HomeMy WebLinkAboutROSEBUD S-3633O
SUBSURFACE SOIL INVESTIGATION
-~ ....... ~-~--~--= . FOR THE
D & L DEVELOPMENT CORPORATION
ANCHORAGE, ALASKA
October, 1974
...., ': $~6,,z ,~ MAY. 6
R&/W ¢ONSULIANT$, INC.
1975
[ ~ ANCllOllAGE
'. FAIRBANKS.
N CONSULTANTS, INC. JUNEAU
October 17, 1974
R &,.M No. 451068
Mr. Thor Osbo, Architect
1005 Securities Building
Seattle, Washington 98101
Re: Subsurface Soil Investigation - Proposed Restaurant, Off~ce, and
Retail Building, D & L Development Corporation~ Anchorage, Alaska
Dear Mr. Osbo: *' z
We are submitting herewith three copies of our report for subject project.
The work has been performed in accordance'with our October 8, 1974 telephone
conservation with Mr. Fred Walatka~ Consulting Engineer, representing D & L
Development Corporation.
We appreciate receiving the opportunity of performing this study. Should
you have any questions with regard to this.report., please do no~ hesitate
to contact us.
Very truly yours,
R & M CONSULTANTS, INC.
Vice President
xc: Mr, Pred'Walatka
II.
III.'
IV.
V.
VI.
VII.
TABLE OF CONTENTS
1
INTRODUCTION .....................
SUBSURFACE INVESTIGATION ............ 1
2
LABORATORY TESTING PROGRAM ..............
SITE CONDITIONS AND GEOLOGIC SETTING ........ 2
SUBSURFACE SOIL CONDITIONS ' 3
GROUNDWATER CONDITIONS ................ 4
4
CONCLUSIONS AND RECOMMENDATIONS ...........
APPENDIX
A-01
Location Diagrmm ...................
B-01
General Notes '
Explanation of Selected Symbols ............ B-02
of Test Holes B-03
Logs ..... '. · ............
C-O1
Grain Size Curve ....................
CONSULTANTS, INC,
SUBSURFACE SOIL INVESTIGATION
FOR THE
PROPOSED RESTAURANT, OFFICE AND RETAIL'. BUILDING,
D & L DEVELOPMENT CORPORATION
ANCHORAGE, ALASKA
INTRODUCTION
The subsurface investigation for the proposed restaurant, office and
retail building to be constructed on Lots 25 and 26, Block B, Rosebud Sub-
division, Anchorage, Alaska, has been completed. The building site is
bordered on the north by 46th Avenue and on the east by the Old Seward_ .
Highway. The subsurface investigation for the proposes structure was
initiated in response to and in accordance with our October 8, 1974 telephone
conservation with Mr. Fred Walatka, Consulting Engineer, representing D & L
Development Corporation. On site field exploration was begun and comPleted
on October 8, 1974.
Based on preliminary design information furnished' by Mr. Walatka, the
building is understood to be an at-grade two story structure~ utilizing
concrete block construction. Building aerial dimensions are to be approx-
imately 50 feet by 110 feet. The building is-to be need for a restaurant~
retail store, and offices. Foundation loadings are anticipated to be
relatively light.
The purpose of this report is to describe soil conditions as encountered
during drilling operations, to evaluate the information obtained from the
field exploration and laboratory testing programs, and to present recommen-
dations regarding foundation design and construction procedures,
II,
SUBSURFACE INVESTIGATION
A total of three test holes were drilled within the project ar&ao Test
Holes 1 and 2 were located within the proposed building areal Test Hole ~
was located in the proposed parking area of the site. Because of difficulties
in accessability, test hoies were drilled as near as practical to desired
locations and in. accordance with the wishes of. Hr. Holt, owner of Triple A
Rental who currently occupies the project site. Test Holes I and 3
extended to a total boring'd~pth of 20 feet'below existing ground
surface. Test Hole 2 extended to a 31o5. f0ot of depth. The results
III.
