ML20199C243

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Regional & Local Geologic Summary at C-E Hematite,Missouri Plant
ML20199C243
Person / Time
Site: 07000036
Issue date: 05/30/1997
From:
External (Affiliation Not Assigned)
To:
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ML20198N074 List:
References
96A002, 96A2, NUDOCS 9711190278
Download: ML20199C243 (54)


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Geologic Summary at the Combustion Engineering, g

Hematite, Missouri Plant E

g Combustion Engineering Hematite, Missouri

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May 30,1997 6&L'LL9 0 US I

GATEWAY ENVIRONMENTAL ASSOCIATES. INC.

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. Regional and Local Geologic Summary at the Combustion Engineering IIematite, Missouri Plant 96A002 l

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Prepared for Combustion Engineering Hematite, Alisson?i E

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E May 30,1997 REUSE OF DOCUMENTS E

Tks &<ument has ' peen developed for a specitle apphcanon amt out for general use, therefore,it may not b. used thout the written arpeoval of Cmeeway Envuonrnantal Associates,Inc,. Unapproved use is at the sole responsikhty of Copyright *, Gateway Environmental Associates,Inc.1997 E

2084 Crmgshas Drive. St Lesis, Missouri 63146,314'205805). FAX: 314/434-4 4

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Table of Contents I ntrod uction................................................................. 1 l

1.0 Regional Geologic Setting................................................... 2 1.1 Bedrock and Structure................................................... 2 1.2 Unconsolidated Deposits................................................. 2 Figure 1 - Isopach Map Jefferson City Dolomite.............................. 3 Figure 2 - Bedrock Geologic Map.......................................... 4 Figure 3 - Schematic Geologic Statigraphic Column............................ i 8

Figure 4 - Schematic Geologic X Section.................................... 6 g

2.0 Regic.ai Hydrologic / Water Supply Information................................. 8 l45 2.1 Precipitation and Steam Characteristics.................................,.... 8 2.2 Wat er S upply.......................................................... 8 2.2.1 S urfac e Water..................................................... 8 8

2.2.2 G ro un d wat e r...................................................... 8 Figure 5 - Drainage Systems.............................................. 9 l

Figure 6 - Stream Flow Characteristics Joachim Creek......................... 10 Figure 7 - Losing Streams, Springs, and Karst Features......................... I1 Figure 8 - Aquifer Usage Group and Areal Extent............................,12 l

2.2.2.1 Spccific Groundwater Use......................................... 13 -

2.3 Regional Potentiometric Map............................................ 13 Figure 9 - Equivalent Freshv r r IIcad..................................... 14 0

3.0 Site Specific Geology - Hydrolog;

......................................15 3.1 Site Specific Physiography.............................................. 15 0

3.2 Site Specific Stratigraphy............................................... 15 3.2.1 Unconsolidated Sediments (Pleistocene Quatemary)...................... 15 3.2.2 Site Specific Bedrock Stratigraphy.................................... 16 8

Figure 10 - Regional Site Location Topographic Map......................... 17 Figure 11 - Depth to Top of Fat Clay...................................... 18 I

3.2.3 Pertinent Site Specific Well Completion Information..................... 19 3.3 Site Specific Hydrology................................................ 19 3.3.1 Surface Water Features............................................. 19 g

3.3.2 G roundwater Surface.............................................. 19 Figure 12 - Groundwater Elevation Contour Map............................. 20 4.0 S ummary............................................................ 21 Re ferences............................................................... 2 2 E

Appendix A - MDNR Specific Water Well Data Appendix B - MDNR Well Log # 14993

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E Regional and Local Geologic Summary '

of the Combustion Engineering. Hematite. Missouri Plant Introduction g

This geologic summary was produced to demonstrate an understanding of the geologic features E

occurring at and near the Combustion Engineering (CE) plant in Hematite, MO and to document a thorough successful search for known information. Gateway Environmental Assor' tes,Inc.

(Gateway) procured data from public information sources, case files of the Missoun Department of Natural Resources (MDNR) Division of Geology and Land Survey (DOLS), the United States Geological Survey (USGS) and several private sources. Meetings were held between Gateway, DGLS and USGS tecquire the technical information cited and otherwise used in this report.

This document should be considered an executive summary for interested parties wisning to understand the geology and hydrogeology of the area. This document was produced to assist CE, their consuhants and regulators who may wish to use the infonnation to guide the negotiation and development of a site specific hydrogeologic investigation work plan.

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Regional and Local Geologic Summary at the Coubution Engineering, llen: tite, Missouri Plant n

1.0 Regional Geologic Setting g

1.1 Bedrock and Structure N

The site is in northern JefTerson County which is on the north, northeast flank of the Pre-Cambrian age St. Frrncis Mountains, Ozark Dome. Cambrian, Ordovician, Siluriar. 'evonian i

and Mississippian sedimentary formations of various depositional environments are dra}<d on the flanks of the dome. CE's llematite, Mo. plant is situated over these format, ions. Based upon the 1979 official Missouri Geologic Map and the Bedrock Geologic Map of the Festus 7.5 1

Minute Quadrangle by Whitfield and Middendorf, the uppermost bedrock beneath the site is the lower Orhvician Canadian series, Jefferson City Dolomite. Figure I from a 1991 DGLS publication, is an isopach map of the Jefferson City Dolomite. Figure 2 :: hows the site in E

reference to the DGLS bedrock geologic map.

The lefferson City Dolomite is described by Martin et al. (1961) as mootly light-browr. io medium-bn wn, medium to finely crystalline dolomite and argillaceous dolomite. Chert which is not abundant, is typicahy oolitic, banded, mottled or sandy. Lithologic ::uccession within the formation is extremely complex and varies among locations. The Jefferson City Dolomite,125 to 325 feet thick in the state, is bounded by the overlying Cotter Formation and beneath by the Roubidoux Formation. Figure 3 is a stratigraphic column showing lithologies and the relationships of the formations taken from the Bedrock Geologic Map of the Festus 7.5 Minute Quadrangle by Whitfield mid Middendorf.

The sedimentary rocks in this area dip very slightly and uniformly to the north, north-east. There are no mapped or suspcted faults within several miles of the site.

k I.2 Unconsolidated Deposits The site is positioned in the valley of the Joachim Creek which has incised into the surrounding Cotter ar ! Jefferson City For T at ons. During late Pleistocene glacial regression, terrace units i

were deposited in the Joachim Creek valley. These units are chiefly derived from loess and colluvium. Meiu (1992) stated that three processes are responsible for the deposition of valley fill (terrace). They are changes in groundwater base level, changes in level of the sediment source area or significant change of c'imate in the source area and increase in sediment load from the contributing stream. Later during tac Holocene, alluvium was deposited in the Joachim Creek valley. Figure 4 is a schematic cross-udion depicting these stratigraphic relations.

The MDNR's Bedrock Geologic Map of the Festus 7.5 Minute Quadrangle by Whitfield and Mid lendorf describes the Flolocene alluvium as clay, silt, sand and gravel chiefly derived from local loess and colluvium. Colluvium is described as a mixture of residuum, from fines to A:\\R JEOSUht.WPD 2

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Regional and Local Geologic Summary

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cobbles, and loess that is moving down slope as a result of slope wash and gravity. Colluvium accumulates at the base of valley slopes and in large valleys washes onto the floodplain, blending l

with the alluvium.

The MDNR's Bedrock Geologic Map of the Festus 7.5 Minute Quadrangle by Whitfield and I

Middendorf, describes terrace deposits as clay, silt, sand and gravel chiefly derived from local loess and colluvium. Terraces contain lenticular beds of sand and gravel interbedded with silt and clay.

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Regional and Local Geologic Summary at the Combustion Engineering, Hematite. Missouri Plant I

2.0 Regional Hydrologic / Water Supply Information G

i 2.1 Precipitation and Steam Characteristics The Missouri Water Atlas produced by the MDNR in 1986 was referenced to determine the following. Figure 5 identifies that the area is in the Mississippi River drainage basin. The area receives 38 inches average of annual precipitation with 12 inches average of annual runoff. The I

E maximum 10 day event expected precipitation is 9 inches in a given 25 year returm g-Obtained from the atlas, Figure 6 shows that Joachim Creek is a permanent flowing stream indicative of a shallow groundwater discharge point. Figure 7 shows the losing streams in the basin. Incidentally, Figure 7 also shows major springs in the drainage basin, but dc,es not show the spring (discussed later) near the site.

