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Southo1d, N. Y. 11971
(516) 765-1938
September 25, 1984
Mr. Irving L. Price
Attorney at Law
828 Front Street
Greenport, NY 11944
Re: Site plan for 382 Wells Road Corp.
located at Arshamomaque
Dear Mr. Price:
The following action was taken by the Planning Board at the
regular meeting of September 24, 1984.
RESOLVED that the Southold Town Planning Board approve the
site plan of 382 Wells Road Corp. for the construction ot a car
was~cated at Arshamomaque, plans dated as last amended
August 13, 1984 subject to this plan being certified by the
Building Department, and a one-year review by the Planning Board
Please forward 6 copies of this site plan for our referral
to the Building Department.
If you have any questions, please don't hesitate to contact
our office.
Very truly yours,
BENNETT ORLOWSKI, JR., CHAIRMAN
~OUTHOLD TOWN PLANNING BOARD~
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By Diane M. Schultze, Secretary
cc: Building Department
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~EL. 765-1802
TOWN OF SOUTHOLD
OFFICE OF BUILDING INSPECTOR
P.O. BOX 728
TOWN HALL
SOUTHOLD. N.Y. 11971
DATE:
June 18,1984
SUBJECT:
Planning Board Members ./
. d . d" el~
V~ctor Lessar , Execut~ve A m~n~strat ~
Certification of Site Plan--382 Wells Road Corp.
TO:
FROM:
Property is located in zone 'B' Light Industrial. The
property was purchased on erroneous advice of the Building
Inspector, so it is now allowable by law.
Off-street parking is to be determined by Planning Board,
100-112 A. Property survey doesn't show any type of drainage,
100-112 E. The property to the north (rear) abutts the railroad
and property zoned 'A' Residential-Agricultural, and requires
screening, 100-134 D 6. The west side may also require screening.
Access to the state Highway will be required per 239K. No
indications of outdoor sign locations (100-134 D 4) and outdoor
lighting locations (100-134 D 3) were indicated. The building
area meets set-back requirements for a business in the 'B' zone.
VL:ec
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Ed-
Do you have a copy of certification for a site plan known as
"382 Wells Road Corp" for construction of a car wash at Main
Road, Arshamomaque. The principal is Robert Ringold.
The survey was last amended August 13, 1984.
Thanks.
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pg (3)
4/9/84
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Pre-submission conference:
7:45 p.m. Mr. Coster, Mrs. Coster and R. Terry esq were
present to discuss the Coster's proposed site plan for
a funeral home located at Southold. Mr. Coster explained
that they would be using an existing building and adding
to the rear of this building approximatelY 30' X 60'. He
further stated that this area would be the two chapels.
He also said that the exterior of the building will remain
the same and the interior would only be moderatly changed.
The proposed addition would match the exterior at the
sellor's request and the applicant's desire that theaddition
conform to the existing building. The Board stated that they
would be amenable to this as it is one of the older buildings
in the hamlet, and would want to see it remain architecturally
the same. The Chairman questioned if Mr. Coster made any
application to the Department of Transportation with reagard
to the curb cuts and the applicant stated that he had not
done so. The Chairman questioned whether the proposed fence
would be necessary behind the building as the property to
the North is business. He stated the plantings may be
sufficient and the applicant agreed that the too preferred
this and would like a white picket fence around the rest of
the property. The Chairman explained to the Board that
the file contained endorsements as to Mr. Coster's character
and noted that it was very encouraging to see such good
endorsements. Mr. Latham had a question with regard to the
roof of the building and the applicant stated that the roof of additi,
will also match the building. Mr. Mullen had a concern with
the availability of parking area, he noted that the plan
indicates parking for 52 cars and questioned how many service
vehichles the business will utilize. Mr. Coster stated that
he intended to rent the funeral service cars, there would
be only 2 cars at best, those being his own car and a service
car.
On a motion made by Mr. Wall, seconded by Mr. Latham it was
RESOLVED that the Southold Town Plannnig Board will conduct
a field inspection of the property and simultaneously refer
the site plan to the Building Department for certification.
This site plan is for the construction of an addition to an
existing building and to create a funeral parlor in the building,
located at Southold.
Vote of the Board: Ayes: Raynor, Mullen, Orlowski, Latham
Wal
Mr. Terry, esq, who was present to represent the seller of the
property of the proposed funeral home, requested that the
Board act as quickly as possible as his client was anxious
to sell it. The Board confirmed that it would be handled
as expeditiously as possible.
* * * * * * * * * * *
Pre-submission conference:
8:00 p.m.-Mr.Robert Ringold of 382 Wells Road Corp. was
present to discuss his proposed site plan for a car wash
located at Southold. Mr.Ringold explained to the Board
that the car wash proposed would be similiar to the present
car wash he operates in Laurel, same building, same operation.
. .
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pg (4)
.
4/9/84
A.\Si
Mr. Ringold stated the site plan would have 15% landscaping,
and the traffic flow would be to the East and the DEC has
noted that the property is not in its jurisdiction. The
Board questioned the proceedure used percolation. Mr.
Ringold explained the process he uses is a filtration system
which prevents any water from going into the ground which
must be approved before the building department can issue
a permit. The further explained that the system filters
out the bacteria and water is recycled, the system is
presently approved by the Department of Health Services in
Suffolk County.
(
On a motion made by Mr. Wall, seconded by Mr. Orlowski it was
RESOLVED that the Southold Town Planning Board will make a
fie~d inspection of the proposed site plan of Robert Rinqold
for a carwash located at Southold and simultaneously refer
the same site plan to the Buildinq Department for certification.
