114

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NEW MEXICO
BUREAU OF MINES
&
MINERAL
RESOURCES
Open-File Report 114
DESCRIPTION OF CUTTINGS
NAVAJO
WATER
WELLS
FROM
IN
NEW MEXICO--1978
&
William 3 . Stone, Hydrogeologist
Randall E. Jackson, Field Geologist
March 1980
1979
Contents
.........................................
Using This Report ....................................
Explanation of Descriptions ..........................
References Cited
....................................
Descriptions of Cuttings .............................
Introduction
1
1
3
7
9-23
Illustrations
Figure 1
Table 1
.
.
Appendix
Catalog
.
.............................
2
of cuttings described .............. 8
symbols and terms .................. 24
Reference map
Key to
1
INTRODUCTION
1 9 7 6 aninformalagreement
InJune
was made w i t h t h e
Water Works DepartmentoftheNavajoTribe
(now Technicaland
E n g i n e e r i n g Services) whereby c u t t i n g s f r o m T r i b a l
wells d r i l l e d i n New llexico would be turned over
water
t o t h e New
Mexico Bureau of Mines and M i n e r a l R e s o u r c e s f o r c a t a l o g i n g
andpermanent
filingintheir
I t was f u r t h e r
s a m p l el i b r a r y .
agreedthatcopies
ofanydescriptions
wouldbefurnished
t o t h eT r i b e .T h i sa g r e e m e n t
beneficialbecause,althoughcuttings
made o f t h e s a m p l e s
i s mutually
are u s u a l l y c o l l e c t e d
from T r i b a l wells a n d d e s c r i b e d i n t h e f i e l d , s a m p l e s
always f u r t h e rs t u d i e d
or p e r m a n e n t l yf i l e d .
presentagreementnotonly
are not
Under t h e
may t h e T r i b e a n d t h e B u r e a u
wells b u t
routinely obtain detailed stratigraphic records for
t h es a m p l e s
will b e p r e s e r v e d f o r f u t u r e u s e t h r o u g h s t o r a g e
i n anestablishedcuttingslibrary.
USSNG THTS REPORT
Only
c u t t i n g sr e c e i v e db e t w e e nJ a n u a r y
~ 1 9 7 8and
1 9 8 0 are described i n t h i s r e p o r t ; o t h e r s a m p l e s
1 ( p - 8 ) l i s t s wells f o r
by S t o n ea n do t h e r s( 1 9 7 8 )T a b l e
w h i c hs a m p l ed e s c r i p t i o n s
A f f a i r s )f i e l d
number.
and a l e t t e r : 14T-569.
BXA D i s t r i c t ( f i g . l a ) .
are given by B I A (BureauofIndian
T h i s number c o n s i s t so f
2 numerals
The f i r s t n u m e r a li d e n t i f i e st h e
The l e t t e r , s i n c ea b o u t1 9 5 0 ,
denotes t h e s o u r c e o f f u n d s u s e d
Common d e s i g n a t i o n s are:
were d e s c r i b e d
to construct the
K = BTA fundsand
T =
well.
. . ..
. .
2
1'
. .
. .
.
.
,.
..
,
.
. .
.Explanation
81A 15' quad.rangle no.
"-. -. -'81A district bdy.
---.Res.etvation
IO"
I.:
-
0 . .
ID
line
+.fn!ion
.rbad'
.
.
.
.
.
.
highway
.Reference map f o r n o r t h w e s t e r n New Mexicoandkey
to n m b e r i n g of Navajo water w e l l s : a) l ' o c a t i o n of'
BIA d i s t r i c at sn d
1 5 ' q u a d r m g l ae s s o c i a t e d
with
. . New. Mexicu . p o r t i o n of N a v a j oI n d i a nR e s e r v a t i o n ;
b) d e r i v a t i o n of BIA . q u a d r a nlgolcea tni ounm b e r s
f o r weils (example showri h a s f i e l d number of
'.LT - 2 2 9 ' a n d q u a d r a n g l e lacation number of
'.
.
'
20
3Om1
c_(.
F i g u r e 1.
.
:: .
bdy.
--"--$~ots
+'US.
.
'
27-3-5.0-15-8.0)
.
.
