HomeMy WebLinkAboutSUB202100173 Review Comments Final Plat 2022-02-24401 McIntire Road, North Wing
o� rnv.7r Count of Albemarle Charlottesville, VA 22902-4579
Y Telephone:434-296-5832
o m COMMUNITY DEVELOPMENT DEPARTMENT WWW.ALBEMARLE.ORG
`�8GIN1N
Memorandum
To: Gwen Lacy (Gwen&raysurveyine.com)
From: Kevin McCollum, Senior Planner I
Division: Planning
Date: February 24, 2022
Subject: SUB202100173 Collins Engineering - Two Lot Division Revised TMP 69-19D
The County of Albemarle Planning Division will grant or recommend approval of the plat referenced above once
the following comments have been addressed: [Each comment is preceded by the applicable reference, which is
to the Subdivision/Zoning Ordinances unless otherwise specified.]
1. [14-308.1] A Tier H Groundwater Assessment has been initiated for this application. Results of the
assessment will be forwarded to the applicant once it is completed. Please see the attached Tier Il
Groundwater Assessment.
2. [14-302(A)(11)] Final plat approval is pending the approval and recordation of application SUB202100176
Collins Engineering BLA. Once that plat has been approved and recorded please update all applicable notes
and labels on the plat accordingly. Comment addressed.
3. [14-309 & 14-3101 Soil evaluations & Health director approval of septic systems. Please provide the soils
evaluations for the proposed lots for Health Department review. Health Director approval is required prior
to final plat approval. Comment stands. Soils evaluations were provided for Lot 3 as a whole with
application SUB202100176 (Attached) but do not include evaluations for Lots 3A and 3B individually.
Please provide this additional information for Health Department review.
4. [14-306 & 14-3171 Provide a private street maintenance agreement for review by the County Attorney. A
private street maintenance agreement template is attached below. Comment addressed.
5. [14-316] Prior to plat approval, VDOT must approve all proposed entrances onto public streets. Comment
addressed.
6. [14-302(B)(1)] Include a date of revision. Comment addressed.
Please contact Kevin McCollum in the Planning Division by using kmccollumkalbemarle.org or 434-296-5832
ext.3141 for further information.
Comments from Other Reviewers:
Virginia Department of Health (VDH) — Alan Mazurowski - alan.mazurowski@vdh.vir inia.gov, review
pending a soils evaluation report.
Virginia Department of Transportation (VDOT) —Adam Moore, adam.moorekvdot.vir ig nia.gov No
objection.
TIER II GROUNDWATER ASSESSMENT
County of Albemarle
x Department of Community Development £
401 McIntire Road, North Wing
Charlottesville, Virginia 22902
434-296-5832 1 www.albemarle.org/cdd
DATE: 11/04/2021
APPLICATION: SUB 2021-00173
PROJECT NAME: COLLINS ENGINEERING - FINAL - DIGITAL
TMP: 06900-00-00-019DO
The pending development on the property affected by the above referenced application number
meets criteria outlined in Albemarle County Code Article IV - Groundwater Assessments to
warrant a Tier 2 Groundwater Assessment. The following assessment uses the best available
sources to outline the various groundwater conditions that could have an impact on this property.
Water Quantity
# of Wells within .5 Miles of Parcel: 18
Range of Depth of those wells: None to 605.0 feet
Range of Yield of those wells: None to 60.0 gallons per minute (gpm)
Median Yield for Wells in County: 6.0 gpm
Water Quality
# of Leaking Underground Storage Tanks (LUSTs) within 2000 Feet of Parcel: 1
# of Superfund sites within .5 miles: 0
# of Landfills within .5 miles: 0
Hydroaraohy
% of Parcel that Contains Required Stream Buffers: 0.0%
Watershed of Parcel (Y/N'):
Mechums River -Stockton Creek (Y) 67.9%
North Fork Rockfish River (N) 32.1%
Geology
Bedrock:
Blue Ridge basement complex(my) - mylonitic schist and cataclastic rocks, undivided 100.0%
Hydrogeologic Units*:
Foothills -II 100.0%
If you should have any questions, please contact the Community Development Department at
434-296-5832.
' A "Y" indicates that the watershed is a water supply watershed. An "N" means that it is not.