Water Resources Report 25 estimates the Lase flow reces" 1, which is the amount of water h

which will flow in a stream after a 30 day rainless period. 'ne base flow recession minimum observed flow from 1961 through 1965 on the Joachim Creek is 0.2 cubic feet per second. These data indicate the stream is gaining.

1 2.2 Water Supp!y 5

2.2.1 Surface Water There are no public water supply intakes on Joachim Creek. According to the EPA field investigation report (1990) most of the residents of Hematitc receive their crir. king water from Rural Water District # 5. The report also states # tt surface water is not used for drinking water E

within a four mile radius of the site. This statement is probably correct but may be somewhat flawed in that the report incorrectly located the site on its map.

2.2.2 Groundwater E-According to Water Resources Report 30 produced in 1974 by the USGS and the Missouri Geological Survey (currently named DGLS), domestic anu industrial water wells 10 the vicinity produce water from the Powell - Gasconade aquifer group which includes the Jefferwn City Dolomite. Wells in the area, especially to the west and southwest, intersect the Jefferson City Dolomite ifit is present, but do not derive significant quantities of water from it. The Jefferson City Dolomite is generally not capable of sustained water production because ofits low storage capacity. Report 30 states that small supplies can be developed in the Jefferson City Dolomite among other fonnations, but are subject to failure during drought or sustained pumping. Figure 8

~ from luport 30 shows the aquifer usc.ge by S.,up and areal extent.

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r-Regiond and Local Geologic Summary at the Combustion Engineering, llcmatue. Missouri Plant E

2.2.2.1 Spedfic Groundwater Use l

The h1DNR's Well llead Protection Division maintains records of specific private water wells.

A two mile radius around the CE site was searched for records of private and public water supply a

wells. Infonnation on twenty two wells is in the MDNR files, including the site's own water 4

supply wdl. Infonnation pertaining to depth of well, casing intervals, stratigraphy, yield and static water level are included in the data. Appendix A contains the data set as acquired from the E

MDNR files and a figure showing a two mile radiunf the site where the wells occur. (The specific addresses of the wells may have to be obteined to post the exact location of the wells.)

This infonnation may be used later if necessary, to detennine potential groundwater receptors.

2.3 Regional Potentiometric Map D.G. Jorgenson (1986) et. al produced an equivalent freshwater head and dissolved solids concentration map of the Cambrian, Ordovician and Mississippian aquifers. This map covers a E

!arge area of the mid-cominent including the CE site. Figure 9 shows the portion of the map covering the site. The map demonstrates that the potential head of the Cambrian, Ordovician and Mississippian aquifers is high to the ;outhwest and low to the northeast, thus illustrating that g

regional deep potable groundwater flows to the northeast in the area of the site.

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R *gionaland Local Geologic Summary at si< combustion n incering. Hematue. Missourt Plant l

s 3.0 Site Specific Geology - Hydrology 3.1 Site Specific Physiography The site is located in the physiographic subregion of the Ozark Mountains called the Salem Plateau which is characterized by gently rolling hills of moderate topographic relief and gradient.

A topographic site figure showing the general location of the site along with generalized topographic features is included as Figure 10. It shows that the plant is located, between the hills to the northwest and floodplain of the Joachim Creek to the southeast. The plant is located on a tenace deposit which has topography that dips gently to the southeast. Southeast of the plant approximately 400 feet, the ground surface elevation then drops into the alluvial plain of Joachim i

l Creek. Northeast of the plant approximately 300 feet, the surface elevation drops into a tributary g

of Joachim Creek. Joachim Creek flows into the Mississippi River near licrculaneum.

l 3.1.1 Aerial Photography E

Two major aerial photo scarch and archive firms were solicited for all available photos of the site. Gateway was only able to acquired aerial photographs of the site for the years of 1962 and E

1971. Unfortunately, neither of these photo sets shows open burial pits. The DGLS has a 1967 l

aerial photo on file which Gateway reviewed, showing open burial pits.

3.2 Site Specific Stratigraphy t

3.2.1 Unconsolidated Sediments (Pleistocene Quaternary)

Several subsurface investigations within the terrace deposit at and near the plant have produced k

geotechnical and geologic infonnation which allows a general stratigraphic interpretation to be made.

In 1967 Woodward Clyde - Sherard and Associates produced a subsurface geotechnical report which includes information on two borings. Boring B-1 found silty clay to 13.5 feet below E

ground surface (bgs), a stiff highly plastic (fat) clay from 13.5 feet bgs to 21.5 feet bgs which graded to a sandy silty clay which flowed water at 22 feet bgs. Water stabilized at 13 feet bgs.

The boring continued through a sandy silty clay to 32 feet bgs where it encountered limestone g

pieces in a sandy clay matrix. Auger refusal occurred at 36.5 feet bgs where limestone pieces occurred. That point was probably at the Jefferson City Dolomite. Boring B 2 found a very similar sequence with similar depths of equivalent stratigraphic units, in 1978 Woodward Clyde installed two more geotechnical borings. Boring B 1 of this study encountered a silty elay to 16 feet bgs at which point it graded to a fat clay, in this boring the fat l

clay contained sand layers 2 3 inches thick. The fat clay with sandy stringers continued in this

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Regionaland LocalGeologte Summary at the Combustion Engineering. Hematite. Missourt Plant boring to 34 feet bgs where a medium grain sand occurred. From 34 feet bgs to 44 feet bgs the log shows a poorly cemented calet.reous sandstone which is likely limestone that was pulverized l

by the pounding split spoon sampler. Boring B 2 nearby showed a similar stratigraphic sequence.

l In 1988 Shannon and Wilson, Inc. (SWI) installed six geotechnical borings which show similar stratigraphic sequence to the two previous Woodward. Clyde reports. During 1991 SWI conducted another geotechnical investigation, installing eight more borings. Only one of these I

eight was advanced below 22 feet. The eight logs report a silty clay shallow foll, owed by a fat clay present at 8 feet to 10 feet bgs. Boring SW 3 was installed to 32 feet bgs, which encountered similar stratigraphy to other borings of equal depth.

During August of 1996, Gateway performed a limited shallow stratigraphy and groundwater l

quality analysis to determine the source of technicium - 99 (" Tc) in a specific groundwater monitoring well. Gateway installed twelve borings and temporary groundwater monitoring wells mnging from 15 feet to 22 feet bgs. Subsurface information generated from this study supports l

the cancept that there in sitty clay unit near the surface bounded on the bottom by a fat clay unit.

Also in August of 1996, Gateway perfonned a limited shallow stratigraphic analysis of an a..>3 at the plar: 'dentified as the evaporation ponds. Six borings in that investigation were installec. to l

20 feet bgs. Each encountered 2 feet to 5 feet of silty fill initially, followed by a silty clay to 20 I

feet bgs. A fat clay was not noted in that area, likely because the borings did not reach sufficient depth. Boring Ep-3 encountered a sandy silt 18.5 feet bgs to total depth.

Figure 11 shows the top of fat clay as determined from locations of the geotechnical borings installed for the four geotechnical studies as well as the 18 borings installed by Gateway. This l

map is useful for a gross determination only, because elevation assumptions are inherent in its construction. That map shows that a fat clay exist beneath the site at varying depths. Some borings may have not been advanced deep enough to encounter the fat clay.

3.2.2 Site Specific Bedrock Stratigraphy In 1956 hintlinckrodt Chemical Company installed an industrial high capacity water supply well for the plant. The hiDNR geologic log (number 14993) documents the bedrock stratigraphy encountered by the well. Unconsolidated sediments are present to 35 feet bgs. The JetTerson I

City Dolomite was present from 35 feet bgs to 125 feet bgs. The Roubidioux was encountered from 125 bgs to 255 feet bgs, the Gasconade from 255 feet bgs to 470 bgs, the Gunter Sandstone hiember of the Gasconade from 455 feet bgs to 470 feet bgs and the Eminence Dolomite from 470 feet bgs to the total depth which is 600 feet bgs. The hiDNR's stratigraphy data and log for this wellis presented in Appendix B.

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Shonnon & Wilson. December.1991 Report N

Combustion Engineerino Depth (feet Delow yound surfoce) to too of Fot (04) Ooy Figure 11 19 Shannon & Wilson. Ju8y.1968 Report Dep o's to Top of Fat Cloy cepth (seet beo. yound ufoce) to top of ret to4) Ooy

(

0,n wood erd - oyde - shepard & Assoc., uy. 59s7 Report Hemotite Focility Depth (feet betow yound su foce) to top of Fat (04) cey Gote-ey Eneronme,tos Assoc w es r

wood ord - Oyde Coasuttants. Fetrvory.1978 Report g

~

gen,* 1 = 150 g,'" 4/23/97 Dept * (feet beo. yound wfoce) to te of Fat (W) Ooy O: cate.oy En-m..nentor Assoc.. september.