3
Tribal funds. The significance of other letter designations
used is less clear. The third part is an accession number
for
that
district,
representing
the
order
in
which
the
wells
are drilled. Tn addition to the well number, the townshiprange location, total well depth, sampled interval, probable
aquifer, and pages covered by the description are also given.
Table 1 may be used in 2 ways:
1) to determine the
availability of sample descriptions for a specific well
of
interest and 2 ) to determine the identity
of
wells
for
which
there are samplesor sample descriptions in a general area
of interest. Tn the first case, look for the well in Table
1 using the BTA field number. If it is listed, a sample
description is included in this report and cuttings
on are
file in the Bureau. In the second case, consult Table
1
for the area of interest using county, township-range, or
B1.A district number (fig.1).
Samples and sample descriptions
axe available for all wells listed.
EXPZANATLON OF DESCRIPTIONS
The
descriptions
which
follow
were
made
by
conventional
study o f the cuttings with a binocular microscope. Abundance
and
textural
characteristics
are
based
on
visual
estimates
following Terry and Chilingar(1958) and Powers (1953).
All qbbreviations used are defined in the to
"Key
Symbols and
Terms!' (p. 24).
Each description includes the following
heading informa.tion: well number, location, sampled interval,
total depth (TD)
, name of analys.t, and date of
4
The well number g i v e n i s g e n e r a l l yt h e
description.
BIA f i e l d
number.
Where p o s s i b l e , l o c a t i o n
i s g i v e na c c o r d i n g
to:
1) s t a n d a r dl e g a ld e s c r i p t i o n( s e c t i o n ,t o w n s h i p ,r a n g e ,
was e x t e n d e d i n t o t h e r e s e r v a t i o n
c o u n t y ;f o rt h i st h el a n dg r i d
f r o ma d j a c e n t
a r e a s ) , 2 ) d i , s t a n c ea n dd i r e c t i o nf r o m
landmark,and
3 ) l o c a t i o nw i t h i n
q u a d r a n g l el o c a t i o n
27-3.50-15.80).
BIA quadrangle.
number c o n s i s t s o f
a local
The B I A
3 parts(for
example
The f i r s t p a r t i s t h e number o f t h e BIA
q u a d r a n g l e i n which t h e well i s l o c a t e d ( f i g .
is the distance in
l a ) . The second
miles west
- of the northeast corner of the
quadrangle,andthethirdpart
is thedistancein
miles s o u t h
of t h e . n o r t h e a s t c o r n e r o f t h e q u a d r a n g l e ( f i g . l b ) .
Wells are a r r a n g e d by B I A f i e l d number as i n T a b l e 1.
D e s c r i p t i o n s are p r e s e n t e d i n t h e o r d e r t h a t t h e
materials
were e n c o u n t e r e d i n d r i l l i n g a n d d e p t h s o f i n t e r v a l s
d e s c r i b e dt h e r e f o r ei n c r e a s e
down t h ep a g e .
s t r a t i g r a p h i cu n i t s( f o r m a t i o n s ,g r o u p s ,
The p r o b a b l e
etc.) penetrated
by t h e well are i n d i c a t e d by t h e a b b r e v i a t i o n s i n t h e
Depthcolumn
at the.left.
The term i n c a p s a t t h e b e g i n n i n g
ofeachdescriptiveentryidentifiestheprobablemajorrock
o rs e d i m e n tt y p e ( s )i nt h ei n t e r v a li n d i c a t e d ,b a s e d
e x a m i n a t i o no ft h ec u t t i n g s .
A s i n g l el i t h o l o g i c
on
term i s
l i s t e d where it i s deemed t o c o n s t i t u t e >50 p e r c e n t o f t h e
t o t a l sample,
Two l i t h o l o g i c terms j o i n e d by "and" are l i s t e d
5
wher.e.
each
constitutes
30-50
percent
of
the
total
sample.
Other abundance terms used are defined
in the Appendix (p. 24).
I
The specific descriptive information given after the
general lithologic term(s) varies slightly with rock types;
for clarity, this information
is always presented in the same
order as follows:
SANDSTONES -- color; texture (grain size, grain
sorting, grain shape); mineralogy; matrix, cement,
induration; miscellaneous constituents or
characteristics.
