon GIS layer. Sensitive Area Setbacks Adjacent to Streams and Reservoirs: 1000 foot buffer from the centerline of perennial streams and the shoreline of any reservoir.

Note on Sensitive Areas: In determining the most sensitive areas within this Drinking Water Protection Area, DEQ used existing GIS layers and other natural resource agency data sets. Not all areas of the state have been mapped for the natural resource parameters of interest or at the level of detail ideal for this type of analysis. DEQ has sought to obtain the best available information tort his composita

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~ Oregon Department of Environmental Quality GIS


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High Soil Erosion Potential (Slope>= 30 Percent and Soil Erodibility Factor> =.251

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pws 4100548 0 drinking water intake -surface water drinking water protection area for watersheds...

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