16 1996 wsse ee, stereo wg :t w t***vf** M A.M s g_A

~-

._(

E Regional and Local Geologic Summary at the combustion Engineering. Itematite. Missourt Plant I

3.23 Pertinent $lte Specific Well Completion Information l

A very important note concerning this well is that upon completion, the well flowed, indicating artesian conditions in at least one of the hydrostratigraphie units it drilled through or into. The casing was set in this well from surface to 220 feet bgs, near the top of the high yield sandstone l

portions of the Roubidioux Formation, g

3.3 Site Specific Hydrology 33.1 Surface Water Features There are five major surface water features at and near the site; Joachim Creek, a spring and its tributary to the Joachim Creek west of the plant, an intermittent tributary of the Joachim Creek l

north of the plant and the plants evaporation ponds. These features all play a roll in determining the movement of groundwater at the site.

3.3.2 Groundwater Surface During the summer of 1996, Gateway Environmental Associates, Inc. created a groundwater R

elevation map. The map shown in Figure 12 is only as accurate as the limited hydrostratigraphic information would allow. This map shows a shallow groundwater high south of the plant with increasing gradients to the west, east and north. Since the lithology is unknown in some of the older piezometers used to create the rnap, there is a chance that hydrostratigraphie units at.d potentiometric surfaces may be mixed in the groundwater surface representation. It is apparent that shallow groundwater generally moves to the Joachim Creek.

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E RegionalandLocal Geologic Summary at the Combustion Engineering. Hematite. Miswuri Plant 4.0 Summary Sufficient general and site specific information is available to create a dependable understanding regarding the geology, hydrogeology and hydrodynarnics of the area. Major aquifers in the area have been identified as well as actual uses of those aquifers, both deep and shallow. The bedrock structural features and stratigraphic relations have been recognized. Unconsolidated sediments, their depositional environment, lithology and stratigraphic relations have been distinguished.

l Information regarding surface water flow and usage has been included.

Deep groundwater flows to the northeast and is discharged to the Mississippi River Valley. In E

fact there is evidence that the bedrock aquifer (s) beneath the site is (are) artesian. The Jefferson City Dolomite the upperrnost bedrock unit at the site is not hydraulically suitable for a water I

supply because it has low hydraulic conductivity. Shallow groundwater flows toward the Joachim Creek which has been identified as a permanent flowing gaining stream.

There is a low permeability fat clay unit present within the terrace deposit. That fat clay may act as a barrier to the downward movement of perched groundwater.

I I

I

.I I

I I

i 1

AAR411:OSUM.WPD 21

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v m

Regional an.1 Local Geologic Summary at the Combustion Engineering. Hematite. Missouri Plant ll References l

Skelton, John, Low-Flow Charatteristics ef Missouri Sutams, Date Unknown, Water Resources j

Report 20, Missouri Geological Survey and Water Resources.

Whitfield, John W. and Middendorf, Mark A., Bedrock Geologic Man of the Festus 7.5 minute j

Quadrangle Jefferson County. Missouri, Date Unknown, Missouri Department of Natural Resources, Division of Geology and Land Survey, Geological Survey Progrmn.

Ecstus Quadrangle Missouri Jerrerson County 7.5 Minute Series (Topogranhici, Date Unknown United States Department ofinterior Geological Survey.

hiissomil'aler Atlas,1986, Missouri Department of Natural Resources, Division of Geology and Land Survey, Jorgenson, D.G.,llelgesen, J.O., Leonard, R.B., and Signor, D.C. Equivalent Freshwater llead andfissolved-Solids Concentration of Water in Rocks of Cambrian. Ordovician. and hiissmippian Age _inalle Northern Mideontir.tente US A,1986, U.S. Geological Survey.

Peterson, M.S., Floods of June 17-18.1964 in Jefferssn. Ste. Genevieve and St. Francois Counties. hiinenti, October 1965, Water Resources Division, U.S.G.S.

Thompson, Thomas L., Paleozoic Succession in Missouri. Part 2 Ordovician System,1991, Missouri Department of Natural Resources, Division of Geology and Land Survey.

McCracken, Earl and McCracken, Mary 11., Subsurface Maps of the Lower Ordovician (Canadian Series) of Missouri, July 1965, State of Missouri, Department of Business and Administration, Division of Geological Survey and Water Resources.

I Miller, Don E., Emmett, L.F., Skelton, John, Jeffery, ll G., and Barks, J.H., Water Resources of the St. Louis Area. Missouri, Rolla, Missouri,1974, Missouri Geological Survey and Water Resources and U.S. Geological Survey.

Skelton, John,llase Flow Recession Characteristics and Seasonal Low Flow Frequency Characteristics for Missouri Streams, Date Unknown.

Booth, L.F., GrofT, D.W., Peck, S.I., McDowell, G.S., Somers, W.M., Bronson. F.L.,

itadiological Survey of the Combustion Encineering Burial Site.11ematite. Missouri, July 1983, Radiation Managemerr, Corporation, Division of Fuel Cycle and Material Safety, Office of Nuclear Material Safety and Safeguards, U.S. Nuclear Regulatory Commission.

A%Gl!OsUht WPD 22 i

f

-s Regionaland Local Geologic Summary at the Combustion Engineering, Hematite. Missouri Plant p

Mearns, Susan L., Ph.D., Preliminary Assessment 11ematite Radioactive Site. llematite, L

Jefferson County.Missemi, April 10,1990, E&E/ Fit for Region Vil EPA. Ecology and Environment, Inc., Field Investigation Team Zone 11, Contract No. 68 01-7347, EPA llazardous Site Evaluation Division.

Oateway Environmental Associates, Inc., Renort of Groundwater Monitoring Well Installation.

{

Abandonments and Maintenance - 1 imited Groundwater livdrodynamics Investigation at the Hematite. Missouri Plant. ABB Combustionfngineering Nuclear Fuel. Combustion Engineering. Inc., July 26,1996.

Gateway Environmental Associates, Inc., Investigation to Determine the Source of Technetiun:-

99 in Groundwater Monitorine Wells 17 and 17B. Combustion Encineerine. llematite.

[

Missouri, September 27,19965

~

[

Shannon & Wilson, Inc., New Pelletizing Storage / Utilities and Warehouse Facilities.11ematite.

Missouri. Combustior: Engineering, July 14,1988.

[

Shannon & Wilson, Inc., Geotechnical Investigation Industrial Waxhouse and Office Building L

Hematite. Missouri, Date Unknown.

Woodward-Clyde Consultants, Soil and Foundation Investigation made for the Proposed Oxide Expansion to Existine Facilities in llenlatile. Missouri. Combustion Fncineering. Inc.,

February 13,1978.

f Woodward-Clyde Consultants, Subsurface investigation Semi Works Oxide & Pellet Plant United Nuclear Cornoration.11ematite. Missouri, July 28,1967.

Missouri Department of Natural Resources, Division of Geology and Land Survey, ABB-Combustion Engineering. Nuclear Fuel Plant. llematite. Missouri Reoort of Findings, November 22,1996.

IJnited States Army Corp of Engineers, Water Resources Science CE890 Special Project Pleistocene Fluctuations in Vallev 1.evels at the Former Weldon Snrine Ordnance Works Syncrftmd Site. St. Charles Co. Missouri. Donald 11. Meier, April,1991 AAR-Gl'03Uht.WPD 23

fi^

's iW i

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(~

APPENDIX A

[

MDNR Specific Water Well Data r

O e

E E

E E

E E

E E

E E

E a

l t

g

.I 1

" "h' * **'*" *"***

El T OF NATURAL RESOURCES i

DIVISION OF GEO!.OGY AND tAND SURVEY f

I P.O. Inox 250 111 Fairgrounds Rd. Rolla, MO 654024250 l

y_,

/

(573) 368 2100 i

r rax om **mi w

~

tj The Water Well Driller's Act (256.600 - 256.640, RShio ) became effective on September 30, 1986. This law required that well drillers meet certain minimum construction requacments c.nd j

report information on all wells drilled in the state of hilssouri after this date. The enclosed data is the information we have on file for wells drilled aller 1986 in the area you requested. The information supplied to us is considered accurate, but has not been verified in every instance. We y

are providing the data we have been given and hope the following list will clarify any questions you might have regarding abbreviations used in the attachtnent. -Ifyou have any questions or need additional information, please feel free to contact Sharon Beistel at (573) 368 2168.