Vote of the Board: Ayes: Raynor, Latham, Mullen, Orlowski, Wall
* * * * * * * * * *
Mr. William Esseks was present to discuss the proposed cluster
~eveiopment or NLChOlas ShLCk located at Orient. Mr. Esseks
sUDmLttea the Sketch map ot the cluster and noted that it is
to be single and seperate from the hotel property. Mr. Esseks
stated that they are no longer persuing the proposal of greater
density and will instead persue the proposal with 20 cluster. (
lots. Mr. Raynor questioned if the area for cluster had been
computed with the hotel property as it was noted that the
duster is not to contain the hotel property. Howard Young
was present and at this time came before the Board to explain
that it has been computed without the hotel. Howard Young
also certified that the map dated August 27, 1983 was the
same map presented to the Town Board for their approval of
the cluster concept, and the only 2-acre cluster map before any
Board in the Town of Southold. Mr. Raynor read correspondence
from the Town Clerk that the Town Board had by resolution on 11/15/83
approved the cluster concept for property of Nicholas Schick
located at Orient Point, NY.
On a motion made by Mr. Wall, seconded by Mr. Mullen, it was
RESOLVED that the Southold Town Planning Board declares itself
lead agency with regard to the cluster development of Nicholas
~ChLCK locatea at or Lent unaer the State Environmental Quality
rteVLew ACt. An LnLtLal aetermLnatLon of non-significance has
been maae. The Board requests that a Long Environmental Form be filed
Vote of the Board: Raynor, Mullen, Latham, Orlowski, Wall
The Chairman noted in the minutes that there has been a change in
counsel representing Mr. Nicholas Schick, the new attorney
is William Esseks. Mr.Esseks questioned if the Board will require
a map indicating 5' contours and drainage, the Board stated c:
as per the ordinance it will be required.
. . . . . . . . . .
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TEL. 765-1802
TOWN OF SOUTHOLD
OFFICE OF BUILDING INSPECTOR
P.O. BOX 728
TOWN HALL
SOUTHOLD. N.Y. 11971
DATE:
June 18, 1984
SUBJECT:
Planning Board Members ~
Victor Lessard, Executive Administrat~
Certification of Site Plan--382 Wells Road Corp.
TO:
FROM:
Property is located in zone 'B' Light,Industrial. The
property was purchased on erroneous advice of the Building
Inspector, so it is now allowable by law.
Off-street parking is to be determined by Planning Board,
100-112 A. Property survey doesn't show any type of drainage,
100-112 E. The property to the north (rear) abutts the railroad
and property zoned 'A' Residential-Agricultural, and requires
screening, 100-134 D 6. The west side may also require screening.
Access to the State Highway will be required per 239K. No
indications of outdoor sign locations (100-134 D 4) and outdoor
lighting locations (100-134 D 3) were indicated. The building
area meets set-back requirements for a business in the 'B' zone.
VL:ec
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COUNTY OF SUFFOLK
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AUG 28 J984
PETER F. COHALAN
SUFFOLK COUNTY EXECUTIVE
SOIL AND WATER CONSERVATION DISTRICT
August 27, 1984
STANLEY A. PAUZER
DISTRICT MANAGER
Mr. Bennett Orlowski, Jr., Chairman
Southold Town Planning Board
Main Road
Southold, NY 11971
Dear Mr. Orlowski:
In response to your report to review the site plan for a proposed car wash,
I am forwarding to you a report prepared by Allan Connell, District Conserva_
tionist for the USDA, Soil Conservation Service. I am sure you will find this
report useful in arriving at a decision on this project and if you have any
questions or need any further information, please contact me.
Sincerely,
.~a~
Stanley A. Pauzer
District Manager
Attachment
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~,"(ll' It,\'V''I.
127 EAST MAIN STREET
RIVERHEAO. NEW YORK 1 1901
1516l727-2315
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United States
Department of
Agriculture
Soil
Conservation
Service
127 East Main
Riverhead, NY
Street
11901
August 27, 1984
Mr. Stanley A. Pauzer, District Manager
Suffolk County Soil & Water
Conservation District
127 East Main Street
Riverhead, NY 11901
Dear Stan:
An on-site visit to the proposed car wash site revealed the following:
The soil appeared to be Berryland mucky sand (Bd). There may also be some
Sudbury sandy loam (Su) present since the soil map indicates that the site
falls between these two soil types. The profile of the test hole augered in
the center of the property resembled Berryland mucky sand.
The Berryland soil is found between areas of tidal marsh and better drained
uplands. In this case Route 25 separates the tidal marsh from this wet area.
This soil has approximately 10 inches of organic matter at the surface followed
by a layer of black mucky sand. Below this are layers of sand that contain
large accumulations of organic matter.
A high water table is present at the surface or within 6 inches of the surface
most of the year. During my investigation the water table was at a depth of
approximately 18 inches.
Due to a lack of a suitable outlet this property would be very difficult to
drain. This would appear to be a major limitation to the proposed use due to
the large volume of runoff created in a car wash operation. There would be no
downward percolation of runoff into the soil profile as is the common practice
due to the high water table condition.
The vegetation and soil type are indicative of a wetland condition. The soil
has severe limitations for construction due to its mucky nature.
If I can be of further assistance, please let me know.
;Wl~
Allan S. Connell
District Conservationist
.t}
The Soil Conservation Service
is an agency of the
Department of Agriculture
SCS-AS-1
10-79
SUFFOLK COUN'l'Y, NfOW YORK
"!flUer conc;i,Js of partly decomposed plant tibers. 'l'llB
mrface layer is black mueley sand 1 inch thick. It is
;llderlain b:r a subsurface layer of grayish-broy,rn, loose
and to a d"])th of 5 inches. The upper part of the sub-
(IiI. to a dq)th of abollt 10 inches, consists or Vd'y dark
~Tayish-brO\vll. friablf' sand that contains large aceumula-
ions of org:anic matter. The lower part of the subsoil
fJllsists of brown to dade-brown loose sand to a depth of
hnut ~() lrwhr.s and grayish-brown sand to n. depth of
hollt. ~3() 111r110s. The suhstrat.um, to a depth of 52 inches,
: light ()lin~-gTfLJr loose sand.