CLAYEY OR SILTY SANDSTONES -- color; texture (of
sand); general commenton clay or silt; mineralogy;
matrix, cement, induration; miscellaneous constituents or characteristics.
OR SILTSTONE -- color; general
SHALE, SILTY SHALE,
comment on silt or sand (if pr,esent); cement,
induration; miscellaneous constituents
or characteristics.
SANDY SILTSTONE OR SANDY SHALE
-- color; texture of
sand grains; mineralogy.of sand grains; cement,
indur,ati.on; miscellaneous constituents or
characteristics.
The rock color chart prepared by Goddard and others
(1948)
and distributed by the Geological Society of America (GSA) was
used for rock color des2gnations. In several~casesidentical
names are givenon the chart for two sightly different colors
such
that
name
alone
cannot
be
used
without
creating
doubt
to the color intended. Three cases of such duplicate color
designations
report:
were
encountered
in
samples
covered
by
this
, and "moderate red".
"light brown", "yellowish gray"
As used here these terms refer to colors 5YR6/4,
5Y7/2, and
5R4/6 on the chart, respectively. All other color designations
e
follow
the
GSA
chart
exactly.
as
6
The
example
200-230
This
below
should
aid
in
using
the
descriptions:
SANDSTONE AND SILTSTONE--ss
wh; grains f to
qtz;.
m, mod w sorted, subang, spher; milky
clay and slt mat, tr silica cem, fri. Sltst
It gry;w ind; carb. Tr sh aa.
description
covers
material
from
an
interval
lying
between
200 and 230 feet below the surface. The interval
is concluded
to
consist
of
nearly
equal
amounts
sandstone
(each constituting30-50 percent of the sample).
and
siltstone
The sandstone
is white, moderately well sorted, with subangular spherical
grains
of
milky
quartz
in
the
fine
to size
mediumrange
It is also friable (crumbly) with only a
(0.125-0.5mm).
trace of silica
cement
between
the
grains
but anhas
inter-
granular matrix consistingof clay and silt. The siltstone
is light
gray,
cemented
by undetermined material, well indurated
(hardened), and contains carbonaceous material. Thereis also
a trace of shale as described above.
The
designations
are
basedon
sample
of
selected
units
of
probable
lithology
in
and
northwestern
Stone and Mizell (1978).
stratigraphic
Bureau
New
maps
Mexico
units
of
penetrated
depth-to-top
prepared
by
7
REFERENCES CITED
Goddard, E. N., Trask, P. D., De Ford, R. K., Rove, 0. N.,
Singewald, J. T., Jr., and Overbeck, R. M., 1948, Rock
Color Chart: Distributed by the Geological
Society.of
America, Boulder, Co. (reprinted 1970).
Powers, M. C., 1953, A new roundness scale for sedimentary
particles: Journal Sedimentary Petrology, v. 23, p. 117-119.
Stone,
W.
J., Brod, R. C., and Anderholm, S. K., 1978,
Descriptions of cuttings
Mexico"1977:
from
Navajo
water
wells
in
New Mexico Bureauof Mines and Mineral
Resources, Open-File Report82, 81 p.
Stone, W. J., and Mizell, N. H., 1978, Basic subsurface data
compiled
for
hydrogeologic
of the
study
San
Juan
Basin,
northwest New Mexico: New Mexico Bureau of Mines and
41 p.
Mineral Resources, Open-File Report 89,
Terry, R. D., and Chilingar, G. V., 1958, Comparison charts
for
visual
estimation
of
percentage
composition:
American Geological Institute Data Sheet, 6,
AGI
Geotimes (April).
New
Table 1.
Catalog of c u t t i n g s from Navajo water wells i n New Mexico described i n 1 9 7 9 .
. .
Well No.
(BIA F i e l d No)
. . .
.
.
.
'.. . .
Location
. .
. . .
. .
T.D.
D e s cPrri op bt iS
aobanlme p l e d
(ft)
Interval
% S e c , Twp, Rge
.
.