IVo
obtained from these borings along with a location diagram are included with
this report. Test Hole locations and vertical control were referenced as
noted on the Location Diagram, Drawing A-O1.
The soil borings and sampling operations were performed utilizing a
truck-mounted CME-55 rotary-type hydraulic drilling unit. The boreholes
were advanced using continuous flight 8-inch diameter hollow-stem augers;
representative samples were obtained by mea~s =~ split-spoon sampling ~
procedures conducted'in accordance with ASTMSpecification D-1586-64T. In
this procedure, a split-barrel sampler (1.4" i~D.) is driven into undisturbed
natural soil with a 140 pound drop-hnmmer having a 30-inch free fall. The
penetration resistance (as measured by the blow Count~ "N") for this s~mpler I
gives an indication of the relative density o~ the inplaee natural'sotlo
After visual classification in the field~ soil s~les were returned .to the
laboratory for further examination and testing.
LABORATORY TESTING PROGRAM "
The laboratory testing program was limited to the evaluation of general
soil index properties. Laboratory determination of water content on recovered
representative samples were performed according to ASTM Specification D-2216-66o
Atterberg Limit values were determined according to ASTM Specification D-423-66
and D-424-59 for the liquid limit and plasticity index, respectively. In-situ
consistency (density) values for' the non-cohesive material were estimated
from the blow count and the soils gradation at the particular sample locations.
For cohesive materials, consistency was determined from recovered smmpleS
where it was estimated from pocket penatrometer data or the blow count and ~
Atterburg Limit values for the particular sample°
' Results of sample moisture.content for the three test holes are presented
on the respective boring lo~s~
SITE CONDITIONS AND GEOLOGICAL SETTING
The proposed building site is located within the southcentral portion
of the Greater Anchorage area° The project site lies in a,.region of relativ~.ly
flat relief. All natural vegetation has been stripped from the proposed
project locatidnl although~ it is believed to have originally consisted of
stunted black spruce' in a swamp environment. Surface soil origina}~y con-
sisted of,varying ~hicknes~'of peat. Presently~ the building site is being
utilized as an equipment storage area. Previous development has included
the placemant of a soil fill section to provide a working surface; the fill
appears to have been placed directly above the original surficial peat.
The project site is iodated on the Anchorage Lowland, a broad, un-
dulating glacial plain. In the project vicinity surficial soils are glacial
out-wash deposits of pre-Wisconsin Age consisting of interbedded, well sorted
soils generally having much fine grained material. These deposits were ov~r-
lain by varying thicknesses of s~amp deposits of recent origin. The well-
known, pre-Wisconsin ARe Bootlegger Cove clay formation generally underlies,
at relatively shallow depth, the surficial, glacial out-wash deposits i~ ....
this area. Below the Bootlegger Cove clay unconsolidated glacial tills,
interbedded sands, silts and clays~ deposited during the Knik subglacia~
advance, extend to great depths to tertiary-age sedimentary rock which in
turn overlie precretaceous crystalline "basement" rock~ the basement rocks
are thought to be very similar in composition to the rock types exposed in
the Chugach Mountains. The entire Anchorage area~ including the project
site, is located in a region susceptible to very strong seismic shaking,
as evidenced by the Great Alaska Earthquak~ of 1964.
SUBSURFACE SOIL CONDITION
The subsurface investigation, comprised of the three test holes, shows
the site to be overlain by 3 fee~ to 5 1/2 feet of soil fill. The fill
consists of several soil types including sands with various percentages
of both silt and gravel and, at the location of Test Hole 3,' clean gravel;
Test Hole 1 showed the fill included a near surface~ 1/2 foot layer of psat.
Underlying the fill ail test holes disclosed the existance of very com-
pressible, dark brown peat and dark brown organic".silt.
