I* 1

IOWA GEOLOGICAL SURVEY
In Cooperation with U# S. Geological Survey
W-c
i
RECORD OF WELL
1
Location-
(
_•
Town:
N E)
'
(__S__W); County
K.,R..:,, W.
A70++-
t i
i
i
9. "
.A>L'Seo# j-^T.
•
•,. ., • ,'
-
Twp,
+ —1
I
I
1
Well name and number
•^
-
__
Address
Owner
Tenant
Address
Contractor
Address
Drillers
Drilling dates
Well data:
Elevations:
Drilling curb
//&p, 7
feet; Land surface
p
,
//##.?
feet
.5 7^3 7^/ C tJ
...
Determined by
~ -
Topographic position
Total depth:
Reported
77pL7'
feet, Measured
feet
Drilling method
Holo and casing data
. '
(Give amount, size, kind* and depth of all casing; type and
"position of seals and packers; cementing; how finished—perforated pipe, screen,
gravel pack, open hole, etc.)
Original depth to water
above
ft- below
Original elevation of water level
Sources of water:
Principal
Date
ft#; Source of data
; Others
Production data:
Date
Static depth to water
/:•: .':•
Measuring point
_______^____ ^
Pumping level
Specific capacity
-'"'•' i
g.p.m.
g.p.ra. per ft. drawdown; Temperature^
Pump data; Type pump
Cylinder or bov;ls: Dia.
Column Dia.
Length
Pover
°F,
Length
Suction pipe
^_^^_____ Airline
Estimated rate of production:
,g.p.m. for
hrs. a daj
Use of v/ater
WATER ANALYSES (in parts per million)
/// - /.
Date sampled
Sampled by
Total solids
Insoluble matter
Alkalinity (l.ieo)
Alkalinity
(Phn)
PH
~ ~
Fe203+ P/ln203+Al203
/,.:
Alkali as sodium
'••",
Calcium
;
Magnesium
___.
Iron (unfiltered)
.£'
Manganese
Nitrate
_
/ •>
Fluoride
Chloride
,
Sulfate
Bicarbonate
Ha'rdness (ppm)
Hardness (gpg)
Remarks
j
_^_„_____
Laboratory data:
Sample storage location_
Sample range
Spls. prepared by
'
No. spls.
Washed range
i
No. dupls. & cond,
by
Driller's log and cond.
Insoluble residues:
Microscopic study
Gen. log
Prepared by
^
Studied by
strip log &<*^. "3 <? /<?5~0
Correl. by
Strip log
^amJ&
March 1, 1948
Mr. £. L. Patera
625 Royal Union Building
Des Moines 9, Iowa
Dear Mr. Patera:
Re:
General geology and ground-water conditions in
the vicinity of Hampton. Iowa.
In response to your request of February 23, we have prepared the following
discussion of the general ground-water conditions at Hampton from data in the
open files of the Geological Survey.
The City of Hampton is located in the central part of Franklin County in
sections 27, 28, 29, 32, 33 and 34, T. 92 H., R. 20 W. The population of the
city was A,006 in 1940. The upland surface in the main part of town is about
1,145 feet above sea level.
Since 1900, most of the city's supply has been secured from deep wells.
Well No. 1 was completed in 1900 in the Jordan sandstone at a reported depth
of 1,709 feet.
In 1920, the non-pumping level was about 50 feet below land
surface. The veil was pumped at the rate of about 160 gallons per minute.
The main supply was reported to have been encountered at a depth of 1,100 feet,
about 65 feet above the top of the St. Peter sandstone. The curb elevation
of the well is about 1,100 feet above sea level.
Veil Mo. 2 was completed in 1926 at a depth of 1,700 feet. The curb
elevation is about level with well No. 1. The principal supply was reported
to have been encountered in the Jordan sandstone. At that time, the nonpumping level was reported to be 153 feet below the surface. At a pumping
rate of 1,000 gallons per minute, the drawdown was 23 feet. In March 1947,
the non-pumping level was 142 feet below the pump base. At a pumping rate
of between 475 and 490 gallons per minute, the drawdown was about 30 feet.