Bl'JTylnnd soils have. a high water table, The water
dll(> is at tlw snrfaee or within 6 inches of the surface
io~t of tJw year. Permeability is rapid. If the water
:lhlu is ]owf>I'rd by dr:dnngc, these soils have very low
',>aihlJlc moisture capaeity. These soils are strongly acid
') yery stTongly acid t.hroughout. Natural fertility is
~\Y. Hooting depth is limited mainly to tho upP~~r G to
~! jnchrs. -
Heprcsentntlve profile of Berryland mucky sand, in a
oodcd area, onc-fourt.h mile cast of the edge of the. vil-
',1rC of Sng l-Tnrbor Oll State Route 114; 200 yards north
f ldghway:
01"-]0 to S incheR, dark rerldi:"1h-hrown (tiYR 3/4) loose leave::;
nnd pnrtly decomposed organic matter.
02-8 inejJf's to 0, hlnck (5YR 2/1) decomposed organic mate-
r.i.ul, heaVily mutted with roots; abruvt, ~mooth
boundary.
.'\1---0 to ] inch, black (10YR 2/1) mUCky sand; m::u;"lve;
T'ery fria hIe; very strongly acid j abrupt, srnootlt
boundary.
A2---1 to fj inche8. grnyish.hrown (lOYR 5/2) sand j sirlgle
t-;rrriI:; loose; a few roots j very strongly ncid; clear,
smooth boUndary.
E21h-5 to 10 inches, very dark graylsh.brown (IOYR 3/2)
sand; nWRsive; friable j a few roots; very strongly
acid; graduaL wavy boundary.
D22-10 in :20 inchc:"1, brown to dark-brown (IOYR 4/3) sand j
single grain; 1008('; a few roots; strongly ncid j
gradual, ',".'!tvy boundary.
B3-~o to 30 inches, grayish-brown (2.5Y 5/2) sand j single
grain: loose; vl'ry strongly acid j gradual, wavy
boundary.
C--30 to G2 inches, light Olive-gray (5Y 6/2) sand; single
gmin ; loose; strongly actd.
The solum ranges from 28 to 40 inches in thiclme.o;s. It is
dominantly sand. but ranges to loamy flwd ill places. '.rhe
solum generall}' is free of coarse frugments, l:ut in old cban.
nel bottoms, the B horizon lws as much as 15 percent Coarse
fragments. Heaction rang<,-s from strongly ndd to vcry
strongly add in tlle solum. The 0 horizon ranges from G to 16
inches in thickness.
The Al horizon is dominnntly black (10YR 2/1 or N 2/0).
T.he Al horizon is massive or the structure is weak granular.
'rbe A2 horizon ran~es from very dark gray (lOYR 3/1) to
grnyisb hrown (IOYl{ G/2). It is mainly sand, hut ranges to
loamy sand in places. The A2 llOrizon is domiua.ntly single
grain, hut wllere the profile has a we~kly exprcBscd A2 hod.
20ll, it rnnges to massive.
'l'he B2Jh horizon ranges from dark reddish brown {5YR
:l/2} to vpry dark brO\"vIl (JOYR 2/2). A chroma of 2 is domi~
nunt. 'I'exture ranges from sand to loamy sand. Consistence
is friable or firm. The B22 horizon ranges from dark reddish
hrowu (GYR 3/2) to brown to dark brown (lOYR 4/3). 'J'he
B2:2 horizon is more stronrrJy developed where the fhctuation
of the ground water level is greater. Tb.e lOwer Dart of tIle n
horizon ranges from pule brown (10YR (j/3) to grayiSh
brown (2.5Y 5/2). Texture is sand or loamy f;and. In places
this horizon contains COar::;e mottles that have n chroma of
m.ore than 2.
The C horizon g-enerally ranges 'from olive gray (GY 5/2)
to pale brown (10YR 6/3), but in u few places wh::re organic
63
(' t!uinlng has penetrnted deep Jnto the profile" value Is as low
'tiS a. Texture ranges from sand to grayclly ~mnd in this horf.
::Oll.
Berry land Salls are near Atsion soils. Der-ryland soils are
fjimHar to these salls, but they have a thicker organic sur-
hce horizon and II higher perennial water table.. They are
al~o nc>ar Walpole and Wareham soils, \,.blcb are IJetter
drained find finer textnred, hut whieh lack n B horizon that
has an accumulation of humus.
Berryland mucky sand (Bdl.-This is the only Berrv-
Iond soil mapped in the county. This wet soil is through-
out the county along the margins of tidal marshes.
ponds, creeks, and streams. Areas of this soil generally
arc small and round or long and narrow,
Included with this soil in mapping arc ~man areas of
Muck and of Atsion and -Wareham soils. Also included
arc a few small areas of finer textured soils that are verv
poorly drained. Some of these included soils, esperia]])-
along- Carmans River and Connetqllot, HiveI', do not,
lw"vo- a well. defined gray subsurfnee layClL" and subsoil
tllut have a large accumulation o:f humus. Also included
along the Peconic River arc very poorl.r' drained cran-
berry bogs that are essentially Be_rryland soils that have
had sand spread on the surface.
Tho hazard of erosion is slight on this Herryland soil.
The vcry high ,vater table in this soil sev('ret~: limits it. for
hath fann and nonfarm UseR. A lack of SUitable outlets
JIlHkcs this soil very diliiclIlt to drain. ~loSL al'pas calt Iw
used as habitat for SOIne types of wildlife.
None of this soil has been cleared. l\iost areas are in
hrush or trees, except along the shore in the southwest-
ern part of the county, where small are:.~s have been
filled to provide sites for homes. Only one commerl'ial
cn.1.ubcrry bog is in operation. The other bogs have been
allowed to revert to their original condition and arc
growing up in water-tolerant grasses and shrubs. Capa-
bjlity unit Vw-l; woodbnd suitability group 5w2.
Bridgehampton Series
The Bridgehampton series consists of deep, well
dmined to moderately well drained, medium-textured
soils that formed in thiek silty deposits over coarse sand
and gravel. Bridgehampton soils are only on the south
fork of the county in an area extending eastward from
the village of Sonthampton to Amagllnsett. These soils
gOJl{~ral1y are nearly level to gently sloping and are
mainly on flat outwash plains, but a small area of these
soils is near ~font.a.uk on uneven moraines, and slope is
as nmch as 12 percent.