Immediately below the peat and organic sil~,.gray clayey silt was
encluntered in Test Holes 1 and 2; and gray silty sand with some clay was
encountered in Test Hole 3o Expec~ for a 4 foot stratum of silty sand
containing some clay in Test Hole 2~ at the respective test hdles these
materials continued to total boring depth. The gray clayey silts were
found to be ~f highly variable strength. However, as discussed in Section
VII the clayes Silts can be ~tilized ms an adequate natural soil bearing
surface.
VI.
GROUNDWATER
Groundwater conditions were observed in each test hole both during
and ~mmediately after drilling operations. Test Holes 2 and 3 indicated
a groundwater table at approximately 12 feet below existing ground surface.
Although Test Hole 1 did not show a water table, one probably exists near
the same level indicated by the latter two test holes. However, perched
groundwater,,overlying the true groundwater table, probably exists iu the ~
peat. Fluctuation in the water table level ca~'be'expected to occur i~
the project site; this is due primarily to variations in surface water
infiltration resulting from rainfall and spring b~eak-up meltwater.
Relatively minor construction difficulties could develop during
excavation operations for the building-the resul~ of the perched ground-
water occurring in the organic soils at the site." This is discussed in
4
Section VII.
VII.
CONCLUSIONS AND RECOMMENDATIONS
A spread footing foundation for support of the proposed structure is
considered adequate at this site provided the design precautions specified
in the following paragraphs are observed.
An over-excavation and backfill procedure is recommended for both a
spread footing foundation system and for interior slab(s)-on-grade; For
both footings and interior slab(s)-on-grade over-excavation should reach a
minimum of ~6:.. inches below the top of the gray clayey silt or silty sand·
strata occurrimg between roughly 8 and 10 feet below existing ground surface
in the proposed building area. We a~e recommending that over-excavation
be utilized under interior slab(s)-on-grade because of-both the variable
thickness and depth to the peat and the highly g0mpressible nature of the
peat stratum-both of which combined could lead to'excessive differential
settlement in the flooc slab(s)o Backfill~ compacted as specified below~
can be placed on the undisturbed gray clayey silt or silty sand°
The thickness of cgmpac~ed backfill extending above the undisturbed
natural soil, bearing surface (the gray clayey silt or gray silty sand) and
below the footings should be a minimum of 1,5 times the width of the footings
(B); t.eo~ compacted backfil~ of minimum thickness 1~5 B Should extend-below
all foundation footings of width B. This is necessary to safely preclude
the possibility of local shear failure in the underlying clayey silt. To
provide frost protection all exterior footings should extend at least
3 1/2 feet below finished grade; interior footings can be placed as near as
practical to finished grade. Under the forgoing recommendations, an allow-
able bearing pressure of 3,000 psf total load can be utilized for the footings.
Proper construction control should be exercised to ensure that the
clayey silt ~or silty, sand natural soil bearing surface is not disturbed
during construction, tn particular, we recommend that the undisturbed
clayey silt or silty sand be covered as soon as practical after exposure
during excavation by a granular backfill filter blanket a minimum of 1 1/2
feet thick. This will help prevent subsequent.disturbance to the clayey
silt or sandy silt from either perched groundwater inflow or constructiou
activities. If, however, the natural soil bearing surface is disturbed,
the soil in the zone of disturbance should be excavated and backfilledo
The final compacted fill bearing surface should be carefully inspected
prior to placing reinforcing steel and pouring concrete to verify that all
loose or disturbed soil, or debris, has been removed from the bearing
surface.
Ail fill placed below footings and interior slabs should be non-frost
susceptible granular material free of organic matter and debris and placed
in lifts not exceeding 9 inches in loose thickness° However, the filter
blanket recommended above can be placed in one lifto Fill placed below
footings and concrete bearing walls should be compacted to a minimum of
95 percent maximum density~ fill placed below interior slab(s)-on-grade
should be compacted to a minimum of 92 percent maximum density. Maximum
density should be determined in accordance with'ASTM Specification D-1557-67T.'"