,H W

ADi!REVIATION EXPLANATION i

REFNUh1 INTERNAL NUh1 BERING SYSTEhi USED IN 4

y TRACKING TIIE WELL RECORDS SUBhilTTED TO OUR OFFICE

,~

SWL STATIC WATER LEVEL - hiEASURED IN FEET

.~

FROh! Tile LAND SURFACE DOWN YlELD hiEASURED IN GALLONS PER hilNOTE i

l USE D-DOhiESTIC WELL M

F-h1ULTI FAhilLY WELL N

11-IIEAT PUhfP WELL l-IRRIGATION WELL M

hi-h10NITORING WELL W-N-NON COhihiUNITY WELL i~

0-OTHER N

P. PUBLIC WATER SUPPLY WELL

_J TOTAL D

  • ~,

TOTAL DEPTH hiEASURED IN FEET H

.q J

n U

.L

\\

as_

Ay

~

V E

-lr...*.,

l

=.

n C

u cemen. o<-e=, e oma mm. on=

NT dF NATURAL RESOURCES r

4 y

DIVISION OF GEOLOGY AND LAND SURVEY q

P.O. Box 250 - 111 Fairgrounds Rd. Rolla, MO 65402 0250 N

(573) 3(6 2100 m

ru msowam 1

4 L

b Fk Prior to the passing of the Water Well Driller's Act in 1986, well cons:ruction was reported on a voluntary basis. The well driller would submit drilling samples and a geologist would evaluate the 7

samples and then compose a log based on the evaluation. Those logs have now been automated M

and are being reviewed for accuracy.

Ifyou have any questions or need additional information, please feel free to call Sharon Beistel at (573) 368-2168.

rk 2

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~-- - -

w tog N Owner:WOLK, WALTER Stv0 Cnty:JEFFCASON

" !1163

'.B LC SC 1RS: 93P T41% ROGi:

Alias:

Lat.233,14,14.125N

'ype sell: Private Well Long. 90,k9, 1.495W

, loi; S

Qued 3tT030b4 Aler:SHCPARD Wf.LL DRLD Date 04/1962 raller Libeen'i.e H Conficenttal:N eie leat.e Dt.

/

mguger:C.F.f;0l(R150N Dat e: 04/1962

s v. : 605 Elev.S Yields 10 SWL (a)150 H2O t 300-350' i
f. D, 2 350 oace:

DrDwns SWL:(t)

TL e

roch at:

10 D a m pl e t. baved:Y Int, corecs 0 to 0

You Fm.300WELL DOLO 14ITC

^ - f m. :JEfff RLO4 Cli s' bOLumil; alems t emarks


Const ruet 1 on bot a-gM 0P1163 Date Comoloted 04/1962 SING: Doth:

40 Diani: 6.25 1/0:0 St. Hole: 0.00 St. Delows 6.25 0

0.00 0

0.00 0

0.90

.uddi:

Type har

/1et mi b t: n a n t, Plup Date Too botttim u

ND:

Cap lype bet at TDH Scrn lyn Size Lpth Glot 0

0 0

0 0

0 11 Treat Tyne Dev ra Comol 6'e r f.

Int er val T u tie P 'v e t,. Oil G a r.

T 109:

0 Bot 0

on Top:POWELL D0 tor;IL t ma t.i ons bot :JCff CTdiON ult Y DOL 0 NITE Other data sources:

meram


St rat i p ra p 9 y ba t a 14 :021163

-Litn-


Minerals-----

bat'e Name Pr Sc Mn Pri Oc Sec Oc Mnr Oc 0

10 H0 GnnPLCG 0

0 0

'O 350 ORDOVICIAN LYSitM o

0 0

0 350 CANADIAN SCRIES 0

0 0

.0 DO POWELL DOLOMITC DL Cri SH 0

0 0

50 260 COTIC4 DOLOMITE DL Ch GD 0

0 0

0 350 JEFFERSON CITY DOL 0nlTE DL CH SH ZnS 1

0 0

0 350 TOTAL DEPTH 0

0 0

oted on 05/20/97 at 07:44:56.

a 1


Header Data--------------

4 Log it Owner BECK, FAANK St:MO Cnty JEFFERSON l

P2655 TRS: $06 T40H ROSE Allas Lat.:

j type well: Private Well 1.ong. :

Enlog Ouad: UNKNOWN S

31er:WELCli BROS Date:10/1963 fdrillerLiscenseits Confidential:N Release Dt.

/

j ger:H.n.GROVCS Date:06/1964 I

l v.

$30 Clev.S Ytelds la SWLa(a) 1120 e' 200' l

T.D.*

220 bases DrDwn:

SWL (b)

IL l

tock ats O

Samples saved:H Int. cored:.

O to 0

l To r) Fw 3 COTTER DOL 0nITC rm. COTTER DOL 0ri1TC

{

blems i

l av4:ss2.5 MI S OF HWY A, 2.5 til W Or HENA11TC I

l' l

f


Coustruetion Data----------

l l

g 11:022655 Date Completed 10/1963 l

?

)

SING: Doth:

15-Diam: 6.60 I/0:0 St. Hole: 0.00 Sz. Below: 5.60 0

0.00 j

0 0.00 O

0.00 007:

Type Hip netha Dt Auna Plup Date Top Bottom

/

/

0 0

l IMP Cap Type Set at TDH Sctn Tyo

$12e Lpth S}ot 0

0 0

0 0

0

^

11 Treat Type Dev Typ Comp 1 Perf. Interval tube Pres. Oil Gas i

Tops 0 bot:

0 i

4, a.en Top 4 COTTER DOLOMITC

(

rmations liot: COTTER DOLONITC Other' data soureuss i

Emeritus

{

- - - - -- - - - - - - S-t r a t. i o e a o h y Data l

t 11 :022655

--L i to -


M i ne r a i s --- --- --

i W~iDar,eName Dr Se Mn Pri Oc Sec Oc Nnr De 0 220 ORDOVICIAN SYSTCM 0

0 0

I f

L

'O 220 CANADIAN SCRIES 0

0 0=

l 0 220 COTTER DOLOMITC DL CH SD ZnS 4

0 0

JO 200 TOTAL DEPTH 0

0 0

nted on.05/22/97 at 07:46:00.

4 1

---Header Data

$.og M OwneranUE(.KER, WALTER Stan0 Cnty: JEFFERSON

'0 3 '/1 fE SE NE TRS: 507 140N ROSE Alias:

Lat.838,12,33.646N 9ewell:Petvate Well Leng.190,26,56.673W log S

Quad:38090B4 1e r it'ELCH FROS Date:06/1961 1

ler Lascense W:

Confidential:H Release Dt.

/

. o e tie r : C. E. RODE R T GON Date:03/1962

.: 682 Elev.S Yields 3.75 SWLa(a) 55 1420 0:65', 125', 275'

.D.:

305 base DrDwn:

SWL a (b)

TL N

rock at:

5 Satopleb baved Y Int. cored:

0 to 0

'o9 fm. COTTEN 00LOl1! T L ara fm.:ROUDIDOUX FORMATION

lems:

M wthst

- -Con 5 t ruet i on Data----------

y N:020371 Date Completed 06/1961 eil rab Doth:

24 Diam: 6.25 1/0:1 Sr. Hole C.00 Sr. Delow 6.00 0

0.00

~

0 0.00 O

0.00 v uuft irpe xap ne t tia Dt sone e'aup Date Too bot wm

/

/

O O

m VD:

Cao Type bet at TDH Sern Tro Bize L p t ri Mot 0

0 0

0 0

0 s

11 Treat Type Dev Typ Comol Perf. Interval Tube Pres. 011 Des 100:

0 bot:

O m

Top COT TER DOL 0 NITE

_ rmations Dot:ROUDIDOUX F0kdAT10N Other data sources

%an s.:

d---


5t ra t i p r a ary Da t a-e n:020371

--L1th-- --~ ~~---Minerais-- - ---

Bate Nanie

'r Se nn Pri Oc Sec Oc nor Oc

~0 5 RCSIDUUI1 & TOP SOIL CL Co 0

0 0

5 305 ORDOVICIAN SYb1En 0

0 0

5 305 CANADIAN SERIES 0

0 0

%S 65 C0rTER DOLOMITE DL CH SD 0

0 0

65 185 JEFFERSON CITY DOL 0aITE DL Cet SD reg 2 6

0 0

30S ROUDIDOUX FORMAT 10H DL SD CH reS2 1

0 0

a 5 305 TOTAL DEPTH 0

0 0

lunted on 05/22/7/ at 07:46: 12.

aum


Headet Data--------------

Log N Owner: JONES, WILLIAN JEWELL REV St:MO Cnty: JEFFERSON B16785 NE SW SW TRS: $09 T40N ROLE H11ast Lat. 38,12,21.779N ype well: Private Well Long.390,20,41.660W

,109: S Quad 3309004 11er: SCOTT DRLD CD Da t e : 09/1'/57 ller L15 cense Na Confidential:N Release Dt.