In a representative profile the surface layer is dark-
brown silt loam 11 inches thick. The upper part of the
subsoil, to a depth of about 23 inches, is yelJo\vish-brown
and light olive-brown, friable silt loam. Below, t.o a
depth of about 34 inches, is friable, olive silt loam that
contains grayish-bl"own and yellowish-bro\vJl mottl<'s.
The lower part of the subsoil, to a depth of 55 inches, is
strong-brown, friable silt loam and very fine sandy loam
that contains yellowish.bl'own and olive-gray streaks.
The substratum is yellowish-red to yellowish-brown loose
sand and gravel to a depth of 80 inches.
Bridgehampton soils have a high available moisture
capacity. Natural fertility is low, but crops respond well
to applications of lime and fertilizer. Roaction is
strongly acid to very strongly acid in the solum and
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The hnzard of erosion is sJigJ]t to moderate on this
S('io soil. The main concern of management is control-
ling- runoff and (,fasion. This soil generally is wet enr1y
in spring~ Dnd it warms up Jate. Consequently, tillage
gl'llpraIlv is ch-:-layed.
This s'oil is well snit.ed to all crops commonly groWIl in
the county. 11 is I11ninly in trees or brush. Small areas
are' used .i'or grass or CI:OpS. Most areas that are used for
('rops are on the moraine near Wading River. Because
ill(' compact tiJJ in this soil is somewhat difficult to exea-
n1/"('. irs lISC fol' engineering works is more costly than it
is for the 8[111(1\. substratum Seio soils. Inasmuch as the
tin is 1"\"(,11 ~T[Hl('d and contains sufIlcicnt fines, it is suita-
hk for uso as road fill and as binder material in other
('otlstrUrl ion wOJ'k. Capability unit lIe-I; woodland
suitahility gronp ;{o1.
Scio silt loam, sandy substratum, 0 to 2 percent
slopes ISdAI.-'1'his nearly level soil is in small, low-lying
\\'pt :II'(l~!" within large units of I-Iaven soils or in Iow-
i\'illg a 1'(':1,'-" u011\,('('n poorly drained to somewhat poorly
dClill('d HaynlW])j soils and adjacent well-drained Jlaven
soils. It is thl'ougllOut the county but generally is 011 out-
wash plains.
The profile of t his soil is similar to the proJile of tlw
soil desct'ib(\d as representative of t,he series, except that
it, oyprlips 1008(' sand and gravel and the texture of its
slll'facp lnY0r and subsoil ranges from silt loam to loam.
Included with this Scio soil in mapping are small
:II'('a8 of 'slldbllry snndy loam and 1-ValpoJe sandy loam.
Also lllclu(1c-'d n1'(\ small arcas of IIaven loam, thICk 8Ur-
fa('(. I:-tvpr, tlJnl has a mottled snbsoil.
Th(" hn%ard of erosion is sligllt. Because of wetness,
This soi11yarHls slowly in spring and cannot be plowed as
e:!rh. as '"pll-drained soils.
Tjli~ soil is wp/J snited t.o all crops commonly grown in
thp (,Ollllty. ex('(\pt Whell it occurs in depressional areas
Olat :ll'(~ Ji1>('1\' 10 r('('(~ive excessive surface wat.er from
IIP:Il'hy ~IoJling :ll'("'as. A large part. of this,soil is elearerl
arid is lls('d ,ril11 lnrg-c tracts of .Haven' soiJs for pota-
t!/rs. cauliflowe1'. onions, ana otlwT truck crops. It is
;d~o llsrd for sod. In the westcrn part of the eounty, this
sniJ is IIspd wit 11 ot h('l' soils fiS sites for housing develop-
Il1i'l1tS. (1,lpability ullit 1Iw-1; woodland suit.ability
uJ'Onp ;101.
Scio silt loam. sandy substratum, 2 to 6 percent
slopes (SdBi.--This soil is throughont the county on
11\'ll':\II1('S ,IlHI 01l1W:18h plains. It. is on gentle side slopes
of d"JWPsslons or in nreas between well-drained Haven
so;1s and 100Y('1' lying arcas of somewhat poorly drained
sods. Arras of this mapping unit are small, and they
III:ll;:t' 1lJ> a \'pI'Y small part of tho total acreage of the
I'Ollll1y.
'I'll:' profik of This soil is similar to the profile of the
soil dl's(,J'ibpd ns reprpscmt.at.ivc of the series, except that
il ')\'('rli('s loose sand nnd gravel and its subsoil is silt
joam or loanL
III('Jl!ded with this soil in mapping are small aren.s of
adj:H'('nt lfayen soils on higher elevations. Also included
art' wd spots of 'Valpole soils. These soils are indicated
OIl th(' detailed map by t.he conventional symbol for a
wet, spot,
'1']10 hnzanl of erosion is moderate to slight. on this
Scio soil. If it is used for erops, measures are needed to
help to control erosion.
.
SOIL SURVEY
This soil is wrll suited to all crops commonly gro\,
t.]w county. Much or this soil is cleared and is used
1nT[~C tr:1cts of Have:n soils for potatoes and other t
crop:.>. ..Arens of this soil and areas of adjoining b
drained soils are used for honsing developments. C
bility unit lIe-I; woodland suitability group 301.
SUdbury Se1ie~
The Sudbury series consists of deep~ moderately
drained, moderately coarse textured soils that :former
a mantle, of fine sandy loam or sandy Imnn over co!
sand and gravel. Tlleso soils are throughout the cou
on outwnsh plains and moraines. They generany arc
low-lying arcas between somewhat poorly drained :
poorly drained 1Valpole soils and wen-drained Ri,
head saits. Slopes rllH,q:e from 0 to 3 percent, and slo
arc concave in many places.
In a representative profile: a thin layer of leaf lih
twigs, fwd d(~COmp08pd organic matter about 2 inc
thick is on the surface in wooded areas. Below this n
is a SHl'Tnce laver of dark-gr:JN sandy loam. In cult-ivai
arc~s the sl1rf~ce Inyel' is mix'ed with material or~gina
in the upper part of the subsoil, forming a dar'k .g-I'ayi~
brown plow layer of sandy loam about 9 inches thick. 1
sllbsoil extr:uds to a depth of abollt 24- inches. It. is friab
light olive-hrown sandy loam that is distinctly mottl
below It dept.h of about 13 inch"s. The snbslratllm to
depth of 21 inches is mottled, friable, olive loam.v san
TllO nr.xt, layer is grayish-brolvn, vpry friable loamy sar
to a depth of ahont 36 inches. Below t.his, to a dept.h ,
about 51 inches, it is loose, pale-brown stratified sand ar
gravel.