For the foundation design, it is recommended that poured concrete
continuous type.footings, having a grade-beam typ~ foundation wall design
where feasible~ be'utilized to provide a more rigid foundation° Where
isolated footings are required care should be taken to minimize the effect
of any potential differential movements'°
Construction problems or difficulties at the site due togroundwater
should be relatively minor so long as over-excavation does not extend
beyond roughly 12 feet below existing ground surface. Excavations of
lesser depths including what will be necessary to remove all organic soil
underlying the building area should only require dewatering of the perched
groundwater which enters the excavation both during excavation of the
organic soil and from surrounding organic soil before backfilling begins.
Removal of the perched groundwater can be accomplished by usual sump pit
and pumping procedures. Utilizing an at-grade structure, we anticipate
no post-construction problems or'difficulties due to groundwater conditions
at the site so long as'final site grading is accomplished in a manner which
will divert surface water drainage away from any sturctures. -
If site grading and foundation excavation operations are to begin this
fall, we emphasize that p~ovisions should be made to prevent frost penetra-
tion into natural soil below foundation footings or any.slabs-on-grade;
'this is necessary to preclude the possibility of any frost heave or
subsequent thaw setbl~ment in. the foundation or slab systems. Frost penetra-
trion below footings and slabs, poured on non-frozen soil, can be 'avoided
during a winter construction hiatus by properly insulating the building
area with, for example, straw and an overlay of plastic sheeting.. The
'effectiveness of the insulation should be monitored by periodically
verifying that frost has.not penetrated to soil existing below foundation
systems.
With respect to pavements and exterior slabs which are to support
traffic loads, if little or no changes in existing grade 'are required, the
underlying peat need not be excavated so long as a-lim/ted amount of annual
£~os~ h~v~ ~'~o!l~r~bl~o However, ~h~ ~ea~ s~rface peat layer encountered
in Test Hole 1 suggests that~ in addition to proof rolling as recoh~ended
below, it may be beneficial to spqt check the n~ural soil subgrade below
pavements and exterior slabs to verify that no peat exists Unusually'near
the natural sol! surface'° These spot checks can consis~ of shallow test
pits dug at appropriate locations on the subgrade~ test pits should extend
a minimum of 18 inches below existing grbund surface° Any organic soil
found should be excavated to a minimum depth of 3 feet below final sub-
grade and properly backfilled as specified above°
If the underlying peat-is not removed~ increasing the existing grade
outside the building lot more·~than roughly 1. foot by placing fill could
lead to set~lements~ due to compression of the pea~in excess of 2 inches°
The magnitude of settlement, including differential settlement, would increase
as the height of added fill increased. In the case of adding significant
amounts of fill, it is suggested that placement of any pavement or slabs
be delayed until at least a major portion of the.. settlement had time to . .
occur-probably a period of two or three years'~
In all cases, the natural soil subgrade f?r pavements and exterior slabs
which are to support traffic loads should be pr'pof rolled prior to the
placement of any new fill; sections of evlden~i.loose or soft soil should be
either properly compacted or excavated and backfilled in the manner specified
above. Also, any debris encountered should be removed from subgrade locations.
Ail new fill including base material for pavements and walkways should con-
sist of material meeting Alaska State Highway ~epartment Specification Di~
placed in lifts not exceeding 9 inches in loose thickness, and compacted
to a minimum of 95 percent maximum density determined in accordance with
ASTM Specification D-1557-67T. Base courses for pavements and exterior
slabs should be a minimum of 4 inches thick. To avoid major crack develop-
ment as a result of stress concentrations at structural connections~ all
exterior slabs should be separated from any building structures by weather.-..'.
sealed, joints.