Aquifer ( s )
'
(Pages)
12T-618
(Newcomb S c h o o l )
SE, 25, 24N, 18W
(San Juan C o u n t y )
16T-594
( S m i t h Lake #1)
500-1560
2024
1 7 , 15N, 12W
(McKinley C o u n t y )
J m , Je
12-14
16T-595
NE27/NW26, 16N, 14W
(McKinleyCounty)
1640
350-1600
Jm,
Je
15-16
(Mariano Lake #1)
16T-596
(MarianoLake
3 3 ( ? ) , 16N, 14W
(McKinley County)
1 6 10
J m , Je
17-20
J m , Je
21-23
16T-597
( S m i t hL a k e
#2)
#2)
1 4 4.0
1 7 , 15N, 12W
0-1939
1939
(McKinley County)
0-1440
150-1610
Kmf
9-11
W
9
Well no: 12T-618 (Newcomb #1)
Location: Sec. 25, T24N, R18W,San Juan Co., N.M.;
100 ft. N of School; 49-11.65-14.70.
Sampled interval: 0-1440
TD:1440
ft
ft
Described by: R.' Jackson
(12/79)
Depth (ft)
0-10
SOIL/ALLUVIUM (Quaternary)
Kmf
-
0
e
10-20
SILTY
20-30
SHALE AND.SANDSTONE--Shaa. S s It gry; grains
f, p sorted, srd; qtz calc cem ind.
30-80
SANDY SILTSTONE--m gry; sand grains f, p sorted,
subang; qtz; calc cem, ind.
80-90
SILTY
SHALE--m
90-100
SANDY
SILTSTONE--aa.
SHALE--m
gry
gry.
100-110
SANDSTONE--1t gry; grains f-crse, p sorted, ang;
qtz; calc cem,ind.
110-160
SANDSTONE
160-180
SHALE--m
180-200
SANDY SILTSTONE--aa.
200-210
SANDSTONE
210--240
SILTSTONE--nun
240-250
SANDY SILTSTONE--m gry; grains
f-m.; p sorted, subang;
qtz and mica; fri.
250-260
SILTSTONE--aa.
260-270
SANDSTONE
270-280
SILTSTONE--m gry, calc cem.
280-320
SANDSTONE AND SILTSTONE--SSIt gry; grains
p sorted, subang; qtz; ind, Sltst m gry.
320-330
SANDSTONE--1t gry; grains f-crse, p sorted, ang;
qtz; fri.
AND
SANDY
SILTSTONE--aa.
gry.
AND
AND
SANDY
SILTSTONE--aa.
gry.
SANDY
SILTSTONE--aa.
f-m,
10
0
Newcomb #1 continued
Depth
(ft)
330-350
SANDSTONE
350-370
SANDSTONE--1t gry; grains vf, p sorted, srd;
qtz; calc cem, fri.
370-510
SANDSTONE AND SILTSTONE--ss aa. Sltst m gry.
510-530
SILTSTONE--m
530-550
SANDSTONEASILTSTONE--aa.
550-560
SILTSTONE--aa.
560-570
SANDSTONE AND SILTSTONE--aa.
570-600
Missing
600-610
SANDSTONE AND SILTSTONE--aa.
610-630
Missing
SANDSTONE
AND
SILTSTONE--aa.
gry.
AND
SILTSTONE--aa.
SANDSTONE--V It gry; grains f-m, p sorted, srd;
qtz; calc cem, ind.
800-830
SANDSTONE
8 30-840
SANDSTONE--1t gry; grainsf, p sorted, subang;
qtz; calc cem, ind.
840-850
SANDSTONE
850-860
SILTY
860-1150
SANDSTONE ANDSILTSTONE--SS It gry; grains f ,
m gry.
p sorted, srd;qtz; ind. Sltst
1150-1160
SANDSTONE--aa, It gry and ye1 gry.
1160-1170
SANDSTONE AND SILTY SHALE--1t gry; grains m-crse;
p sorted, ang; qtz; calc cem, ind. Shm gry.
1170-1200
AND
AND
SHALE--m
SILTSTONE--aa.
SILTSTONE--aa.
gry.
SANDSTONE AND SILTSTONE--ssIt gry; grains
m- vcrse, p sorted, srd; qtz; ind. Sltst m gry.
11
Newcomb #1 continued
Depth
(ft)
1200-1210 SANDSTONE AND SILTY SHALE--sS
It gry, grains f-m,
p sorted, srd; qtz; ind.
Silty sh m gry.