1
69-19 E
69-19 D
69-6G
69-19A7
69-19C
Tier II Groundwater Assessment Site Map 0 60 1
20 1
80Feel
p8 APP#• SUB 2021-00173 O Subject Parcel - LUSTs
u
� TMP: 06900-00-00-019D0 O Known Water Wells A Superfund Sites
Map Created by CDD on: 11/04/2021 Water Protection ■ Landfills
Aerial Imagery from Y2018MM` Ordinance Buffers tr�
2
*Hydrogeologic Units Defined
Taken from the 1213012003 Albemarle County Hydrogeologic Assessment Phase ii —
Groundwater Availability and Sensitivity Assessment with Proposed Groundwater Assessment
Standards. Prepared by ENSAT Corporation, Culpeper, VA.
The process of investigating groundwater availability at the County -wide scale involved identifying distinct
hydrogeologic units and comparing the units based on groundwater availability characteristics for which data
could be obtained. Each hydrogeologic unit shares some common characteristics with regard to geology,
soils, and topography, although there is quite a bit of variability within each unit.
Nine hydrogeologic units were identified across the County, as follows, and as shown on the Albemarle
County Hydrogeologic Unit Map (Figure 2).
1.
2.
3.
Figure 2 - Albemarle County Hydrogeologic Unit Map
Blue Ridge West-IW: This unit lies primarily
on the steep eastern slopes of the Blue Ridge
Mountains and is dominated by the Myersville
and Parker Soils, and to a lesser extent the
Chester. Slopes range from 2-60%. These soils
are residual in nature. The Myersville soils are
derived from weathered volcanic metamorphic
rocks (greenstone) and Parker and Chester soil
series are derived from weathered granite and
granite gneiss. These soils are considered to be
relatively deep and well drained.
Blue Ridge East-IE: The Blue Ridge East unit
overlies volcanic greenstone rock and represents
the eastern limb of the Blue Ridge Anticlinorium.
The area is characterized by the presence of a
prominent ridge and trends generally northeast
within the otherwise rolling piedmont landscape.
Portions of this ridge are known locally as Green
Mountain, Carters Mountain, and the Southwest
Mountains. This area is dominated by the Rabun
and Myersville soils and to a lesser extent, the
Catoctin. The Rabun soil series is deep and well
drained and like the Myersville soil series is
formed from weathered greenstone. The
Catoctin soil series is considered to be
moderately deep and well drained and is also
formed from weathered greenstone.
Colluvial Fans -II: The Colluvial Fan unit lies at
the base of the eastern slopes of the Blue Ridge
Mountain and is characterized by relatively steep
drainage swales that extend to more gradual sloping conditions. The area includes a series of
intermittent drainages that include ephemeral drainage ways. Many of the intermittent drainages
become perennial streams as this area includes stream bottom valleys. A significant portion of the unit
area consists of transported soils including the Braddock and Thurmont. These soils are formed in
colluvial and alluvial materials found on colluvial fans and terraces and are the product of weathered
granite, granodiorite, granite gneiss, and greenstone. Both of these soil series are deep and well
drained with slopes ranging from 2-25%. Residual soils including the Hayesville and the Chester are
also abundant. These soils are also deep and well drained and are formed on upland slopes from
weathered products of granite and granite gneiss. Slopes of these soils typically range from 2-45%.
Bedrock geology consists largely of metagranitic rock of the Blue Ridge Basement Complex and
metasedimentary, metaconglomerate and phyllite of the Swift Run Formation. The accumulation of
transported soils (colluvial and alluvial) can form "cappings" over residual soils and parent material,
which can add to the overall thickness of the overburden.
4. Piedmont Foothills -III: The Piedmont Foothills unit is characterized by rolling upland to relatively
steep topography. Soils within this area dominated by the Hayesville, Ashe and Chester soil series
which are moderately deep to deep, and generally well drained. These soils are found on the piedmont
upland and foothills of the Blue Ridge Mountain on slopes ranging from 2-45%. These soils are formed
from weathered granites and meta -granites of the Blue Ridge Basement complex. The Piedmont
Foothills area is bifurcated by Hydrogeologic Unit IV (Lynchburg).