Because soil characteristics may vary throughout a given site and
change sharply within certain limited distances, it is reco,..~ended that
a qualified soil engineer or engineering geologist inspect the foundation
excavations and backfill procedures, during construction; this will permit
verification that conditions are as anticipated in the design~
We appreciate being g~wn thi~ opportunity to perform th~s subsurface
investigation. If you wish~ we would welcome the opportunity to review
plans and' 'specifications after they are prepared .so that we'might have
the occasion, to-comment on the effect of the sit~',sOt~', conditions upon
the design and specification, ~Jk"~'~o~'°o~ ~J~% ~ ~ '
Charles Lo Vita
Soil Engineer
ChV/JWR:rr
TM. 3
Engineering I~ Geological Consulfanfs Inc.
ANCHORAGE FAIRBANKS ALASKA ' -,UN,AU
~ [DWN BY W.T.J.
DATE 10- {5-74, ISC~AL-~ ITM 40'
LOCATION DIAGRAM
DI~L DEVELOPMENT CORR
ANCHORAGE, ALASKA
lc. Ko .Y c.v. . I..o~..o..,ooo ]~
SOILS
CLASSIFICATION, CONSISTENCY AND SYMBOLS
CLASSIFICATION: Identification and classification of the soil is accomplished in
accordance with the Unified Soil Classification System. Normally, the grain size
distribution determines classification of the soil. The soil is defined according to
major and minor constituents with the minor elements serving as modifiers of the
major elements. For cohesive soils, the clay becomes the principal noun with the
other major soil constituents used as modifier; i.e. silty clay, when the clay partlales
are such that the clay dominates soil properties. Minoz soil constituents may be
added to the classification breakdown in accordance with the particle size proportion
listed below; i.e. sandy silt w/some gravel, trace clay.
no call - 0 - 3% trace - 3 - 12% some - 13 - 30%
SOIL CONSISTENCY - CRITERIA: Soil consistency as, defined below and determined
by normal field and laboratory methods applies only to non-frozen material. For'
these materials, the influence of such factors as soil structure, i.e. fissure
systems, shrinkage cracks, slickensides, etc., must be taken into consideration
in making any correlation with the consistency values listed below. In permafrost
zones, the consistency and strength of frozen soils may vary significantly and
unexplainably with ice content, thermal regime and soil type.
Cohesionless Cohesive
N*'(blows/ft) Relative Density
Loose 0 - 10 0 to 40%
Medium Dense I0 - 30 40 to 70%
Dense 30 - 60 70 to 90%
Very Dense - 60 90 to 100%
*Standard Penetration "N": Blows per foot of
a 140-pound hammer falling 30 inches on a
2-inch OD split-spoon except where noted.
T- (tsf)
Very Soft
Soft
Stiff
Firm
Very Firm
Hard
0 - 0.25
0.25 - 0.5
0.5 -1.0
1.0 - 2.0
2.0.-4.0
-4.0
DRILLING SYMBOLS
W0: Wash Out WD:
WL: Water Level BCR:
WCI: Wet Cave In ACR:
DCI: Dry Cave In AB:
WS: While Sampling TD:
Before Casing Removal
A£ter Casing Removal
After Boring
Total Depth
Note: Water levels indicated on the boring logs are the levels measured in the
boring at the times indicated.' In pervious un'frozen soils~ the indicated elevations
are considered to represent actual ground water conditions. In impervious and
frozen soils, accurate determinations of ground water elevations cannot be obtained
within a limited period of Observation and other evidence on ground water elevations
and ~onditions are .required.
M
CONSULTANTS'.; INC.'