This solI has moderate to high available moist.m
eapncity. The depth of the water table ranges from IS I
24. inchC'R in wet periods; hO'i'irpvcl', in some dr,v pcnod:
it is below 30 inches. PprmeabiJitv is moderate to mocl(,l
a.tely rapid in the sllr:fnce layer fl'nd subsoil and rapid i.
the subst.rat.um. Natural :fertility is low. Reaction 1
st.rongly lleid or very strong-I."\.' acid t,hroughout. Crop
responci fairly well t.o applications of lime and fertilize!
The root, %01W is in t.he upper 24 to :W inches.
Rcprps~ntnJ.ive profile of Slldbury sandy loam, in [
,vooded arf'fl, one-fonrth mil(' ]']orth of lTallppall,g('-K(Is
Con set Hond, C.R. 85 alld ollc-half mile Wf'sl of Terl'."
Hoad:
01-2 iO('h03 to 1 inch, loose leave;;; und twigs.
02---1 inch to 0, dccomposf'd organic matter.
A2-0 to 1. inell, dnrk-gray (!OYH 4/1) sand.v loam: \Vf'<1k,
finn, granular structure; vcry friable; man.\' tinp
roots; strongly acid; c-'enr, smooth houndary.
B21-1 to 13 inches, light olh'~browIl (2.5Y 5/4) f;an(]y
loam; Q few, fiue, faint, ~n'lJowish.brown mottlp;:;;
weak, coarse, subunguIal' hlot'ky structure; friahIp;
many fine roots; strongI:v acid; dear, smooth uouLHI-
ary.
B22-13 to 24 inches, light Oli1!e-brown (2.5Y 0/4) .<:andy
lonm; a few, fine, distinct, strong-brown, and It ff'\\',
me'Hum, distinct, light b:rownish-gray mottl('s; Weak.
COf!J'f,f", r;uhangular bIoeky structure; friable; a ft!w
roots; strongly acid; clear, smooth boundary.
1101-24 to Rl inches, olive (5Y 5/3) loamy sand; c.ommoll,
medium, distinct, strollt::"-hrowll mottles and COmm01l.
medium, faint, o]jye-gray mottles; massive; frinhh"
a f':,'w I'Oots; strongly add; clear. smovth boundary.
II02--31 1:0 30 inches, graYisb-brown (2.5Y 5/2) loamy sanrI:
mns"ive; very friable; a few roots; strongly acid;
clear, smooth boundary.
-
--
r::,",(:Ti';:'0~J-:-\. CC7;"-;'T":r, NE"';"T YO~3:.
S7
IlIC3-36 to 51 inches, pale-brown (lOYR 0/31 t.j nun d :~" d
and gravel; siugle grain; luose;: :1.r(( It lil (~
gra vel; strongly acid.
The solum ran~es from 20 to 40 inches in t1 '(~";:V"S. D>rrl:h
to underlying Hand and gravel ranges from ~JJ I:) <0 iIl{ IJ('fL
'l'he content of coarse fragments range.'] from 0 t<) :t') j;!'l\::Vjt
in the solum and from 10 to 35 percent in Liw H IHl rallHr,.
Reaction rUIlg"es from strongly acid. to vcrs f:n()l!{ly :w:~J
throughout. 'l'extnrc ranges from tine sandy )OEll to Hauliy
lo:~m in all Ilorlzons of the solum excelli in 1i;{~ n~ 11{jl'L~o,rl.
Texture in the substratum is COa1'8e sal~d, h:nlJ 1;;1 'ld, (1-:'
stratified sa no and gravel.
'['he A1 horizo:l ranges from very dark browIl (WVlt 2/2)
10 brown or dnrl{ brown (lOYR 4/3), StrnctuO:2 !~UjiW,:i fl'Olll
weak to JJlo(krnt(', fine, granular, COW:;iKtpll('(' i:; 1';']"/11,, OJ'
v{'J'y frinhif'.
In ('ultivnf('ll areas an Ap horizon runges L'om brOIVll or
dal'k hruwn (lOYH "1/3) to dark grayish Lrowil (lO~{H 4/2)
It. ran.L':('~ frOlli 8 to 10 ine!)('s ill thicknes.'1,
'J'lJe -A~ horizon rang'E'S from dark gray (lOYIl1/1) II) gray
(lOYH. :)/1). ;-;rrl.Jt'Jurp rangeI': fnllll \Yl'ak to IBod.)!"al". tiUE'
grnnu]llr. Consistenr:e is very fMalJle or friable. In pIllc( ,'j t.b~
1\2 horizQf1 ]111:, 11 \'('l'Y thin brown to dark-lnO\vH ('1.GYH 4/4)
iJorizOllllJat: ('old:nius an u('culIIulatioll of iron l"wd JULlllS
'l'lw B21 horizon rnnges from ;relloy,rh:h browIl (lOYH G/l))
in light olive browll (2.GY 5/4). The .l:;2~~ l:oJ'.i.~(jn r.Uig(;,'j from
~'elJo"dsh broWIl (10YH 5/4) to olive (GY fi/4) , lJi;,Lind
browllish and J~ra.rish mottles arc llre::::<:nt at u dl.'~;~h of ]5 to
It; iudlC'S. The B horizon is nwssive and has wl'ak, ('cau,,', suL-
fJng-u]ur blocky stJ'1wtur~. C01J:~ist(,!l('e i8 friHble or very fl-j,dJle,
The thin, traw;i1ional loamy sund (11 and (;:2 horizons are
grayish brown (2.(jY 5/2) to olive (5Y 5/3). 'l~hl~Y ure lllas-
I~ive or single grain, Consistence r:lngi.:3 fl'ODl friable to loo.oe,
Till' lower Jlart. of ihe C horizon ralJges frum IJale lH'OWH
(lOYH 6/3) to gray (lOYR 5/1). 'l'hey ~lre single gIain. Con-
sjslf!11ce is JOOSt'.