Thus, while the well is still capable of being pumped at a large rate, the
specific capacity has fallen off considerably. This may be due to sand having
filled in the lover part of the hole and retarding the movement of water into
and up the well bore. The non-pumping water level may be affectod by other
aquifers open to the well which have a higher head than that of the Jordan
sandstone.
In the vicinity of Hampton, the drift is thin. In the shallow stream
valleys, there are numerous rock outcrops. The following tabulation of the
anticipated geologic section at Hampton to the St. Lawrence formation is
based on a starting elevation of 1,145 feet, the elevation of the upland
slope.
Mr. E. L. Patera
-2-
Formation and Description
March 1, 1948
Thickness
From
To
50
0
50
-45
50
95
30
95
125
60
125
185
40
50
185
60
225
275
225
275
335
formations (limestone and dolomite) 300
335
635
635
695
695
Pleistocene system (undifferentiated)
(clay with thin gravel bed at
base)
Missi3sippian system
Prospect Hill formation (siltstone)
Hannibal formation (dolomite, gray to
yellow)
Maple Mill formation)
Devonian system
) (shale)
Sheffield formation )
Lime Creek formation (dolomite)
(dolomite and shale)
(shale)
Shell Rock-Cedar Valley-Wapsipinicon
Ordovician system
Maquoketa formation (shale)
(dolomite)
(shale)
(dolomite)
Galena formation (limestone)
60
50
30
140
240
Decorah-Platteville formations (lime
stone)
(shale)
St. Peter formation (sandstone)
Prairie du Chien formation (dolomite
sandy)
(sandstone, dolomitlc)
(dolomite)
745
775
915
745
775
915
1155
1155
1175
1215
1175
1215
1275
160
1275
1415
1515
1415
1515
1675
30
1675
1755
20
40
60
140
100
Cambrian system
Jordan formation (sandstone)
St. Lawrence formation (dolomite)
1755
The drift material and the consolidated rocks above the Shell Rock forma
tion are composed mostly of clay and shale. Appreciable water has not been
encountered in the limestone and dolomite beds in this interval and in places
where a large supply of water is requirei, the wells have been cased to the top
of the Shell Rock formation in this locality.
The Shell Rook, Cedar Valley and Wapsipinicon formations are potentially
water bearing. However, in general, no large supplies of water have been
encountered in these rocks in the vicinity of Hampton. The Hemp Mill well
located in the south part of Hampton was finished in rocks of Devonian age
at a depth of -4-83 feet.
a drawdown of 40 feet.
A supply of 12 gallons per minute was secured with
A well drilled at Seeds Lake State Park to an equivalent
depth of about 600 feet at Haapton, obtained a supply of 50 gallons per minute
with a drawdown of about 30 feet.
At Hampton, the static water level would
probably stand within 60 feet of the surface on the upland in a well finished
in rocks of Devonian age. The quality of the water pumped from the Hemp Mill
and State Park well is shown on the attaohed data sheet.
Mr. E. L. Patera
-3-
March 1, 1948
The next lower promising horizon is the limestone strata belonging to
the Galena and Decorah formations. These strata usually yield some water
but no large yields of water have been reported from the^e aquifers except
in city well Uo. 1.
Here a production rate of 160 gallons per minute was
reported but the accompanying drawdown was not given.
In Mason City, to the north of Hampton, a well finished in the St. Peter
formation produced 220 gallons per minute with a drawdown of 68 feet.
Large supplies of water have been developed from wells finished in the
Jordan sandstone and the underlying St. Lawrence dolomite. Analyses of
waters from wells finished in the Jordan sandstones are shown 6n the attached
data sheet.
In summary, there is a possibility of developing a supply of 100 gallons
per minute from aquifers in the Devonian system of rocks at a depth of 635
feet or less. A supply of 200 gallons per ainute might be developed from
aquifers in the St. Peter and higher formations. The most consistently
large yielding aquifers arethe Jordan sandstone and the St. Lawrence dolomite.
If we can be of further assistance to you in this matter, please let us
know.