/

ger:J. WELLS Date:11/1957

.: 447 Elev.S Yield SWL (a)000 H2O 0:

. D. :

225 Dase DrDwns SWL a (o)

.3 TL rock ats 35 Samples e,aved:N Int. coredt 0 to 0

og Fne. JEfrE9504 CITY DOLONITE in.:GASCONADE DOLONITC 5'91 ems:

n arks 0LD WELL DEEPENED (H20923) IN 1960 225-590' EgH016785


Construction Data-------

Date Completed 09/1957 Doth:

235 Diam: 6.00 1/0:0 Gr. Hole: 0.00 Sr. Below: 0.00 EGING:

0 0.00 0

0.00 0

0.00

.OU1 Trae Rip nethe Dt Abnu Piup Date Too bottom G

/

/

0 0

m's Cap lyse Set at T Drt Bern Tro Site L tth Slot 0

0 0

0 0

0 11 Treat Type Dev Typ Compl Derf. Interval T u be P'r et,.

011 G a s, Too:

0 Dot:

O en Too:GASCONADE DOL 0 NITE r nia t i o ns, bot:GASCONADE DOLOmi1E utner data sources:

ra a r P.t

--Stra t

.1 p r a p 4 y Da t a H 016735

- L i cn - - - - --- - - - ni ne r a l s - --- -

bat,e Nanie Pr Se nn Pri Oc Sec Oc Nor Oc 0

35 NO SAMPLES 0

0 0

15 390 ORDOVICIAN SYSTEM 0

0 0

5 390 CANADIAN SERIES O

O O

5 90 JEFFERSON CITY DOLONITE DL CH SD 0

0 0

90 215 R00blDOUX FORnATION DL Crt SS Zns 1

0 0

5 390 G"4SCONADE DOLOMITC Dt. SD CH 0

0 0

0 590 NO SanPLES 0

0 0

YJO 590 TOTAL DEPTH 0

0 0

nted on 05/22/97 at 07:46: 48.

I


Header Data--------------

f Log II Owner: JONES, WILLIAM J.

Stan0 Cnty:JEFFEASON lg20923 NC SW SW TRS: SO9 740N ROSE I

l5 Alias:

Lat.238,12,18.512N ype well: Private Well Long.:90,28,42.356W l

Quad 38090B4 j

j l

e logs S

i i

11er: SCOTT JRLG CD Date:03/1960 Confidential:N Release Dt.

/

.er 11er Liscense H r

ger:C.E.ROBERTSON Date 11/1962 i

v.: 447 Elev.t Yield O

SWL (a)

H2O es 71.

(

.D.:

390. base

.$ r Dw n :

0 SWL (D) j toch at:9999 Samples, t,aved:N Int, cored:

0 to 0

'oa rm.
JEFFERSON CITY DOLOMITC i

rm. UPPER GASCON4DC DOLONITC ol esis arks 0LD WELL DCEPENEDC - SCE LOG H16785 I


Construetion Data-g N 020923 Date Completed:03/1960 1

Doth:

23$ Diam 6.00 I/0:0 St. Hole: 0.00 Sr. Below 0.00 i

831N0:

0 0.00 0

0.00 0

0.00 OUI:

Type Hip hetnd Dt Aonc Plup Date Top bottom

/

/

0 0

WP P Can Type bet. at T Dit Setn Typ Stre Lpth Slot J

0 0

0 0

0 0

11 Treat Type Dev Typ Comp 1 Perf. Intetval Tu tie P r e t.. 021 G a s, Too:

0 Tiot O

Top JEFFERSON CITY DOL 0nITC en

. r m a t i o ni.

Dot: UPPER GAOCONADE DOL 0nITC

Otner cata sources

t b ei l' t! E

)E IE

?rinted on 0L/22/97 at 07
46:52.

I E

J

~

_.. _ _........ _, _ _ _ _. _.. ~ _... _.., _,,, _ _,,..., _. _ -...

m_,

1 i

'------------Head er Data--------------

1 1 1 og N Ow.ser: ENGLAND, W.R.

M1 Stan0 Cnty: JEFFERSON SE NW SW TRS: S03 T40N ROSE B)2485 Alias:

Lat.:

fue well
Prf vate Well Long.:

t 106: S Quad: UNKNOWN E11er:HAVERSTICK, C.W.

Date:10/1931 briller Liscense H Confidential:N Release Dt.

/

!r ger: CHARLES GLCASON Date

/

ev. : 430 Elev.S Yields 48 SWt: (a)000 h20 9:230', 275', 298', 380',

).D.:

SPS base:

DrDwn:

SWLa(o) 450' TL r ese r at ES Samples beved:Y Int, corea:

0 to 0

i og re. JErfERSON CITY DOL 0 NITE rm. E 11NENCE DOLOMITC

)l t?lh 5 :

peinarh.:"TLOWING WELL"; 2 LOGS i


Strati giapny Data----------

1; av H 002'*85

- L a t n - -- - --- - - N i n e r a h --- - -- -

liase Nanie f'r S c M n P ri Oc Sec Oc rinr Oc 0

25 NO SAM?LES 0

0 0

1 25 430 ORDOVICIAN SYSTEn 0

0 0

I

'5 430 CAwADIAN SERIES 0

0 0

3 100 JErfECLON CITY DOLOMITE DL Cd LD 0

0 0

!tvo 240 ROUb!D0uA I0dnATION DL CH SS 0

0 0

f?io 430 DASCONADC DOLOMllE DL D SD 0

0 0

0 250 UPJF< GASLOmADE DOLOSITE De CH 0

0 0

0 000 "RICHLA8D DOLONITE P'EMDEk" De CH 0

0 0

' CSO 420 LOWER GALCONADE DOLO?llTE DL CH 0

0 0

0 430 GUNTER SANDSTONE MEh0ER DL CH LD 0

0 0

O 528 CAeDRIAN SYSTEr1 0

0 0

430 526 UN'ER CAMPRI AN SERIES 0

0 0

j '0 SLS EntwCNCE DOL 0mITC De CH 0

0 0

3 528 TOTAL DEPTH 0

0 0

IvintN vi O3/22/97 at 07:46:58.

4

'E t

E E

E o____-


Header Date--------------

i Log M Owner: UNITED NUCLEAR CORP St:MO Cnty: JEFFERSON 1/,993 SW kC SW TRS: 509 T40N ROSE Alias:

Lat.338,12,25.563N Irpe well: Industrial High Capacity Well Lonp. 90,28,39.937W i logs S

Quad:3809004 11er:HAVERSTICK WCLL CD Date

/1956 jr:11er Lisconse N:

Confidential:N Release Dt.