:-ludblll'Y soiJ.~ nre slightly more olive in the upper part of
the n horizon Ihan the uefined range for the series. This dif-
f('renel' dOES not alter their usefulness or behavior.
Sudllllry soi]:..; are associated witb niverhead, Seio, llnd
Walpo]{' soils. ~uduury soils are similar to these soils, uut
Hin:>rlJe:ld soil!': lack the seasonal l1igh \\'ater table ntul the
distinet motUI$ in the B horizon of Sudbury soils. They are
similar to Seio soilf:; in drainage, but they lJave u sandier
solum. \ValJloJp soils are not so \vell drained as Sudbury
soils, and they :ue gray(>r throughout tbe !SolUm. -
Sudbury sandy loam (Sul.-This is the only Sudbury
soil mapp(:u ill tlw count.y. TIlis lwarly level .soil is
bChveen areas of more poorly drained soils and adjoin-
ing ,veIl-drained soils of the Rivcrhead series. In a few
places this soil is in the bottom of c10Si~d deprc;Jsioll,s in
large tl'ucts of Hin:rhead sandy Joams. Aiost areas are
small.
hwlllded ,,,it.h this soil in mapping are small areas of
Walpo]e soils in wet spots and of well-drained Hiver-
head soils on ltjg-her elevations. Gently sloping, moder-
atelv well drained sandy loams are also incllloed,
Tiw hazard of erosi;n is slight on this Sudbury soil.
If fliP inrluded wet. nreas arc cnltivated. artificial drain-
agcl, is 1lC'(lded. Becallse of wetness. this soil warms slowly
in spring and eannot hp plowed ns early as well-drained
soils. In deprpssional areas t.his soil ponds in ,vinter, und
winter crops am damaged.
This soil is well suited to all crops commonly OTOWll in
the C'OllJlty-. The only areas that have been clc~Ted for
farming. (l'rC' spot-s is~1ated in large tl'aets of well~drained
.c;oils. }\Jost Jar:2'p arcas that. are next. to sons where drnin-
~!f-~t' i~ r~()(~r tire wooded, This soil is used for building
~lj('S 1:F It: IS part. of a larger development area, Capabil-
It.y Illllt 1 J w-1 ; ,,,oodland ~uitabiIity gronp 301.
-..,.
'~
.'"
....
..;,.-.
'T'iIJd rH:WGh
Tidal marsh {Tm} is made up of wet arcas t.hnt an~
throu!:hollt the eounty arOlmd the borders of caluH'1'
rmbayrnellfs :md tidal creeks. These level an'aH n ro not
inull(lrJed by daily tide flow, IHlt. the',y alT, sl,hj('('~ 10
flooding during' abnormally high moon or storm t I(/('S.
r~I:'he areas range from about 2 to several hundrpd acre'S.
Tidal marsh has an organic mat on the slll'facl' that
ranges from a few inches to sen~ral feet in t hic!nH's'<-;.
'I'he OJ.gaJlic mat overlies pale-gray or whitt' S:llld. III
Illany places the profile of the man:;h is made lip of ~d((lr-
l1ating layers of sand and org-:mic material as a 1'1'::1111, of'
s:tnd deposited OIl t.he organic, rnat during abllOrlllttll.y
high storm tides.
Ineluded wit.h this land t.ypo in mapping an', al'(';l$ of
tidal marsh that. adjoin dunes. Sand that blows frolll j II('
dlln<'s covers tlH'se areas. In many of t.hE's!' pln('(',~, the
dunes have completely encircled t.he marsh, nl1d j he
marsh is no 10ngeJ' directly connpcted to a body 0 r sa 11
watcr.
These very poorly drained areas are not suited 10 any
kind of farming. They are best suited to use as }wbitaL
for certain t.ypes of wildlife. Capability unit VIJ"'-~I;
woodland suitability gronp not assignc(1.
Urban Land
lJrbnn J:-~nd fUr) consists of areas that. are moT'(' thall 80
percent' ~aYeI'-ed by buildings and pavements. EXflmpl('~
are parking- lots, business districts cl>f lal'g-er \.illnges, :lnd
densely developed industrial parks. Examination and
identiGcation of the soils in these areas are impract ic:! L
Capability unit not assigned; woodland suitahilit.y grOllp
not assigned.
Wallington Series
'rhe "\Vallington sl'ries consists of doe,p, somewhat,
poorly orained, medium-textuI'e'u soils that. lw\rp a fragl-
pan at a depth of 18 to 2c1 inches. They formed in a
mantIe of silty material over thick deposits of moder-
ately coarse textured or eoarsp textured matt'r'ial, Thpse
soils arc in flw 1\fontauk Point, an'u. of the l'Ollllt \. and
ilre in lmv-lying- urcas along- drainagewa.:rs and 11(':1']' per-
('Hnial ponds. Slopes are 0 t.o !) pe'l'ecnt. Natln> n';2'I>tn-
tion consists of shadbush, blueherry, and alder.
In a rppI'('~;pnt.at.ive profile of a till :'-111bstl'atlltll ph:ISP.;1
thin layer of lean's and ol't:!anic mnU(lf' is on tfj(l sl:t'f,l/'('
in \"ooded areas. Below this la\'or is a 81l1'[;](,(' 1:1 \'('1' o/'
very dark ,.!.!THV silt loam abo"ll :? )111'fw,", j hick 1"\('1' n
snbsltrface Ja:r(_'-l' of grayish-hrown to light hro\\ II i~h-
g-ra.y silt 10n111 t.hat. has a few di:'-1tilld Ill()ttl('~. 'I'll" ,''';l1h-
surfnce laypr extends to a depth of allout 10 illrJl('~, 'I'll('
upper part of the snbsoil, to a depth of about L<;;'; i]wIH':-:.
is mottled, grayish-brown, fl'inhlf'. silt Joan!. TIll' )0\\('1'
part. of the subsoil, to a dl~pth of :W illchps. is lllllttl{.(1
light olive-brown silt loam that lnakes up <I {inn and
brittle fru{.!:'ipan. The Sl1bstratmn to a dl'pth of 17 il]('IH'~
is mottled gray to lig-ht-gray, friahle :",ilt, loam. He!o\\'1 to
n. de.pth of nhollt (i0 inrhcs, till'. ~lJh~t.r:ltllnl ('oll.--.:i:;/,--,: of
fir'm. st.rong-brown fine snndv ]Oillll .!.d:1cial jill.