GENERAL NOTES
DATE: 3' I - 72 SCALE N/A OWN eY LDS CHKD aY GLB
St
Ss
SI
Sh
Sx
Sz
Sp
Hs
HI
NOTE~
STANDARD SYMBOLS
ORGANIC MATERIAL [~ COBBLES 8~ BOULDERS ~
CLAY ' ~ CONGLOMERATE ~
SILT ~ SANDSTONE ~
SAND ~"~ MUDSTONE [~
IGNEOUS ROCK
METAMORPHIC ROCK
ICE~ MASSIVE
ICE -SILT
ORGANIC SILT
SANDY SILT
SILT GRADING TO
SANDY SILT
SANDY GRAVELs
SCATTERED COBBLES
(ROCK FRAGMENTS)
INTERL/~YEREO SAND
B SANDY GRAVEL
SILTY CLAY w/TR. SAND
SAMPLER TYPE SYMBOLS
. 2.5" SPLIT
2.5" SPLIT
2.0" SPLIT
1.4" SPLIT
2.5" SPLIT
1.4" SPLIT
1.4" SPLIT SPOON WITH 47-;~ HAMMER Ts
1.4" SPLIT SPOON WITH 140# HAMMER Tm
SPOON WITH 140# HAMMER Pb
SPOON WITH 540# HAMMER Cs
SPOON WITH 140# HAMMER Cd
SPOON WITH :~40~ HAMMER Bs
SPOON, PUSHED AD
SPOON DRIVEN WITH AIR HAMMER G.
2.5" SPLIT SPOON DRIVEN WITH AIR HAMMER
SAMPLER TYPES ARE EITHER NOTED ABOVE THE' BORING LOG OR
SAMPLE DEPTH.
SHELBY TUBE
MODIFIED SHELBY TUBE
PITCHER BARREL
.CORE BARREL WITH SINGLE TUBE
CORE BARREL WITH DOUBLE TUBE
BULK SAMPLE
AUGER SAMPLE
GRAB SAMPLE
ADJACENT TO IT AT THE RESPECTIVE
FROZEN
SANDY GRAVEL
Cd 95 SCHIST .~--'GENERALIZ£D $O/L OR ROCK DESCRIPTION
£OCATION ' 50' ~ DRILL DEPTH
~ FtO.-WHILE DRI&UNG~ A.B-APTER BORING
Engineering ~ eeologicol Consullenfs inc.
AN~HO" AGE FAIRBANKS · ALASKA
.
TYPICAL BORING LOG
BORING NUMBER~.,,~T. H. 3~0-15 Elev. 274.6 **--ELEVATION IN
Dare DRILLED--~,.iO_21. 70 . All Samples Ss~''SAMPLER TYPE
0
ORGANIC MATERIAL I'
Consid. Visible Ice O'-T ICE+ML
ICE, SILT '
SAMPLER rYPE%ss Estimatego, 56.~%65 Yo Visible IC~srRArA' ~HANGE
~ SANDY SILT
~APPROXIMAT~ STRAT~ CHANG~ ,"
GRADATIONA~ ~,,
Liffle toNoVisible Ice 15L50
~ 72 5Z1% 859pcf ~e~-GP , (CORPS OFKNG/N~BS METN~)
Ss ~ ~ '~ ' ' ~ ' ~ ~U~FIED O~ FA~ CL~SS/F/c~r/ON
~ ~ ~ ~ TEMP~AruR~
. k--8~o~s/roor
' 'EAMPLE NUMBER
OATS 2-16-72 [eCALE: NONE lawn ay 'LOS [CHKD BY
EXPLANATION OF SELECTED SYMBOLS
GLB IPeou. NO. GENERAL Iowa NO. B-02
T.H.- I
10-8-74
~ Brn GRAVE L ,.,~
OR GA N I C---"~'~L (PEAT)
Bm. .- I'
GRAVELLY SAND W/TRACE
~. __ SILT
3/6,20%
SAND W/TRACE SILT~Gray
Loose 5.
9,143%
SOIL (PEAT)
Drk. Brn.~ Compressible T.O~
)RGANIC SILT .8.57'
20, 20°/o,CL'ML . .
CLAYEY SILT W/TRACE TO/
SOME FINE SAND
Gray,Stiff fo Very Firn~
Q 12,20%
Q33,Z9%
, · '20.0
NO WATER TABLE T.D.