/

r 9er:R.D. KNIGHT Date:09/1956 s v. : 436 Elev.S Yields 125 SWL (a) 13 H2O P
1. D. :

600 base DrDwn:

Y SWLa(b)

TL rot h at:

35 Samplen saved Y Int. coreos 0 to 0

I oa Tm. JErFEl< SON CITY DOLOMITE Fm. EMINENCE DOLOMITE

]

alems:

ocarks
P HEMATITE; FORMERLY NALLINMRODT CHEMICAL C04 WELL ORIGINALLY FLOWED 1

Construet1 on Data----------

g 88 :014993 Date Completed

/1956 i

l

gSING
Dpth:

220 Dian.: S.00 I/0:0 Sr. holes 0.00 St. Below: 0.00 lg 0

0.00 0

0.00 0

0.00 UUT Troe Rap detha Dt hono Piup Date Top lio t t om e

/

/

0 0

jl

!innD:

Ceu Type bet at TDH Sern Typ Stre Lotn Slot 0

0 0

0 0

0 11 Treat Type Dev Typ Comol Perf. Interval Tube Pres. Oil Gas Top 0 Bot 0

on Topt r<0VBIDOUX FORMATION

<,,rma t ions bot:EN1NENCE DOL 0 NITE l0therdatasources:

narks:

I

.--Strai 1 0raoh y bata N 0147)3

' --L i t a - - - - --

-M i ne ra i s ---- - -

Fate Name Pr Se nn Pri Oc Sec Oc Nor Oc O

35 NO SAMPLCS 0

0 0

S 470 OkDOVICIAN SYSTEM 0

0 0

3 470 CANADIAN SERIES 0

0 0

.> D 125 JEFFERSON CITY DOLONITE DL CH SD Zns 1

0 0

05 255 ROUDID00X FORMATION DL SS Cri ZnS 5

0 0

)g5 470 GASCDNADE DOLOMITE DL Ctt SD 0

0 0

lW5 315 UPPER GASCONADE DOLOMITE DL Cti SD ZnS 2

0 0

255 305 "RICHLAND DOLONIT~ nEMBER" DL SD 0

0 0

5 455 LOWER GASCONADE DOL 0 NITE DL CH 0

0 0

5 470 GUNTER LANDSTONE NEn0ER DL CH 5D 0

0 0

i4 0 600 CAMBRIAN SYSTEM 0

0 0

4?O 600 UPPER CAnbRIAN SCRIES 0

0 0

1 0 600 EMINENCE DOLONITE DL Cti ZnS 23 0

0 j

0 600 TOTAL DEPTH 0

0 0

o

Header Data----------

Log #

Owner: HARRISON, GEORGE St:NO Cnty: JEFFERSON NW SW NE TRS: S11 T40N RO5E 6712 Alias:

Lat.:

rpe well: Private Well Long.:

Guad:UtMNOWN

. logs G

5,allerLiscenseW:

.ler:LCOT1, C.H.

Date

/1941 Conficential:N Release Dt.

/

o nerinCCRACKEN Dates

/

_/.

505 Clev.S Yielos 3

SWL (a) 90 H2O es TL

. D. :

130 pase:

DrDwn:

SWLa(o) oen at:

15 Samoles, s,aved: Y Int. cored:

0 to 0

o, Fm. :POWELL DOL 0n!TC Fm. POWELL DOLONITC

>1 ems:

thste HARR150N LAKE, NEAR HEMATITE


Construction Data-Ep--

H 00;712 Date Completed:

/1941 22 Diam: 6.25 I/0:0 Sr. Hole: 0.00 St. Below: 0.00 831ND.Dath:0 0.00 0

0.00 001:

Type Rg ri Dt Aanc i' A u p D.it e T o.)

bottow

/

/

0 0

'IP Cao Type Set at TDH Scan Tyo Site Lpn iia ot Q

0 0

0 0

0 11 Treat Type Dev Typ Comol Perf. Interval Tube Pres. Oil Gas Too:

0 Fot:

0 r'

t Toa:POWCLL DOLOMITE i

en l

rmationb bot:POWELL DOLONITE l Other data r,ources:

Waares:

-Stiata g raoh y Dat a t

i

--L2tn - ------ ~iinerais---- ----

rH 006712 Pr Se nn Pri De Sec Oc Mar Oc I

Dat,e Name 0

0 0

0 15 NO SAMPLES O

O O

JS 130 ORDOVICIAN SYSTEM 0

0 0

(

3 130 CANADIAN SERIES y5 130 POUELL DOLOMITC Dt Cri SD 0

0 0

0 0

0 130 130 TOTAL DEPTH lI t

05/22/97 at 07:47:26.

4 nted on 1-lp-Q l

F-


H eader Data------

Log H Owner: PRICE. HOMER V.

Stano Cnty:JER CRSON r*W kW SE TRS: S11 T40N ROSE 820309Alias:

Lat. 39,20, 5.?3SN ype well: Private Well 1ong.394,38,55.806W S

Quad 3?O94C6 delogs llvt:LCOTT DRLG CD Date:05/1961 tiller Lascense N Confidential:N Reicase Dt.

/

gerth.n. GROVES Dates

/

v.

O Clev.S fielo 12 SWL (a)150 H20 8:

.L.:

355 aase DrDwn:

5WL (r;)

TL M_

)

g r occk at: 225 painoles saved:Y I nt. cored:

0 to 0

io) fm. JCJ CRSON CITY DOLONITE fin. ROUBIDOUX FORMATION 8tilemst vmaths:3 MI E Of HEMA'/ITE; OLD WELL DEEPENED; LOCATION OVESTIONABLE

- -- -- -- - - -Construetion Data-------

.p J:020309 Date Coenoleted:05/1961 SINO: Dath:

21 Di a tu 6.25 I/0:0 Gr. hole: 0.00 Sz. Below: 6.00 0

0.00 0

0.00 0

0. 00 E..001:

Type T,2 ti

,9 e u r Dt iwou Plue Date Toa Dottom

/

/

0 0

EllE nP Cao Tyae Set et TDu bc rn (yo Stre Lyth Slot 0

0 0

0 0

0 11 Treat lyoe Dev Typ Cowal perf. Interval Tuoe Pres. 011 Gas Toa:

0 Lut:

0 en Toa:JE TCkSON CITY Dfh.0MITC ll srmations bar:ROUltIDDUX f0RnAT10N lOther oata sources:

r,io r u :

9 t r at i o r aotiy Data--

I H:000309

- -t i t n -


ninerais---

1 P r St. an Pri Oc Sec Oc Nor Oc i D a t.e ame I

0 225 80 S W LES 0

0 0

"'S t.>5 06DDV1CIArs SYSTEM 0

0 0

0 0

0 E.J5

'5 355 CLADIM SERIES 290 JErfEh50N CITY DOLOMITE DL CH SD 0

0 0

i 290 355 RCJDIDOUK FORMATION Du CH SS 0

0 0

5 355 TOTAL DEPTH 0

0 0

canteo on 05/02/97 at O'7:47:31.

'E a

.... Header Data--------------

, tog H Owner:LONG, HARRY StahD Cnty:JEFFERbON l

}

05678 SE FW NW TRS: 516 T404 ROSE l

Altas Lat.:

.yve well: Private Well Long.:

[

S Quad:UNKN04n 8elog 11erabCOTT, C.N.

Dates /1939 l

rtiler Liscease H Confidential
N Reicane Dt.

/

lr gerinCCRACKEN Date:10/1939

v. : 440 Elev.S Yiulos 6

GWL (a) 18 1100 es

. D.

67 Dase DrDwn:

GWL (a)

TL roer. att 25 Samoles saveo N Int. cored:

0 to 0

102 Fm. JCFFERSON CITY D0LONITC Fm.: JEFFERSON CITY DOLOMITE 1

alems:

.< marks:C SD OR RR TCK e liEMATITC DEkIND LONG'S STORE; BTWH CK AND RR TRACK 0.sg ---------c""

    • "c'*

H 005678 Date Completed:

/1939 Doth:

25 Diam: 6.25 I/0:0 Gr. hole: 0.00 Gr. Below 0.00 ESING:

0 0.00 0

0.00 0

0.00 E

.m0UT:

1"ce Rig ret hri Dt Anna Plug Date Too bottom

/

/

0 0

  • P Ceo Troe bet at 1DH Sern Tyo Lire Lpth Slot 0

0 0

0 0

0 11 Tient Type Dev Typ Comol Perf. Interval Tube Pret. 011 Das Too:

0 bot O

en Too:JEFFLaA4 CITY DOL 0 MITE tmationu Itot:JEFFU64h CITY DOLOMITC Other data sourcer:

Emarcs:

- - St r a ti praoh y Data----------

--L a i n -- --- --- --- h t n e r a i s ---- - -- --

EM005678 habe Name Pr Se Mn Pil Oc Sec Oc Mnr De 0

25 NO SAMPLES 0

0 0

5 67 ORDOVICIAN SYSTEN O

O O

5 67 CANADIAN SERIES 0

0 0

b 67 JEFFERSON CITY DOL 0aITE DL Cet SD 0

0 0

6'l 67 TOTAL DEPTH 0

0 0

uted on 05/22/97 at 07:52:28.

E E

5


Header Data Lug 16 Owne r tliOUNK, E. It.

Steno Cnty: JEFFERSON WiSL72 SE SW NE TRS: S16 140N ROSE Altas Lat.:

ype well: Private Well Long.:

. logs G

Guad:UNKHOWN Aler: SCOTT, C.N.

Date

/1939

. aller Lascense it

'onfidential:N Re* ease Dt.