"\Vallington soils have a 'hip:h \~'aj('r J-ah/(' wil!lio fi
inches of the surface during wet, prrioc1."1 but. it drops to
.-"'"'->C"'-'~
...."..
. ""'WI'
.....__.--,~,
.
Southold, N. Y. 11971
(516) 765-1938
August 7, 1984
Mr. Stan Pauzer
US Department of Agriculture
Soil and Conservation Service
Riverhead, NY 11901
Dear Mr. Pauzer:
Enclosed is a copy of a site plan for a car wash, which
is a proposal before the Planning Board for approval.
Also enclosed is a copy of a tax map of the area.
Would you please review the site and report to us
your findings.
FollOwing a field inspection by the Town Planner, we are
concerned with the possibility or a wetlands area, as well
as, the feasibility of the proposal.
Thank you for your assistance in this matter.
Very truly yours,
enc.
BENNETT ORLOWSKI, JR., CHAIRMAN
SOUTHOLD TOWN PLANNING BOARD
D-tA---^----CCt: O~Uo~> L, (l
By Diane M. SChultze, SecretaryfC-
'ci'14
NEW YOIlK STATE DEP.....lri' OF_E~mr.OmlENTAL COllSERVAT.
Regulatory Affairs Unit ______. .
Bldg. 40, SUliY--RoolII 21.9---- ...----
Stony Il:rook.. NY '11794
_ .-...-" ' (516) 751-7900
../V,:flfllVrn ~. rpR IC~ Je. J. ):).7 )8</
~ 2.8 t-l<.bNT S-+REE, 0 \ R J
d -I-oR 382. W~l S Of.) Corp
GreEuf'o'.<.II N,e...J 11l"K.
~~_~fOe/"~ c ~ ~lS2. LJ-el\5 ROA1l Corp AI ARShAtnCmA'i'U~
Dear '0\ R.. ?r-ic...-e I .
.Areviewhasbeenmadeofyour!'roposal.to: C.Q~Trv~\ A- bu;\cl~.,,)' .
O~ '&0-.,& propH-4-1 ll:lekl.l,..I{2.ecO A<.::. SCT~ IOOO,S"{'/II~"""'d3
Locatioti: 1Jc..~ o-C:' Yl\ I\~ ~ Roll t1. So~+Q.. <> ~ k .T. R. f2. A R.s hA n--. 0 m A- 'l ",e.
lOw...:! oC S:..AR..1 J I C<>,,),...)~ 0 ~ S'.)(:~<..lll<.
New York State Department of Environmental Conservation has found the
)(' parcel project to be:
XGreater than 300 I from inventoried tidal wetlands.
~ Landward of a substantial man-made structure m AI~ K 0 A d
greater than 100' in lenp,th constructed prior to September 20, 19J7.
Landward of 10' contour elevation above mean sea level on a gradual, nat-
ural slope.
Landward of topographical crest of bluff, cliff or dune in excess of 10
feet in elevation above mean sea level.
Therefore, no permit under Article 25 (Tidal Wetlands of the Environmental
Conservation Law) is required at this time since the current proposal is beyond
State mandated jurisdiction purSuant to this act. However, any additional work
or modifications to the project may require a permit. It is your responsibility
to notify this Office, in Writing, if such additional work of modifications are
contemplated.
'-..
"
Very truly yours,
~j.
~R..
Daniel J. Larkin
Regional Supervisor of
Regulatory Affairs
.-
~.
"" .",.",.,.._-
.
.
Southold, N.Y. 11971
(516) 765-1938
July 11, ]984
Mr. Lawrence Tuthill
1215 Inlet Lane
Greenport, NY 11944
Re: 382 Wells Road Corp.
site plan at Arshamomaque
(lOOO-56~4-3 & 2)
Dear Mr. Tuthill:
It was the consensus of the Planning Board at the
July 9,1984 meeting to request that you make an
inspection of the above mentioned site, which
is a proposal for a car wash.
The Planning Board requests that following your
site visit, you report to the Board your comments
and/or recommendations.
Enclosed is a copy of the survey for this proposal.
If you have any questions, please don't hesitate to
contact our office. Thank~you for your assistance.
Very truly. yours,
BENNETT ORLOWSKI,JR., CHAIRMAN
SOUTH OLD TOWN PLANNING BOARD
By Diane M. Schultze, Secretary
enc.
.
.
tL. 765-1802 -
TOWN OF SOUTHOLO
OFFICE OF BUILDING INSPECfOR
P.O. BOX 728
TOWN HALL
SOUTHOLD, N.Y. 11971
DATE:
June 18, 1984
TO:
Planning Board Members .~
. d . d" al.~
V1ctor Lessar , Execut1ve A m1n1strat ~
Certification of Site P1an--382 Wells Road Corp.
FROM:
SUBJECT:
Property is located in zone 'B' Light Industrial. The
property was purchased on erroneous advice of the Building
Inspector, so it is now allowable by law.
Off-street parking is to be determined by Planning Board,
100-112 A. Property survey doesn't show any type of drainage,
100-112 E. The property to the north (rear) abutts the railroad
and property zoned 'A' Residential-Agricultural, and requires
screening, 100-134 D 6. The west side may also require screening.
Access to the State Highway will be required per 239K. No
indications of outdoor sign locations (100-134 D 4) and outdoor
lighting locations (100-134 D 3) were indicated. The building
area meets set-back requirements for a business in the 'B' zone.