5. Lynchburg -IV: The Lynchburg unit is characterized by a relatively narrow band that trends in a
northeast direction and includes a relatively long segment of the Mechums River valley. Soils within this
unit are dominated by the Hazel and to a lesser extent by the Elioak and Glenelg soils. The Hazel soil
series are moderately deep and well drained and are formed in the weathered products of
metagraywacke sandstone and mica schist. Hazel soils lie on uplands and their slopes range from 7-
45%. The Elioak soil series are deep and well drained and are formed in the products of weathered
micaeous metamorphic rock. Slopes of the Elioak range from 2-25%. The Glenelg soils are also deep
and well drained and are formed in the weathered products of quartz mica schist. Slopes of the Glenelg
range from 2-45%. The area is underlain primarily by the Lynchburg Formation and/or the Mechums
River Formation which consists largely of metagraywacke, meta sandstone, and graphitic schist.
6. Ragged Mountain-V: The Ragged Mountain unit is characterized by mountainous terrain located in the
southwestern portion of the County and is underlain by the metagranitic rocks of the Blue Ridge
Basement Complex. The soils in the area are dominated by the Chester, Hayesville, Ashe, and Parker
soil series. These soils are derived from weathered granite and granite gneiss and are deep and
excessively well drained. These soils range in slope from 2-45% with some slopes up to 60 percent in
the Parker soils.
7. Candler -VI: The Candler unit is underlain primarily by the Candler formation. Bedrock geology includes
phyllites and to a lesser degree laminated metasiltstone. Soils underlying the unit area are dominated
by the Manteo and Nason series. Manteo soils are shallow and somewhat excessively drained. The
Manteo soils are formed in the weathered products of sericitic schist/phyllite on uplands and range in
slope from 2-45%. The Nason soil series are deep and well drained and are also formed in the
weathered products of sericitic schist/phyllite. The Nason soils are formed on uplands and range in
slope from 2-25%.
8. Newark Basin-VII: The Newark Basin unit is characterized by low relief topography, which exists over
Mesozoic basin geology. The unit is underlain by the Newark Supergroup which consists of sandstones,
siltstones, and shales. Soils within this area are dominated by the Totier, Rapidan, and Penn series.
The Totier soil series are deep and well drained and are formed from weathered Triassic red shale.
These soils are found on uplands and range in slope from 2-15% deep to moderately deep and well
drained. Slopes range from 2-25%.
The Rapidan soil series are also deep and well drained and are formed in weathered products of Triassic
conglomerate. The Rapidan, like the Totier, are found on uplands and range in slope from 2-25%. The
Penn series are moderately deep and well drained and are formed from the weathered products of
Triassic red shale. The Newark Basin hydrogeologic unit includes the Scottsville Basin located in the
southern portion of the County and much smaller area of the Barboursville Basin located in the northern
portion of the County.
9. Piedmont Proper-VIII: The Piedmont Proper unit is characterized by gently rolling piedmont
topography. The bedrock geology underlying the unit is mapped as Metagraywacke, quartoze schist,
and melange. Soils in the unit area are dominated by the Nason and the Manteo in nearly equal
percentages. Although these same soils also dominated the Candler unit, it should be noted that the
Manteo soils were nearly twice as prevalent as compared to the Nason. Manteo soils are shallow and
somewhat excessively drained. The Manteo soils are formed in the weathered products of sericitic
schists/phyllites on uplands and range in slope from 2-45%. The Nason soil series are deep and well
drained and are also formed in the weathered products of sericitic schist. The Nason soils are formed
on uplands and range in slope from 2-25%.
10. Barboursville -IX: This unit exists in only a small portion of the County at the area where Route 20
enters Orange County. Evidently this hydrogeologic unit was small enough that it did not factor into the
ENSAT report and therefore does not have a description like the other units. You can see an unlabeled
delineation of this unit in the map (Figure 2) along the northern County boundary near the right-hand
side.