Very truly youre,
H. G. Her3hey
HGH:WEH:ASH
Enc. 1
Sheet No; I
Location
Name of Well
...J....M.*.JL..&..^Jrrr.
.^.... Date Drilled
£fc.
Survey No
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Sheet No
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Name of Well Clhi \AjPJl. -4i^^-«
Location ...&&XK.fidl}.Jcl1....l.XiJKAJ..
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Date Drilled
/
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00
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Name of Well.
Date Drilled
Analyst!.//?.././^..
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IOWA
GEOLOGICAL
SURVEY
TABULATION OF WATER ANALYSES
COUNTY
'•*-• ••«
(parts per million)
LTOWN Well No.
Use & location
Depth' Geol.jDiss. jlns.
Ft., form. •Solids!Mat. N03
Na
,
I&Bpton H«mp Ml 11
teeds Lake
J.-._£i»te ?aj*__
/,**•
L
per.
292
600* ]&•••
3t.Peter
laaptoa City Ho. 2
i/to/vi? //
,
.
ill
Fe 1Mn j Al F
...
26.0
0.23
3.9
27.8
75.0
' 494
|Jfp Jordan
fflffl Jordan
709
J12.0
0.0
1.1 io.o !
b.4
po4|bos
,
304
1
11.0
Calc.
Hard.
I
0.6
,41.5
i
64.1 |U5.5
4.2 i 0.1
1
9.0
0.0
22.4 !105.1 33.6 | 0.2
625
25.1
0.0
65.0
0
(j? /
_
|
357
73.9 1396.5
"T
430
o#<!
g.5
.
HCO*
1.0j 6.0 1353.8
-i
27.4 0.5_!p.o4
i29-3 j 97.6
>
Cl i S04
-.
1
• -—r-
i
iaaaa city Mn. 11
Mg
Ca
54.5
65.4 1 0.5
ftrp
'• tJ
&*0
JO.O |46.0,172.4
0.0
380.8
370.9
i
1
0.0
1.2
12.01 35.0
475.8
0.9 1.0
10.0 192.0
397.7
406
3%
JJm~ r
o
f9f
/•
UL
i
1
•1
422
i
j
1
1
..
..
(..
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t>¥ Y
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1
NOEns;
^
Hampton
(FRANKLIN)
Location of City Wells 1 & 2
SW/c-NE-SW-SE-NW-54-92-20
In the pumping station, E. of town
Ground level at wells est. 40' below ground at standpipe on basis
of pressure readings, according to city clerk.
11/25/41
K.E.A.
Elevation of Oity Wells 1 & 2
Pumps set in pit in pumping station, curb (air gage, etc.)
4' below ground level
Ground level at pumping station is 45.2' below U.S.C.& G.S
B.M. at City Hall, dete mined by hand level from city
datum bench marks.
City Hall B.M. » 1147.888'
Ground Elev. = 1104.7'
Curb Elev.
- 1100.7'
ld^CUU.fj£^*d-£- it^HLINVESTIGATION OF THE GROUND WATER RESOURCES OF IOWA
IOWA GEOLOGICAL SURVEY
Mount Vernon, Iowa,
m
w:
M&™^^
Deab Sir:—
In the investigation of the deep wells of Iowa, we wish to obtain all facts relating to their present condition
and especially to any failure or deterioration and its causes. The importance of this inquiry, will I trust, en
list your cooperation. Will you kindly fill out as fully as possible the following blank as to your own well, and
return it in the enclosed envelope which requires no postage. The results of these replies will be published to
gether with much other valuable information for the information of well owners in a bulletin, a copy of which
wll be sent you gratis. Thanking you for any help you can give us.
Yours very truly,
W. H. Norton.
1. Is your deep well still in use?
kx.fv*
2. Has there been any loss of head or pressure, or diminution of flow or pumping capacity?
3. If so, when was it first noticed?
.'
;.
Or the height above
curb to which water will now rise in tube?
What is the discharge?
5. If non-flowing, how far below the curb docs the water now stand?
6. What is its present pumping capacity in gallons per minute?
l.r^?....-Ll..
£..l£..l^
Is the capacity of the pumps the same as when the well was first used?
