c^ ^//^ IOWA GEOLOGICAL SURVEY ^ ^ ^J/f , /t^y,^^^- Iowa City, Iowa r̂ V&V/1^J?U*^ ^Well Log Record

/- / I -Owner of well / VU *J /7_jy iaj 0p

Tenant ' ILocation sec. T.

_C ounty_

.Town f'lM M-tfJi/

S. . R.E.

.W._ JTwp.

Curt) elevationPresent

_ft. depth

aboveStatic level: (Depth to water vJJJ-J curb)

Contractor _, Date drilled

final

ft. depth - : ft.Pumping

ft. level •_..;, ft. at •:. - g.m.

Description* FEET

—

Description* FEET

Thick From To Thick From To

H 4t

.,.:_ .. ... ;.,'.' (

'

/

.._ 1

^Abbreviate descriptions:'use one line.for each formation.

Remarks on water zones and casings

, •;•-.

Temperature; Air °F.,Water,

'Record obtained from

r

°F. at_A.M.

P.M..

Recorded by_

.19-^

LOGAN OLINGER

OWA FARMS

Dr. Allen C. Tester,Iowa City, Iowa.

Dear M* . Tester •

INSURANCEOF ALL KINDS

Maxwell, Iowa

April 20th 1936.

PAUL OLINGER

^d*^ ^w^Th£/o2

Z~.X~f>(im, F

me and note thatYour letter of mouiry of the 13th reached

you had made Inquiry before.

Your former letter I did not receive, which I presumeis due to the fact that our mail trains have a habit of jerkingthe. mail sacks under the wheels and destroying the contents and'you letter was doubtless among those destroyed.

In answering your inoujries, the ground elevation atthis noint is 880 feet.

Cur city well was drilled, to a depth of 382 feet andin drilling we struck a rook formation at 134 feet, which thelog of the well showed to he of sandstone and lime stoneformation, with perhaps a small strata of shale, producingwater started at about 150 feet coming from crevices in thestone and increased along with the depth. At I beleive adepth of 250 feet the drill went through a small strata ofwhat the driller logged as soan stone, peihaps was 2 or 3 feetthiak. To a depth of' 200 to 225 feet the formation wast hePennsylvian, below that depth we encountered the :•. 1 ssi ssinianand well was finished in this formation.

Our well shows a considerable amount of Flonriftes, butwhether this comes from the botton of the Pennsylvian or thetop of the ITi ssi ssipian formation we pre unable to tell. However,it is my opinion that we penetrated the I'ississipian formation

only 8 few feet or enough to tap the strata conlaining theflour ides.

the well is as follows^ 8 inch casingrock formation 134 feet deep. Inside thewith 6-5/8 to a depth of I beleive 300all in good shape so far as we are ablebeen for the soar) s1 one formation, no

casing would have been necessary as rosv formation extendedfrom 13 4 feet to depth of the well.

I will appreciate any further suggestions you mightwish to make, or any information you can give us regardingthe flouride condition of this well p^ to how ,it might becont r ol led . Your g truly

"OAAj

r lis casing inwas driven into the8 the well is casedfeet. The casing isto tell. Had it not

•yor .

\ \ AirXrVe//, q±ry C* 77^^^^

Cart £/'&/. = e<?o'

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Proa/t/c/oa fcrmat/o*) : A/jss/ss'//>/>/or,Basement rock. : Pt/„, #.•/• /3#' * <S/. 7</6 'See report ort p//nera/ onotysis &7hbc,4 cc?'.

Former si/f^ty : from <^//^\///j/i? m /ad&a. Creek s/o//ay. f^/Zai/JUm here ^0-/00' /-h'/cJk. )

7~wo st/iaZ/ow wells go. «gy?<s/ /oo' e/eef>. Vo/is/ne XX:' reports a sari7s-7r7e/v*~y saon/y

of ye>od rtarer. /e/al or yoroc/c/Qt/on f^rcs ;

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rt><? tfens-g/,. Base of K^/ysar-j^ ia Ahase/i - gedrect <:<>/, t/>at /S't /» present n/g//,

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and sta/tc /<sva/ *//], /tamera as :,i,-m yv&//s 2ao -#e>o' deep i- /h £..-

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/-

IOWA GEOLOGICAL SURVEY•In Cooperation with IT. S« Geological Survey

Location:

T.own: M^ujdi

RECORD OF WELL

(HE)(SI) :County $fory

aeo. T \ ,".N.,R. W.j^ _, Twp.

Well name and nun

Owner -••• '•• Address

Address"enant

Contractor / hnts-h-tn, jj ,

Drillers

Drilling dates

Well data:

Elevations: Drilling curb

Determined by-

Topographic position.

Address

feet/ Land surface

Total depth: Reported . j V 2, feet, Measured^

Drilling method

w-3te?f

feet

feet

Hole and casing data 11 t/'c <>~f I O'1 Ttb^ •f^ <*- "/o // 0 '

ID!of^ s^€

' : ;: . • • - iJff<-tj •'

aDOve

Original depth to water__ _J^# below

Original elevation of water level ft+j Source of data

Date

Sources of water: Principal ; Others

I

w

i

Production data:

Static depth to water-Pumping level .

Specific capacity..

Pump dataj.. Type pump.Cylinder or bowls:. Dia«

Power

Date.

Measuring pointr—at _<Li. g.p.rru

g.p.ra. per ft. drawdown; Temperature-

.Column Dia»

Length

Airline

_ Length.Suction pipe

Estimated rate of production:.