~
1210-1220 SILTSTONE AND SHALE--Sltst m gry; calc cem; mica.
Shale m gry.
1220-1300 SANDSTONE AND SILTSTONE--SS
It gry; grains f, p
sorted, subang; qtz, biotite; ind. Sltst m gry.
1300-1330 SANDSTONE--1t gry; grainsf, p sorted, subang;
qtz; calc cem, ind.
1330-1440 SANDSTONE AND SILTSTONE--ss
It gry; grains f, p
sorted, subang; qtz;calc cem, ind. Sltst pk-m gry.
12
-
Well N o :
#l)
1 6 T -(5S9m
L4iatkhe
Sec. 1 7T,1 5 N ,
Location:
R12W, McKin l e y C o . ,
N.M.;
104-7.80-15.62
Sampled Interval:
TD:
500-1560
ft.
2024 f t .
Described by:
R.
Jackson ( 1 2 / 7 9 )
Depth ( f t )
Km
-
dk gry; calc cem; mica.
500-590
SILTY SHALE--m
590-610
SILTSTONE-- m l.?k g r y ; calc cem.
L i t s i l t y ss It
g r y ; sand g r a i n s m-crse, p sorted, srd; q t z ; c a l c
cem, f r i .
K
d
-
610-630
SANDY SILTSTONE--m dk gry; s a n d g r a i n s vf, w s o r t e d ,
ang; calc cem, f r i ; mica.
630-660
SANDSTONE--1t
g r y ; g r a i n s v f , mod sorted, srd; q t z ;
c a l c cem, w i n d .
mica
660-670
SANDSTONE--aa;
670-690
SANDY SILTSTONE--aa.
690-700
SANDY SILTSTONE--m I t g r y ; g r a i n s vf f , m s o r t e d ,
srd; q t z , b i o t i t e ; f r i .
700-710
SANDSTONE--1t gry; g r a i n s vf f , m sorted, srd;
q t z , s l i g h t l y calc, fri.
710-720
SANDSTONE--V I t gry; g r a i n s f - m ,
q t z , biotite; ind.
720-730
SANDSTONE--aa.
730-750
SANDSTONE--aa;
b u t g r a i n s are f .
750-760
SANDSTONE--aa;
b u t grains f-m.
760-770
SANDSTONE--aa;
grains f .
m s o r t e d , srd;
T r dk g r y s l t y sh.
13
Smith Lake #1 continued
Depth
(ft)
770-830
SANDSTONE AND SANDY SILTSTONE--ss
aa but grains f-m.
Sltst mdk gry; sand grainsf, p sorted, srd; qtz;
fri.
830-850
SANDY SILTSTONE
predominates.
850-860
SANDSTONE
m-crse.
870-880
SANDY SILTSTONE
cr
se
880-890
SILTSTONE--m dk gry; calc, fri.
AND
.
AND
SANDY
AND
SANDSTONE--aa
but
sltst
SILTSTONE--aa sbut
s grains
SANDSTONE--aa
but
s s grains
Jm
890-900
SILTSTONE--aa.
900-910
SILTSTONE--aa; trof s s aa.
SILTSTONE--aa
but
color
m
and
It gry.
SILTSTONE--aa; It gry predominates.
940-980
SILTSTONE--aa.
980-990
SILTSTONE--aa
except
some
990-1000
SILTSTONE--aa
except
slightly
1000-1010
SANDSTONE. AND SILTSTONE--ss It brn gry; grains
m-crse, p sorted, srd; qtz, biotite; calc cem.
Sltst It qry and brn gry; ind.
1010-1100
SANDSTONE
1100-1110
SANDSTONE, SILTSTONE AND SHALE--ss
aa.
Sh It gry and m gry.
1110-1120
SANDSTONE, SILTSTONE, AND SHALE--ss It brn gry;
grains f-crse, p sorted, srd; qtz; ind. Sltst m
gry, It gry, andIt brn gry. Sh m dk gry.
1120-1210
SANDSTONE AND SILTSTONE--ss It brn gry; grains
v'crse,
p sorted, srd; qtz; ind. Sltst v It gry; fis.
Tr m gry sh.
AND
brn
gry.
coarser
grain
size.
SILTSTONE--aa.
Sltst aa.