0
COMMONWEALTH OF VIRGINIA
Application for: EJ Sewage System 0 Water Supply
Owner: Mountain View Land Trust
Mailing Address: 3209 Clarke Lane
Charlottesville. VA 22901
Agent: Stockton Creek LLC c/o JeseP44kimpeerr r3I0.r, Iftw
Mailing Address: 455 2nd Street SE, Suite 201 Charlottesville, VA 22902
Site Address: TBD
Afton, VA 22920
Directions to Property:
Subdivision:
Tax Map:
Corner of Route 250 & Route 151
69-19D
Section:
Other Property Info:
Phone:
Fax:
Phone:
Phone: 2
45
VDH USE ONLY
Health Dept. ID#
Due Date:
540-331-0037
Fax:
Email: as�onatroetirmmenegmLOrent:zom
Block:
Lot:
Acreage: 4.56
Sewage System
Type of Approval: Applicants for new construction are advised to apply for a certification letter to determine if the land is suitable for
a sewage
system and to apply for a construction permit (valid for 18 months) only when ready to build.
❑ Certification Letter ❑ Construction Permit F] Subdivison Approval ❑
Repair
Proposed Use:
Single Family Home (Number of Bedrooms) 5 Multifamily Home (Total # of Bedrooms)
Other (Describe):
Basement Yes Walk -Out Basement? F1 Yes Fixtures in Basement?
Yes
❑ No ❑ No ❑
No
Conditional Permit Desired? ❑ Yes Ej No If yes, what type of conditions are desired?
❑ Reduced Water Flow ❑ Limited Occupancy ❑ Intermittent or seasonal use ❑ Temporary Use (1 yr. maximum)
Do you wish to apply for a betterment loan eligibility letter? ❑ Yes" 0 No
"There is a $50 fee for determination of eligibility.
Water Supply
Will the water supply be ❑ Public or 0 Private Is the water supply ❑ Existing or 0 Proposed
If proposed, is this a replacement well? ❑ Yes 71 No If yes, will the old well be abandoned? ❑ Yes
❑ No
Will any buildings within 50' of the well be termite treated? ❑ Yes [21 No
All Applicants
Is this a private sector OSE/PE application? 0 Yes ❑ No If yes, is the OSE package attached?
2 Yes
❑ No
Is the property intended to serve as your (the owners') principal place of residence? ❑ Yes F] No
In order for VDH of process your application for a sewage system, you must attach a plat of the property and a site sketch.
a
plat of the property is recommenced and a site sketch is required. The site sketch should show your property lines, actual and/or proposed
buildings, and the desired location of your well and/or sewage system. When the site evaluation is conducted, the property lines, building location
and the proposed well and sewage sites must be clearly marked and the property sufficiently visible to see the topography.
I give permission to the Virginia Department of Health to enter onto the property described during normal business hours for the purpose of
processing this application and to perform quality assurance checks of evaluations and designs certified by a private setter Onsite Soil Evaluator
or Professional Engineer as necessary until the sewage disposal system and/or private water supply has been constructed and approved.
0i C L,
1-5 LI
Signature of Owner/Agent Date
TbYMomAwj %%M"M ftVW%Cbd�%"WMArt VA-UMYMON
= U-" Only Dsfa Eruered: Date Doz
FmS HDR) # Fltwww No 0
Faytllsm l pVcka # MHD 0 Rewipt li
Page I of 10
❑ Construction Permit ❑ Repair
Permit
OSE/PE Report For:
❑ Voluntary Upgrade ❑ Certification
Permit
Letter
0 Subdivision Approval
Property Location:
911 Address: TBD City, State, Zip: Afton, VA 22920
Lot: Section: Subdivision:
GPIN or Tax Map #: 69-19D Health Dept. ID #:
Latitude: Longitude:
Owner:
Name: Mountain View Land Trust
Address: 3209 Clarke Lane Charlottesville, VA 22901
Prepared by:
OSE Name: Chris Heltzel License # 1940-001460
Address: PO Box 554, Woodstock, VA 22664
PE Name: License #
Address:
Date of Report: 1211012021 Date of Revision #1:
Date of Revision #2:
iContents/Index of this report:
I
'I1. Cover Sheet 7-8. Well Specifications
�2. Soil Evaluations 9. Site Sketch & Sanitary Survey
3-4. Profiles 10. Site Location
5-6. Abbreviated Designs
Certification Statement
I hereby certify that the evaluations and/or designs contain herein were conducted in accordance with the applicable provisions of the
Sewage Handling & Disposal Regulations (12VAC5-610), the Private Well Regulations (12VAC5-630), the Regulations for Alternative Onsite
Systems (12VAC5-613) and all other applicable laws, regulations, and policies implemented by the Virginia Department of Health. I further
certify that I currently posses any professional license required by the laws and regulations of the Commonwealth that have been duly issued
by the applicable agency charged with licensure to perform the work contained herein. The potential for both conventional and alternative
onsite sewage systems has been discussed with the ownertapplicant.