Use of water: ;

.g.p.m. for

Date samples

Sampled by

Total solids

Insoluble' matter

Alkalinity (Meo)

Alkalinity (Phn)pH

Fe203+ l&igOj!.+AI2O3Alkali as sodium

Calcium

Magnesium

Iron (unfiltered)

Manganese ..

Nitrate

Fluoride

Chloride

Sulfate

Bicarbonate

Hardness (ppm)Hardness (gpg)

Remarks

Laboratory data:

Sample range J / Pa

Spls. prepared by •-/ ,.- ^..

Driller's log and cond.

Insoluble residues: Prepared by

Microscopic study

Gen. log

WATER ANALYSES (in parts per'million)

Sample storage location-

.Kb. spls. jX~ 0—Washed ranee.

_No. dupls. & cond*.

1 by :

hrs. a day

Studied by. Strip log

strip log

Correl. by_

\Q?M NO. 79 -In ttcck anj for tale by Mirf-Weit Trie. Co., "Uiss W - 3^9"**'*

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k&L £22.TO. /2.2_'

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MMWEii Csro^y)ory e>^ /hakiasclcl

COMMENCED

bee. 3,/9¥Cp

THOgPC OlfcLL £» •

COMPLETED

CASING RECORD UUft." »f 'O" f *°««. +l\ -/le |

-e f 0/r S-fla"plPC, G^VO^-facT-

T^y -2.3. , HVy w.L-li-Tf)t:REMARKS

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T<t_c. . BA*r. /V.Mtc . soy. (6.i9n.<ustt, •«*>•' roy. ?*ifl

T'l-L.C^. OALC.ti. SoV *"/>»/* P«Ispy *vwn\ pgisf

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S/r»£l DlKV/y IO»?/i<i.i fscl "?*«M.cS£|fWp cu<iw/,fw( -C^tf. VMM <-"io. ""-Ticc, c«. c*'c, soy, *"/* « is.ic.*$l

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Lab. No. 84103

County __or.y __.

Town . Maxwell

IOWA GEOLOGICAL SURVEY

Water Analysis Reporti

Date Sampled ..J[___ ** 1934

_.__.., Sampled by .___._Mark ,

__.:. Location ____ ______

.. .. ._ .. Sec. T. N., R._;_._W,

Owner ^CJ_t_„of.__:well_ Well Mo. • T.D. 582 ft.

Type of Well Drilled ; Curb Elevation ft.

Producing Formation

Remarks on Condition of Weii or Formations

Constituents.

Total Solids

Dissolved Solids

Insoluble Matter

Alkalinity (MeO)Alkalinity (phn)

Parts PerMillion

... 1059£p_.

»• ?_5 __

... 8,0

. _308_0_

,.._ _. 12,,0__

Nitrogen as Ammonia(NR4) ....._ -__..._Nitrogen as Nitrite(NOg). 0.35Nitrogen as Nitrate(N03>.. 0.12Alkalies as Sodium (Na) .. _364.0.Calcium (Ca) ............. 16.7

Remarks on Composition

Constituents

Magnesium (Mg)Iron(Fe)(unfiltered).Iron(Fe)(filtered) ..Manganese (Ma)

Aluminum (Al)Fluorine (F) .Chlorine (Cl)Sulphate (SO4)Bicarbonate (HCO3) ..Phosphate (PO4) ."....Borate (B05)Calculated Hardness .

• • • • •

• • • • •

PartsTPerMillion

—J7..9-...

_9*?

-_Q,0.

„.4„3

_.__5_5.

„J-4,0_

500.4

346.5

0 03

75.0

Analysis by State Yfeter Analysis, Dr. J. J. Hinman, Director, Iowacity, Iowa.

Sent to:

Bates

.,i.t<&:Y .:

+*•'••''

m\*''

tfc<*

2340 SIXTH AVENUE

DES MOINES, IOWA

Hi-Drilled for 01 tV Of MaXWell _

fF*// is /oca/<?</ miles N-E-S-W and miles N-E-S-W from.

in the % Va Section— Township

Maxwell, Iowa

Range-

Drilling started 12/3/^k J9- Completed 12/?*/^ JTP-

JF«// iVo. Kind of Well gravel PfrPfc DtpM 12JL

&0 ftrtfe Aearf 151-

Si** Ao/tf started* / Si V

F/fiis* ID G. P. M,

Wflter was first encountered at—

Remarks-

Approx. AmU

Drawdown-

Temp*.

RECORD OF PERMANENT PIPE TEMPORARY PIPE

SIZEPIPE

AMOUNTOF PIPE

DEPTH TOBOTTOM OF PIPE

DEPTH TOTOP OF PIPE

MAKE OF PIPESIZEPIPE

AMOUNT

10M 1124"1 110' £% above &v WTlfl 13 3/8

5 3/ L6 9* 112' 103 attach sd to screen

6" p sreen 10f 122' 112

Driller-

Driller-

Driller-

AMOUNT IN FEET

2122610

162912

From Surface to-

From

From

KIND OF SOIL OR FORMATION (BE SPECIFIC)

Black dirt

Yellow sandBlue sandy claySand A gravelBlufc sandy claySandBlue claySand & gravel

feet to .

. feet to

-feet-

-fee:

-feet

TOTAL DEPTH FEET

2

nko5065#1

110122