14
S m i t hL a k e
#1 continued
Depth
(ft)
1210-1220
SANDSTONE--It b r n qry; g r a i n s f-crse,
subanq; q t z ; c a l c cem, f r i .
1220-1230
SANDSTONE AND SHALE--ss
1230-1270
Missing
1270-1320
SANDSTONE--1t b r n qry; g r a i n s f-crse, p sorted,
subanq; q t z ; c a l c cem, f r i . T r m qry s h .
1320-1370
SANDSTONE AND SHALE--ss I t b r n q r y ; g r a i n s f-crse,
p s o r t e d , srd; q t z ; c a l c cem, f r i . Sh m dk q r y ;
s i l t y ; calc cem.
aa.
p sorted,
Sh m g r y .
Jcs
1370-1390
SANDY SILTSTONE AND S H A L E - - s l t s t I t b r n q r y ; sand
g r a i n s f , p s o r t e d , srd; q t z ; c a l c cem, f r i . Sh m
qry; s i l t y .
1390-1430
SANDY SILTSTONE--m
qry; sand g r a i n s f , p s o r t e d ,
srd; calc cem, f r i .
1430-1450
SILTY SHALE--m
1450-1560
SHALE--m
q r y ; c a l c cem.
g r y ; v a r i a b l e amounts c a l c cem.
15
Well no: 16T-595 (Mariano Lake #1)
Location: Sec.
26 or 27, T16N, R14W, McKinleyCo., N.M.
Sampled Interval: 500-1600 ft.
TD: 1640 ft
Described by:
R. Jackson (12/79)
Depth (ft)
Km
500-510
SANDSTONE--1t gry; grains m-crse, mod sorted,
srd;
qtz; calc cern.
510-520
SILTY SHALE--1t gry.
520-530
SILTSTONE--drk gry.
530-590
SHALE--lt
and
m
gry;
calc.
Kd
-
590-600
SANDSTONE--1t gry; grains
m-v crse, p sorted, srd;
qtz; calc cem.
600-610
SHALE--1t
610-710
SANDSTONE--1t brn gry; grains m-v crse, p sorted,
srd; qtz. Tr It gry sh.
gry
and
m
gry.
Jm
710-910
SANDSTONE--1t brn gry; grains f-m,
p sorted, srd;
qtz, fledspar; calc cem;
tr It gry sh.
910-950
SANDSTONE AND SHALE--ss aa. Sh m gry; calc cem.
950-1000
SANDSTONE--1t gry; grainsf, p sorted, srd; qtz;
calc cem.
1000-1020
SILTSTONE--1t brn gry. Tr ss aa.
JCS/JS ( ? )
1020-1450 SANDSTONE-lt brn gry; grains f-m, mod sorted,
srd; qtz; calc. Tr m gry sn.'
16
Mariano Lake #1 continued
Depth (ft)
Jt
1450-1460 LIMESTONE--m-It
gry; finely crystalline;
unfossiliferous.
Je
1460-1600 SANDSTONE--mod reddish orange; grains
m-c, m
sorted, srd; qtz; calc cem. Tr m gry sh.
17
Well no:
(Mariano L a k #e 2 )
16T-596
R14W, McKinley C o . ,
L o c a t i o nS: e c2. 3 ?T, 1 6 N ,
Sampled i n t e r v a l :
TD:
N.M.
150-1610 f t .
1610 f t .
Described by:
R.
Jackson ( 1 2 / 7 9 )
Depth ( f t )
Km
-
g r y ; c a l c cem; mica.
150-160
SHALE--m
160-200
SANDSTONE AND SHALE--ss I t gry; g r a i n s m, p s o r t e d ,
srd; q t z ; calc cem, i n d .
Sh aa.
200-280
SANDSTONE--1t g r y ; g r a i n s m, mod s o r t e d , srd; q t z ;
c a l c cem, i n d . T r m g r y s h .
280-290
SANDSTONE AND SHALE--ss
aa.
Sh m g r y .
SANDY SILTSTONE--m gry; sand g r a i n s f , p s o r t ed,
ang; q t z , mica; s l i g h t l y calc.
SILTSTONE--m
350-360
360-390
g r y ; q t z and mica; i n d .