0 The work attac r page has been conducted under an exemption to the practice of engineering, specifically the
exemption ir%,d, "to ii L 'on 54.1-402.A.11
I recommend that a: ��OonS4r ikp i?f 0 Subdivision Approval be: ❑ Issued
C Ce pgiplBA rs, > e rmit ❑ Voluntary Upgrade ❑ Denied
HELTZEL
Lic No. 1940001460
v., 11oiyna.wc. J Date:
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Page e7— of ko
SOIL SUMMARY REPORT
GENERAL INFORMATION
Date: 9/8/2021 Submitted to: Albemarle County Health Department
Owner: Mountain View Land Trust Telephone Number: 540-331-0037
Address: 3209 Clarke Lane Charlottesville, VA 22901
Agent: Stockton Creek LLC Go Joseph Simpson Address: 455 2nd Street SE, Suite 201 Charlottesville, VA 22902
Property Location: TBD Tax Map/GPIN: 69-19D
Subdivision: Blk/Sec: Site: 13-1
1. Position in Landscape Satisfactory: El Yes ❑ No
Describe: Convex Upland Sideslo e
2. Slope: 11 %
3. Depth to Rock or Impervious Strata: Max. 73"+ Min. None 21
4. Depth to seasonal water table (gray mottling or gray color): Not Observed Yes ❑
5. Free Water Present? 21 No ❑ Yes Range: inches
6. Soil Percolation rate estimated: Yes Texture Group: I ❑ II 0 111 ❑ Iv ❑
❑ No Estimated rate: 50 mpi @ 40"
7. Permeability Test Performed? E1 No ❑ Yes
If yes, note type of test performed and attached results. Test Type: NA
Site Approved. Drainfield to be placed at 40 " depth at site designated on permit.
❑ Site Disapproved. See reasons for rejection.
Reasons for rejection:
1 ❑ Position in Landscape subject to flooding or periodic saturation.
2 ❑ Insufficient depth of suibable soil over hard rock.
3 ❑ Insufficient depth of suitable soil to seasonal water table.
4 ❑ Rates of absorption too slow.
5 ❑ Insufficient area of suitable soil for drainfield and/or reserve area.
6 ❑ Proposed system to close to well.
7 ❑ Other (Specify Below. Add additional pages if necessary)
Additional Notes:
Page'of to
Heltzel Soil Consulting
Property Address: 250/151 Site: 13-1
Tax Map Number: 69-19D Date of Evaluation: 9/8/2021
Profile
Horizon
Depth
Description
Texture
Class
IOYR 4/3 silt loam, weak fine subangular blocky
P1
A
0-9
structure, friable, many roots
III
5YR 6/6 & 7.5YR 5/8 loam, weak medium subangular
Bt
9 28
blocky structure, friable, common roots
II
5YR 5/6 & 7.5YR 7/6 light loam, weak coarse
BCt
28-35
subangular blocky structure, friable, common roots,
II
few 10YR 8/1 lithochromic mottles
5YR 5/6 & IOYR 6/6 light loam, very friable, few
C
35-70
roots, common IOYR 8/1 lithochromic mottles
II
IOYR 4/3 silt loam, weak fine subangular blocky
P2
A
0-10
structure, friable, many roots
III
SYR 6/6 & 7.5YR 5/8 loam, weak medium subangular
Bt
10-30
blocky structure, friable, common roots
II
SYR 5/6 & 7.5YR 7/6 light loam, weak coarse
BCt
30-39
subangular blocky structure, friable, common roots,
II
few 10YR 8/1 lithochromic mottles
SYR 5/6 & 10YR 6/6 light loam, very friable, few
C
39-69
roots, common 10YR 8/1 lithochromic mottles
II
IOYR 4/3 silt loam, weak fine subangular blocky
P3
A
0-9
structure, friable, many roots
III
SYR 6/6 & 7.5YR 5/8 silty clay loam, moderate
Bt
9-28
medium subangular blocky structure, friable,
III
common roots
SYR 5/6 & 7.5YR 7/6 silt loam, weak medium
BCt
28-35
subangular blocky structure, friable, common roots,
III
few 10YR 8/1 lithochromic mottles
SYR 5/6 & 10YR 6/6 silt loam, very friable, few roots,
C
35-70
common IOYR 8/1 lithochromic mottles
III
Page A of 10
P4
A
0 8