.I
11,5 W,D,
?
T.H.~
~0-8'74 .- 0.0'
CLEAN GRAVEL
Grey; Fill Material
O ORGANICSOIL(PEAT}~ ' ~.0'
4WOOD FRAGMENTS
Drk, Bm.; Compressible
· , 6.5'
SILTY SAND W/SOME
CLAY a GRAVEL
Gray; Msdium Dense'
?o Dense
Q 29~9.2°/o
GRADING W/dOARSE ,
GRAVEL a CO?BLES['"~ t8
T.H. ~'
10-8-7'4.
SILTY SAND W/SOME GRAVEL
GRAVELI'Y' S-~'~'D W---7'~"~AC.E SILT
SAND W/TRACE GRAVEL
ORGANIC SOIL(P~'AT)
Drk. Brn.;Compreesibls
13, 15 °/o,CLo M L
CLAYEY SILT W/SOME SAND
TRACE FINE GRAVEL
' Gray;Firm toVe. ry Firm
28~J2°/o
GRADING MORE SANDYt'~ I§~
, --2.5~
'
~10.0'
Q24,.27%
GRADING LESS SANDY
SILTY SAND W/SOME G~VEL
8~ SOME CLAY
Gray;Dense
CLAYEY SILT'W)TRACE BAND--
Gray;Firm to Very FIrn~
Q 18,15°/o, CL- ML
27°
LOG OF TEST HOLES
D E~ L DEVELOPMENT CORP.
ANCHORAGE, AI~ASKA
Encjineering ~ GeoIogicol-Consultonfs Inc.
~NC.O.^~ .Am.~.~S ALASKA
L;-U.L
DEP~RTMENT OF ENVIRONMENTAL
QU~L~? TY
PLATTING OR PLANNING & ZOHING CASE REVIEW
CASE NO. J- ~f//
TITLE: ~2~~
Date Case Received
By
Suspense Date Comments to Planning Department
For' Planning & Zoning Commission Meeting Date
Environmental Engineering
Air Pollution
Noise
ROUTING
Environmental Sanitation
COMMENTS:
O'
GREATER ANCIiORAGE AREA BOROUGH
3500 Tudor Road
Anchorage, Alaska 99507
S- 2707
PLAT STATUS: Final
BOROUGH:
Platting Engineer
Public Works Department
~ar~~C~ccf~,~~e~tal Quality
'Fire Department
Street Names
Tax Appraisers
School District
DATE: May 2, 1972
OF ANCHORAGE:
Fire Marshal
Municipal Light & Power Department
Property Management Off±cer
Public Works Department
Telephone Utility
Traffic E~ine.er
Water Utility
OTHER:
Alaska Department of Highways
Alaska Railroad
Anchorage Natural Gas Corp.
Central Alaska Utilities
.Chugach Electric Association
GAB.Telecommunications, Inc.
Matanuska Electric Association
Matanuska Telephone Association
Assistant Superintendent of Mails
Alaska Department of Fish & Game
DESCRIPTION OF PROPERTY:
OWNER: Kensun Corporation
Vac: 10' utility easement south side of Lots 2 thru 6,
Blk. 1, Rosebud Subdivision and north side of Bi. 10,
Heather Meadows.Subdivision.
Gent I~men:
A petition has been received by the Greater Anchorage Area Borough Planning
Department for the proposed Vacation of subject property for the
May_31, ~97~ Planning Commission Meeting.
At~ached is a copy of the proposed plat. Will you~please submit your comments
in writing', specifying any easements or other requirements that your department
er agency may~need.
'I~f we do not hear.from you by _M~y 18,
do not wish to submit any comments.
, we will assume that you
If you have no further use for the attached print, please return it with your
comments.
'P~anning Department
[{ nc lo sure
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..MAY 3 ! 1972