VL:ec
.
tL. 765-1802
TOWN OF SOUTHOLD
OFFICE OF BUILDING INSPECTOR
P.O. BOX 728
TOWN HALL
SOUfHOLD, N.Y. 11971
DATE:
May 22, 1984
TO:
Planning Board
-(
Lessa~~
FROM:
Executive Administrator Victor
SUBJECT: Certification of 382 Wells Road Corp.
Before certification of this project can be considered, the
applicant would have to do the following: this type of project
is not permitted in a B Zone, therefore a Special Exception
would have to be granted by the Zoning Board of Appeals. This
would have to be applied for after a Disapproval is issued by
the Building Dept. A copy of this memorandum will be sent to
the applicant.
~ 'S \ 2'-/8tl
.
.
T
Southold. N. Y. 11971
(516) 765-1938
April 10, 1984
Mr. Robert Ringold
We 11s Road
Peconic, NY 11958
Re: 382 Wells Road Corp.
Site Plan
Dear Mr. Ringold:
Please let this confirm the action of the Planning Board
at the regular meeting of April 9, 1984.
RESOLVED that the Southold Town Planning Board refer the
site plan "382 Wells Road Corp" for the construction of
a car wash at Southold to the Building Inspector for
certification. The Southold Town Planning Board will
make a field inspection of the proposed site plan.
Please forward three (3) maps and upon receipt of these
will make our referral to the Building Department.
If you have any questions, please contact the office.
Very truly yours,
HENRY E. RAYNOR, JR., CHAIRMAN
SOUTHOLD TOWN PLANNING BOARD
N~ F. q:>Ch,n.'Y'I J C\A..~
By Dian~M. schul~~ seclktary
cc: BUilding Department
J' ~
j ~ 0)-" I()
~\~\
..
.
.
IRVING L. PRIGE, JR.
ATTORNEY AT LAW
828 FRONT STREET
GREENPORT, L. I.. N. Y. 11944
FEB 06 1984
(l'ue) 477-1016
February 3, 1984
Planning Board
Town of Southold
Main Road
Southold, New York 11971
Re: 382 Wells Road Corp.
Gentlemen:
In accordance with your letter of February
1, 1984, I enclose herewith six (6) sketches of the
proposed site plan. Also enclosed please find check
in the amount of $50.00.
If you have any questions, please do not
hesitate to contact me.
Please inform me of the date and time of the
pre-submission conference.
Very truly yours,
~z~~~
ILP:kk
Enclosures
.
.
LD
Southold, N.Y. 11971
HENRY E. RAYNOR, Jr., Ch4i'T1IQ"
JAMES WALL
BENNETT ORLOWSKI, Je.
GEORGE RlTCHlE LATHAM, Jr.
WILUAM F. MULLEN, Jr.
TELEPHONE
765. 1938
February 1, 1984
William H. Price, Jr.
Attorney at Law
828 Front Street
Greenport, NY 11944
Re: 382 Wells Road Corp.
at Arshamomaque
Dear Mr. Price:
Enclosed are the sketches you submitted for the above
mentioned site plan.
Please re-submit these to comply with Section 100-134
and 100-135 under Article 13 of the Southold Town Code.
We will then schedule this for a pre-submission conference
at the next available meeting.
Please note, also, the fee for a site plan has been
increased to $50. as of November, 1983.
If you have any questions, please contact this office.
Very truly yours,
HENRY E.
SOUTHOLD
~~
By DiaU
RAYNOR, JR., CHAIRMAN
TWON PLANNING Bom
E Gi / d i1--0.
M. SC~C tary
enc.
J
.
UM' 2 0 19B-
1#/4am Jf.' gj.'ce. cft..
ATTORNEY AT LAW
828 FRONT STREET
GREENPORT. N.Y. 11944
Phone (516) 477-1016
January 20, 1984
Planning Board
Town of Southold
Main Road
Southold, New York
11971
Re:
382 Wells Road Corp.
Premises at Main Road
Arshamomaque
Gentlemen:
Enclosed herewith please find sketches of
proposed site plan of the subject premises.
Please schedule this for a pre-submission
conference and advise me of the date and time of
same.
If you have any questions, please do not
hesitate to contact me.
Very truly yours,
~-~ ~..' -~
// ... / ~
~/ /. ';'
William H. Price, Jr.
WHP:kk
Enclosures
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LlCtHSEO LAND YnQR5
GlfEENI'ORT HeW YORK
SUFFOLK CO. H TH DEPT.APf'ROVAL
H.S. NO.
STATEMENT OF INTENT
THE WATER SUPl"L Y AND SEWAGE DISPOSAL
SYSTEMS FOR THIS RESIDENCE WILL
CONFORM TO THE STANDARDS OF THE
SUFFOLK CO DEPT. OF HEALTH SER,VICES.
(SI
APPLICANT
SUFFOLK COUNTY DEPT. OF HEALTH
SERV ICE S - FOR APPROVAL OF
CONSTRUCTION ONL Y
DATE:
H. S. REF. NO.:
APPROVED:
SUFFOLK CO. TAX MAP DESIGNATION:
DIST. SECT. BLOCK PCL.
1000 56 4 2~3
OWN€RS ADDItESS:
~eE~T e./NGOhQ.
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It!! IKIS SUIYEY IS A YIOlATION Of
Eno,.,. 720f Of THE HEW YOII STAn
I(IJD_ lAW.
C:OJ!tE$ Of THIS SUlyn MAl I'IOT .....1....
~.E I,AN).SUlYEYOrS INKED SfAL OR
~ SEAt. SHAU NOT II C~lMkIO
lQ JI A YALID TRUE COIY.
GUARANTEES INDICATED HEREON SHALL IUN
ONLY TO THE PERSON fOR WHOM THl SUlVH
IS PREPARED. AND ON HIS 8fHALf TO JHf
nru COMPANY, aOYERI4Mf.NTAL 4GfNCl ~
JaI)1HG lNSTlTUnON LISTED l'iUE()f\I.. "HO
lO JIft ASSIGNEES OF THE lENDING INS",
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SUFFOl.Y (cur-,J r y Dl:pr C:i- '11 A: '4f
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APPROVAL
SUFFOLK CO HEALTH OEPT
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f=~PfQ Of nus SUMV MA9 MOT SU<JiNQ
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