10YR 4/3 silt loam, weak fine subangular blocky
III
structure, friable, many roots
5YR 5/6 silty clay loam, moderate medium
Bt
8 27
subangular blocky structure, friable, common roots
III
5YR 5/6 heavy loam, weak medium subangular
BCt
27-41
blocky structure, friable, common roots, few 10YR
II
8/1 lithochromic mottles
C
7.5YR 5/6 & 10YR 8/2 silt loam, very friable, few
41-73
roots
III
PS
A
0-8
10YR 4/3 silt loam, weak fine subangular blocky
III
structure, friable, many roots
5YR 6/6 & 7.5YR 5/8 silty clay loam, moderate
Bt
8-35
medium subangular blocky structure, friable,
III
common roots
5YR 5/6 & 7.5YR 7/6 light silty clay loam, weak
BCt
35-47
medium subangular blocky structure, friable,
III
common roots, few 10YR 8/1 lithochromic mottles
5YR 5/6 & 10YR 6/6 silt loam, very friable, few roots,
C
47-73
common 10YR 8/1 lithochromic mottles
III
Heltzel Soil Consulting
Abbreviated Design - Conventional
Site 13-1 PRIMARY DESIGN
Page Z� of lO
A.
a. Estimated percolation rate. (minutes per inch)
so
b. Recommended trench bottom. inches
40
c. Depth to impervious strata/ or water table/ or limit of evaluation.
(inches)
73
73
73
d. Minimum separation distance required. (inches)
19
18
24
e. Separation distances in inches provided in design.
33
33
33
f. Sloe (percentage)
11
g. Minimum trench bottom due to slope. inches
19.5
h. Is the sloe greater than orequal to 10%?
Yes
i. If Ai is Yes, does 24 inches or greater to rock/impervious strata exist below
Ab?
Yes
j. If yes to Aj, add 1 ft. to the minimum center -to -center spacing beginning at 20%
slope and continue for each 10% slope increase above 20%. If no to Aj, add 1 ft. to the
minimum center -to -center spacing beginning at 10% slope and continue for each 10%
slope increase above 10%. (Report the value, in feet, of the increase in center -to -center
spacing above the minimum).
0
s.
ITrench bottomsquare feet required per bedroom Table 5.4
376
C.
a. Number of bedrooms.
5
b. Gallons per day in design
750
D.
a. Length of trench. feet
100
b. Length of available area. (feet)
100
E.
Width of trench. (feet)
3
F.
Number of trenches.
7
G.
Center-to-centerspacing. feet
9
H.
a. Width required. (feet)
57
b. Width of available area. (feet)
57
I.
Trench bottomsquare footage required.
1880
J.
Trench bottomsquare footage in design.
2100
K
Is a reserve area required? Yes
X INo
a. Percent required?
100%
b. Percent available:
100%
Notes: 'See attached abbreviated design form for reserve"
Heltzel Soil Consulting, LLC
Page ` of td
Abbreviated Design - TL3 Effluent with Trenches
Site 13-1 RESERVE DESIGN
A.
a. Estimated percolation rate. minutes per inch)
50
b. Recommended trench bottom. (inches)
40
c. Depth to impervious strata/ or water table/ or limit of evaluation.
inches
73
73
73
d. Minimum separation distance required. (inches)
18
12
24
e. Separation distances in inches provided in design.
33
33
33
f. Sloe (percentage)
11
g. Minimum trench bottom due to slope . (inches)
11.5
i. Is the sloe greater than orequal to 10%?
Yes
j. If Ai is Yes, does 24 inches or greater to rock/impervious strata exist below
Ab?
Yes
k. If yes to Aj, add 1 ft. to the minimum center -to -center spacing beginning at 20%
slope and continue for each 10% slope increase above 20%. If no to Aj, add 1 ft. to
the minimum center -to -center spacing beginning at 10% slope and continue for each
10% slope increase above 10%. (Report the value, in feet, of the increase in center -to -
center spacing above the minimum).