8. Has the well been repaired by deepening
by repacking
9.
„
„
i..>...V-
by cleaning out J..I/D
When were such repairs made
and what was their effect?
or" sudden
11. Is the cause of such loss known to be either leakage around old packing
sediment
LWfy
^J.....by rimming out '.Z.v^l?..
, by recasing, (if so, mention lengths and place of new casing.)
10. In case of loss of head, was the loss gradual....;.....-:....
, rusting out of casing
and when did it occur?
tr-.Ni
i::\...i:^Af7&^h£^l
latter, mention new well and date of its completion).....J.!\..Ju4/£..J^y*kJLJ!^..^
12.
:
.'
4. If flowing, what is the present pressure of the well in pounds?
7.
'.....'.
'..S^..D.....
.^._.L.i..._
, filling up with
, interference of new well or wells, (if the
^..!Z>^^-—/-4—'—%-
Names of owners of deep wells drilled the last ten years years in your town and county and such wells in prospect
M?^a^..Zilh^
INVESTIGATION OF THE GROUND WATER RESOURCES OF IOWA
IOWA GEOLOGICAL SURVEY
.Mount Vernon, Iowa,...A.pr-il-S&,-•••'-25
M
fJfee..J.ftP.SMJ!lJLfta$.ft^tt.„Af.„.»a.tjajRKarkB
...HzffiptorAji....Ia.f
Dear Sir:—
In the investigation of the deep wells of Iowa, we wish to obtain all facts relating to their present condition
and especially to any failure or deterioration and its causes. The importance of this inquiry, will I trust, en
list your cooperation. Will you kindly fill out as fully as possible the following blank as to your own well, and
return it in the enclosed envelope which requires no postage. The results of these replies will be published to
gether with much other valuable information for the information of well owners in a bulletin, a copy of which
wll be sent you gratis. Thanking you for any help you can give us.
Yours very truly,
W. H. Norton.
1. Is your deep well still in use?
s.M..LiJ
2. Has there been any loss of head or pressure, or diminution of flow or pumping capacity?
3. If so, when was it first noticed?
A.
(£££:...:.?f<L:
If flowing, what is the present pressure of the well in pounds?
Or the height above
curb to which water will now rise in tube?
5.
What is the discharge?
If non-flowing, how far below the curb does the water now stand?
6. What is its present pumping capacity in gallons per minute?
L.i:...'~.
r.
8. Has the well been repaired by deepening
by repacking
-..<.:!.
<M41
by cleaning out
^..:.
„/..\....s.
?:.V&Jr4r:
&k$.
by rimming out
, by recasing, (if so, mention length:, and place of new casing.)
When were such repairs made
10. In case of loss of head, was the loss gradual..../^!^
sMdd.
rusting out of casing
\C*Ai.
^>.lr'.?.'^r:
and what was their effect?
or sudden
11. Is the cause of such loss known to be either leakage around old packing
sediment
./^x.
........Jr^t~.
7. Is the capacity of the pumps the same as when the well was first used?
9.
^}£^y..
$i.<<*2.
latter, mention new well and date of its completion.).....*^. QiQtrr.
,
and when did it occur? £^....
-r^^L-S?..
, filling up with
, interference of new well or wells, (if the
iifSL^fbi.
**<t ^u^-,
12. Names of owners of deep wells drilled the last ten years years in your town and county and such wells in prospect
r
I
Name of WellHatopttH l/K-GQZ L Sheet No. J_
Depth Range
^ioo - tT^ o
Scales 1 inch=10 feet
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Name of Well Hai-u pfbh l/f/'OOZJ
Depth Range
£~oo-
roc- 6? r -
Sheet No.
2z
Scale: 1 inch=lO feet*
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...
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Name of Wellf/^, p7^ U*-p$^/
7/-V
Sheet No. 3
Depth Range
(co0-7co>
Scale: 1 inch=10 feet.
5A&/o'. -Jh>-£o cp0 //ft" 6^0 wi* 7% ++cf<//s& /£>*ou/* SA<?/>, IjO-^ok^
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Depth Range
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