/

A gerinCCRACKEN Date:10/1939

/. : 480 Elev.G Yield 0.5 SWLa(a) 35 H2O 3:

. D. :

70 base:

DrDwns SWLa(n)

TL

och at:

20 Samoles s.aved:N Int. t o t et;:

0 to 0

o) Tru. JEffECON CITY DOLO 31TE fm.:80Vb!DOUX FORelATION ilems:

. marks 0.0 MI E Or HEMATITE


Cont, tt uetion Data----------

9 H:005672 Date Completed: /1939

';I NG : Dutna 6 Diam: 6.2S 1/0:0 Dr. Hole: 0.00 Sr. below: 0.00 0

0.00 0

0.00 0

0.00

.n001:

Troe Ran fietne DL A snc; Pluo Date Top bottoru

/

/

0 0

1P Can Tyne Det at T'A Sern Typ SAre atn Slot 0

0 0

0 0

0 11 Treat Tyoe Dev Tyo Comol Perf. Interval Tuoe Pret;. Oil

Gat, Toat 0 Dut:

0 on Top:JCFIERS0ri CITY DOLOMIT-t en a t io n s DotskOUDIDOUX FORrtATION iltner data Sources hartiL

._.-Strat2 y r a o ti y Data---- --- - - -

H 00T672

- -L a On -- -

- -- --m i ne r a i s --- -- -- -

base Name Pr Sc Mn Pr1 Oc Sec Oc nnt Oc 0

20 NO san?LES 0

0 0

0 70 ORDOVICIAN SYSTEN O

O O

O

/0 CANADIAN SC3IES 0

0 0

_0 60 JEFFCRSON CITY DDL0ri1TC DL Ce SD 0

0 0

60 70 ROUBIDOUX FORMATION DL CH SD 0

0 0

0 70 TOTAL DEPTH 0

0 0

. anted on 05/22/97 at 07:S2:36.


Header Data--------------

Gog H Owner: WILLIAMS, SILAS Staho Cnty: JEFFERSON 05673 SJ W NW TRS: S16 T40N ROSE Alias:

Lat.:

liyne wall: Private Well Lonp.:

'e logs S Quaa: UNKNOWN 11er: SCOTT, C. N.

Dates

/1939 iller Liseense H:

Confidential:N Release Dt.

/

X.ger:NCCRACKEN Date:10/1939 I

ev.: 472 Clev.S Yields 6

SWL (a)

H2O 0:60', 90' i S. :

95 base:

Dr0wn SWL (b)

TL toch at:

17 Samoles saved:H Int. corea 0 to 0

iao Fa. JEFFERSON CITY DOLOITE h ra.. JEfrCRSON CITY DOLONITC ibicas marks "CAN'T FAIL DRY", () hCNATITE ONE btK W Of RR TAAC4 ON SCHOOL HOUbi "'


Const ruet1 on Data----------

.oc N 005673 Date Completed:

/1939 iSING: Doth:

25 Diam 6.25 I/0:0 Sr. Hole: 0.00 Gr. Below: 0.00 0

0.00 0

0.00 0

0.00 4:0u1:

Type A10 ne t a t, Dt Aand Piup Date Too bo t t oru

/

/

0 0

'UNP:

Cao Tyue Set at Tlni Sern Tya Sire ph Sat 0

0 0

0 0

0 s11 Treat Type Dev Tyo Comol Perf. Interval Tutie Prec. Oil Gas Too:

0 Butt 0

een Top JEFfLRSON CITY DOLO M TC

'ormations bot: JEFFERSON CITf DOL 0 NITE Mner data sources.:

tmarns:

-. - ---Str at A n r aaay Da ta

i it:005673

--L i t n - - -----h t ne r a i n----

a Doce Haste Pr Se nn Pri Oc Sec Oc nnr Oc 0

17 NO sat'WLES 0

0 0

1,7 70 ORDOVICIAN SYSTCn 0

0 0

.7 70 CANADIAN SERIES 0

0 0

17 70 JEFFERSON CITY DOLONITE D Cd SD 0

0 0

470 95 NO SAMPLES 0

0 0

15 95 TOTAi DEPTH 0

0 0

rinted on 05/22/97 at 07:52:42.

1-------------Heaoer Data--------------

Log N Owner:STIS (STIO?), RICHARD Stan0 Cncy: JEFFERSON

  • 10248 SW kW kW TRS: S16 T40N RO5E Altas:

Lat.:38,1d, 6.413N eype well: Private Well Long.390,28,44.539W tv ! log S

Quad:38090B4

.llerablDOMSDALE EXCAVATION CODate:05/1957 aller Liscense N:

Confidential:N Re19ase Dt.

/

of,ger R.D. KNIGHT Date:07/1957 v.: 400 Elev.S Yield 10 SWL:(a) 55 H2O 0:120-132' I.D.:

140 base:

DrDwn:

SW :(c)

TL

{

crock at:

15 Samoles saved:Y Int, corea:

0 to 0

. p Fm.: COTTER DOLOMI(E Ord fs. COTTER DOLOMITE diems:

M marks:

l

.-----------Construetion Deta------

eg N 016248 Date Completed:05/1957 l

r!SIhG: Dotn 35 D:am: 6.00 1/0:0 Sr. Hole: 0.00 Sr. Below: 0.00 0

0.00 0

0.00 0

0.00 OUT:

Type Rip octau Dt 00nc Plug Date Too Bottoni

/

/

0 0

i t.P :

Euo Type Get at TDH Scrn Tyo Size L9th Slot 0

0 0

0 0

0 11 Treat Type Dev Typ Comol Perf. Interval Tube Pres. 011 Gas Toa:

0 Bot:

0 sen Too: COTTER DOL 0kII K m!Urmations Bot: COTTER DOL 0aITE Otner data sources:

imarks:

--Stra L1 e ea ony Data-H:01ca4S

-- - t 2 t a - -


Minerais---------

.s

, Dase Name Pr Sc Mn Pri Oc Sec Oc rint Oc 0

15 RESIDUUM & TOP SOIL CL Cn 0

0 0

15 140 ORDOVICION SYSTEN 0

0 0

S 140 C&ADIAN SEF.I"S 0

0 0

.5 140 COTTER DOLOMITE De Cri SD Zns 1

0 0

110 125 80 SAi1PLES O

O O

O 140 TOTAL DEPTH 0

0 0

rinted on 05/d2/97 at 07:52:4S.

W 6

.--...--------Header.

Data--------------

Liog H Owner:NOSCR, HARRY Stan0 Cnty: JEFFERSON f12875 SE NW SE Ti,S: S16 T40N ROSE Alies:

Lat.338,11,38.063N ype well:*+1vate Well Long.90,08,10.284W e logs S Quaos38090B4 aller:HAVEASTICK L. ELL CD Dates

/1954 iller Liscense Na Confloential:N Release Dr.

/

.qger: LEWIS AND CLARK Date:09/1954 ev.: 476 Elev.S Ytelas i

SWLi(a) 30 H00 en Tu?.

140 oase:

DrDwn: 100 SWL: ( b)

TL d r oc6: at:

5 Samoles naved:Y Int. corea:

0 tc 0

soo Fm.200TTER DOLOMITE i : Fm.: JEFFERSON CITY DOLONITC abiems:

mai 6;s s Wo.-----------Construetion Data----

g H:012875 Date Completed

/1954 9 SING: Data:

15 Diam: 0.00 1/0:0 Sr. Hole: 0.00 $2. Delow: 0.00 0

0.00 0

0.00 0

0.00 j

001:

Tyoc hu nethe Dt Aano Plug Date Too Bottom

/

/

0 0

vaP:

Cas Type Set at IDo Sern Tyo Size

.g tn Slot 0

0 0

0 0

0 ell Treat Troe Lev Typ Comol Perf. Interval Tube Pres. 011 Gas Toa.

O Dot O

pen Toa: COTTER DOL 0dITE ormations Dot: JEFFERSON CITY DOLOMITE trae r caue sources:

tim a rk t. :

= -


Stcati prap ny Dat H:012875

--LitV - ------- Minerais----------

Wa) base Name Pr Se nn Pri Oc See Oc nnt Oc 0

5 NO GAMPLES 0

0 0

?5 140 0'<DOVICIAN SYSTCM 0

0 0

15 140 CA8ADIAN SERIES 0

0 0

5 45 COTTER DOLONITC Du CH SD Zns 1

0 0

d5 140 JI;FCQSON CITY DOL 0 NITE DL CH SD Zns 1 Pos 1

0 60 140 TOTAL DEPTH 0

0 0

,rinteu on 05/02/97 at 07:52:54, t

t W

....-..geae,7 3,ga.