0
B.
a. Design Type?
TL3
b.Trench bottom square feet required loading rate, gpd1ft2
0.89
c.
a. Number of bedrooms.
5
b. Gallons per day in design
750
D.
a. Length of trench. feet
100
b. Length of available area. (feet)
100
E.
Width of trench. (feet)
3
F.
Number of trenches.
3
G.
Center-to-centerspacing. feet
9
H.
a. Width required. (feet)
21
b. Width of available area. (feet)
21
I.
Trench bottomsquare footage required.
843
J.
Trench bottomsquare footage in design.
900
K.
a. Is a reserve area required? Yes
X
No
b. Percent reauired
100%
c. Percent available
100%
Notes:
ieltzel Soil Consulting
Page? of
VDH USE ONLY
SYSTEM SPECIFICATIONS
HDIN:
Application Information
Name: Mountain View Land Trust
Address: 3209 Clarke Lane
Phone: 540-331-0037
Charlottesville, VA 22901
Location Information
Tax Map/GPIN #: 69-19D
Property Address: TBD
Subdivision:
Section: Block: Lot:
Directions: Corner of Route 250 & Route 151
General Information
Well Purpose (select all that apply): 0 Domestic Drinking Water ❑ Agricultural
❑ Irrigiation ❑
Industrial/Commerical ❑ Geothermal
Well Class: 3B
Minimum Casing Depth: 50 ft.
Estimated Water Usage: 750 gpd
Minimum Grout Depth: 50 ft.
Horizontal Setbacks
Distance from Building Sewer: 50
ft., min. Distance from Pretreatment Unit(s) 50 ft.. min.
Distance Conveyance System: 50
ft., min. Distance to Absoprtion Area: 50 ft., min.
Distance from Property Line: 50 ft
Distance from Foundations: 50 ft., min.
Distance from other source(s) of contamination:
50 ft., min
List other sources: NA
Notes:
This form contains personal information subject to disclosure under the Freedom of Information Act.
Addendum to AOSE/PE Certification Statement
For Private Well Construction Permit
Page � of 10
The proposed well site shown herein,
x— 1. Is located a minimum of 50 feet from all property lines.
0 2. Is located within 50 feet of the adjacent property line(s) but I have determined
that the adjacent property is not used for an agricultural operation.
0 i. Written affirmation from the adjacent property owner(s) that
their property is not used for an agricultural operation.
ii. Other confirmation that land use is not an agricultural operation,
please describe.
0 3. Is located within 50 feet of the adjacent property line where the property is used
for an agricultural operation. For confirmation, I have attached the appropriate
documentation pursuant to § 32.1-176.5:2 of the Code of Virginia.
(check one below)
0 i. Written permission from the adjacent property owner's) for
the well construction.
0 ii. I certify that no other site on the property complies with the Board's
Regulations for the construction of a private well.
Proposed Well Site is located within 50 feet of an Adjacent Property Line(s)
Property is not used for an Agricultural Operation
Statement for Adjacent Property Owner(s):
I affirm that my property is not used for an Agricultural Operation as defined in
§ 3.1-22.29 of the Code of Virginia.
Signature of Property Owner
Date
Proposed Well Site is located within 50 feet of an Adjacent Property Line
Property is used for an Agricultural Operation
Appropriate documentation to comply with § 32. i-176.5:2 of the Code of Virginia:
Written Permission
I grant permission for the construction of the proposed private well described herein
which is within 50 feet of my property line.
Signature of Property Owner Date
Heltzel Soil Consultinq, LLC
PO Box 554, Woodstock VA 22664 c:(540) 331-0037
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PROPOSED WELL
Site Sketch & Sanitary Survey
TM# 69-19D
Albemarle County, VA
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Page I of Iv
ALL KNOWN WELLS & DRAINFIELD SITES WITHIN
200' OF THE PROPOSED DRAINFIELDS ARE SHOWN.
T.M.69-19D
REVISED LOT 3
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December 10, 2021
DRAWN BY: CH
Heltzel foil Consulting, LLPaged of
C Site Location
PO Box 554, Woodstock, VA 22664
200' 400
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