Log it Owner:HENNE, OTTO St no Cnty: JEFFERSON-12876 C NW SE TRS: 516 T40N ROSE Alias:

Lat.:38,11,41.485.4 ype well Private Well Long. 90,28,13.046W 3 log:

S Quad 38090B4 ler:HAVERSTICK WELL CD Date

/1954

,.'ller Liscense its Confidential:N Release Dt.

/

.o.ger: LEWIS C. PARTIN Date:09/1954

V.
470 Elev.S Yiein 12 SWLa(a) 30 h20 Os
i. D. :

195 Dase DrDwn:

60 SWL:(c)

TL rocn at:

5 Samoles saved:Y Int. corect 0 to 0

.oa Fm. COTTER DOL 0 MITE ir Fm.*ROUBIDOUX FORr1ATION alems:

. arks LENAY W(g-64:


Construet1 on Data----------

012876 Date Comoletea:

/1954 SING: Dotna O Diam: 0.00 I/0:0 Sr. hole: 0.00 Sz. Below: 0.00 0

0.00 0

0.00 0

0.00 OUT:

Type Rap Metnc Dt Aanc Plup Date Too Do t tora

/

/

0 0

MP:

Cao Type Set at TDn Sern Typ 512e

_gtn 5 ot 0

0 0

0 0

0 11 Treat Type Dev Typ Comol Perf. Interval Tuoc Pret;. 011 Gas Top:

0 Dot:

0 en Too: COTTER DOLOMITC rmations Bot:ROUDIDOUX FORMATION Otner cata sources:

marns:

-Strat ipraony Da ta-11 :012376

--Litn-- ---------Minerais---------

base Name Pr Se nn Pri De Sec Oc Nnt Oc 0

'S NO SAMPLCS S

0 0

5 195:0RDOVICIAN SYSTEM 0

0 0

5 19'.i CANADI AN SERICG 0

0 0

5

.35 COTTER DOLOMITC DL SD CH 0

0 0

33 17S JEFFERSON CITY DOL 0 NITE Dt CH SD Zns 1

0 0

5 195 ROUDIDOUX F6RMATION DL CH SD 0

0 0

5 195 TOTAL DCPTH 0

0 0

nted on 05/22/97 at 07:53:00.

l l

- - - - - - - - - - - - - H ** a d e r Data--------------

l u g 41 Owner: SMITH, DALE Stan0 Cr.ty: JEFFERSON

'18152 SE NE SW TRS: S17 T40m ROSE

't Alias:

Lat.238,11,45.452N yee well: Private Well Long.90,29,58.420W

% e log: S Quad:38090B4 11er:HAVERSTICK WELL CO Dater

/

iller Lascense H:

Confidential:H Release Dt.

/

.cgger:J. WELLS Date:07/1959 ov. : 452 Elev.S Yield:

.8 SWL a (a) 20 h20 2:

T.%

100 case:

DrDwn:

SWL : ( b)

TL roen at:

30 Samples i,aved:Y Int. coreo:

0 to 0

i io) Fm. JEFFERSON CITY LOLOGITE lI I'.Fm.s.1EFFERSON CITY DDLONITE 1e nemu.

ma r e.s :

i


Construet1 on Data--

oo H 016152 Date Completea: /

' 111 Wit Datn:

0 Diam: 0.00 I/0:0 Sz. Hole: 0.00 Sr. Below: 0.00 0

0.00 i

0 0.00 O

0.00 OvT:

Type R:p detnn Dr Aona Plup Date Too bottom j

0 o

i s.? :

Cao Type Get at T Del Sc rn Tyt>

Lire L e t ti Sloc 0

0 0

0 0

0 11 Treat Tyne Dev Tyo Comol Perf. Interval Tube Pres. 0:1 Gas Too:

0 Dot:

0 4

ea Too: JEFFERSON CITY DOLOCTE ormations Lot:JEriERSON CITY D0'.0MTE j

Cm er data sources:

l n a rts:


Strati uraony Data---

H:0181"d

-L i tn -- -- ----- - -m i n e r a i s------

Dane Name Pr Se en Pri Oc Sec Oc fint De 0

30 NO SAnPLES C

0 0

2 0 100 ORD0VICIM SYSTEn 0

0 0

'O 100 CANADIM SERIES o

0 0

,30 100 JEFFERSON CITY DOLOMITE Du Cet ZnS 1

0 0

i ISO 100 10TAL DEPTH 0

0 0

nted on 05/22/97 at 07:53: 16.

t 4

-- - -. - - n earer Da a

i

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Cons truetion Data----

iPu H:022355 Date Coraoletec:07/1963 D at :

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---+----Heaoer Data-- -

d tog M Owner:PROPST, EZM St:+0 Cnty:114CRGGs 22420 SW hE Sw Tis 522 T404 R052 j

Olias:

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Cor f acentrai N ielease Dr.

/

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LCOTT DRLG C0 Date:03/1963 11er L:scento h:

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g 4:022420 Date Comoieted:03/1963

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is, APPENDIX B l jf MDNR Well Log # 14993 i.

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r#R-10-1P/7 12:35 t10 DtR/DCLS D o.:oo 4111 F.u4 e

- _ - - _ _._ - _ _ - - - - H o a d a r Data--------------

_a

~~9 Log i Owner: UNITED NUCLEAR CORP St:MO Cnty JEFFERSON SW NE SW TRS: S09 T40N ROSE d

014993 Lat.138,12,25.563N Alias:

Type wellilndustrial High Capacity Well Long.: 90,28,39.937W Quad:38090B4

,.l Type 109:

S d

Driller:HAVERSTICK WELL CO f>ato

/1956 Confidentiel:N Release Dt.

/

Driller Liscense #:

Logger:R.D. KNIGHT Date:09/1956 Elev.: 436 Elev.S Yield:

125 SWLa(a) 13 H2O 9:

T.D.:

600 base:

DrDwn:

Y SWLi(b)

TL Bedrock at:

35 Samples saved:Y Int. cored:

0 to O

Top Fm. JEFFERSON CITY DOLOHITE E

Bot Fm.: EMINENCE DOLOMITE Problems:

Remarks:@ HEMATITE; FORMERLY MALLINKRODT CHEMICAL CO; WELL ORIGINALLY FLOWED

---Construction Data----------

Log i 014993 Date Completed:

/1956 CASING: Dpth:

220 Diam: 8.00 I/O:0 Sz. Hole: 0.00 Sz. Below: 0.00 0

0.00 0

0.00 0

0.00 GROUT:

Typo Rig Methd Dt Abnd Plug Dato Top Bottom

/

/

0 0

PUMP:

Cap.

Type Set at TDH Scrn Typ Size Lgth Slot 0

0 0

0 0

0 Well Troat Type Dev Typ Compl Perf. Interval Tube Pros. Oil Gas Tops O Bot:

0 Open Top:ROUBIDOUX FORMATION Formations Bot: EMINENCE DOLOMITE Other data sourcoot Remarks:


Strat1 graphy Data

-Lith-- ---------Minerals---------

Log 4:014993 Pr Sc Mn Pri Oc Soc Oc Mnr Oc Top Base Name 0

0 0

0 35 NO SAMPLES 0

0 0

35 470 ORDOVICIAN SYSTEM 0

0 0

35 470 CANADIAN SERIES 35 125 JEFFERSON CITY DOLOMITE DL CH Sc.'nS 1

0 0

M 125 255 ROUBIDOUX FORMATION DL SS CM ZnS 5

0 0

255 470 GASCONADE DOLOMITE DL CH SD 0

0 0

315 UPPER GASCONADE DOLOMITE DL CH SD znS 2

0 0

M 255 305 "RICHLAND DOLOMITE MEMBER" DL SD 0

0 0

255 315 ~455 LOWER GASCONADE DOLOMITE DL CH 0

0 0

455 470 GUNTER SANDSTONE MEMBER DL CH SD 0

0 0

0 0

0 470 600 CAMBRIAN SYSTEM 0

0 0

1'*~

470 600 UPPER CAMBRIAN SERIES 470 600 EMINENCE DOLOMITE DL CH ZnS 23 0

0 0

0 0

600 600 TOTAL DEPTH W

WM-10-1W/

12:33 t10 DtF./DGLS 573 360 2111 P 03/05 4.M.c,p;ic.Qi

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