SILTSTONE AND SANDSTONE--sltst aa. S s I t g r y ;
g r a i n s m, p s o r t e d , subang; q t z ; i n d .
SANDSTONE--1t gry; g r a i n s f-m;
T r m g r y sh.
p sorted, s r d ;
q t z ; fri.
e
aa.
390-400
SANDSTONE AND COAL--ss
400-420
SANDSTONE AND SILTSTONE--ss
T r coal. ,
420-450
SANDSTONE--1t gry; g r a i n s f - m ,
f r i . L i t coal.
450-500
SILTSTONE--drk
500-510
SANDY SILTSTONE--1t
subang; q t z ; i n d .
510-520
C o a lb l k .
aa.
S l t s t m gry:
p sorted, srd; q t z ;
gry; mica: i n d .
gry; g r a i n s v f - f ,
p sorted,
SANDSTONE AND CARBONACEOUS SHALE--ss It gry; g r a i n s
Sh blk.
T r coal.
v f - f , ' p sorted, srd; q t z ; ind.
18
Mariano Lake # 2 continued
Depth
(ft)
520-560
sANDsToNE--lt brn gry;
grains f-crse,P sorted,
subang; qtz, feldspar; calc cem. Tr drk 9rY sh.
560-580
SANDY
580-600
SANDSTONE--1t brn gry; grains f-crse, p sorted,
srd; qtz, feldspar; calc cem.
600-610
SILTSTONE--1t gry andIt brn gry; ind.
610-630
SANDSTONE
SILTSTONE--aa.
AND
SILTSTONE--aa
s s vcrse
but
Jm?
630-640
It gry; grains f-crse,
SANDSTONE AND SILTSTONE--ss
p sorted, srd; qtz, feldspar; ind. Sltst aa.
640-650
SANDSTONE--1t gry; grains f-m, p sorted, srd; qtz
feldspar; ind.
650-660
SANDSTONE AND SILTSTONE--ss It brn gry, grains
m-vcrse, p sorted, srd; qtz, feldspar; ind. Sltst
It gry, It brn gry, and m gry.
660-700
SANDSTONE--1t qry; grains f-m, p sorted, srd; qtz,
feldspar, mica; ind.
710-750
SANDSTONE--aa. Little
750-760
SANDSTONE--1t brn gry; grains m-vcrse, p sorted,
srd; qtz; ind.
760-800
SANDSTONE--1t brn gry; grains vf-m, p sorted, srd;
qtz, feldspar. Little m gry andIt gry sltst.
800-830
SANDSTONE AND SHALE--ss It gry; grains f-m, p sorted,
srd; qtz; ind. Sh It gry; silty.
830-840
SILTSTONE--1t
840-900
SANDSTONE--1t gry; grains m-crse, p sorted, srd;
qtz; ind. Tr It gry sh. Tr of coal 8 7 0 - 8 8 0 ft and
890-900 ft.
900-910
talc.
SILTSTONE AND SHALE--sltst m gry;
910-920
SANDSTONE AND SILTSTONE--^^ It gry; grains f-m,
P sorted, srd; qtz; calc cem,ind. Sltst m gry.
gry
sltst~mgry.
and
m gry.
Sh m gry.
19
Mariano Lake #2 continued
Depth
a
(ft)
920-940
SANDSTONE--1t gry; grains m-crse, p sorted, srd;
qtz; calc cem, ind. Trm gry sh. Tr It brn gry s s .
Tr coal.
940-950
SILTSTONE--m gry andIt brn gry; calc. Tr of It
gry ss aa.
950-1000
SANDSTONE--1t gry; grains m-crse, p sorted, srd;
qti; calc cem, fri.
1000-1080
SANDSTONE AND SILTSTONE--ss aa. Sltst m gry and
brn gry.
1080-1130
SANDSTONE--1t gry; grains f-m,p sorted, srd; qtz;
.il?.d. Tr m gry and brn gry sltst.
1130-1140
SANDSTONE AND SILTSTONE--ss It gry and It brn
grains f-m, p sorted, subang; qtz; calc cem.
Sltst m gry and gry red purple. Tr coal.
1140-1150
SANDSTONE--It gry andIt brn gry; grainsf-m, mod
sorted, subang; qtz; calc cem. Tr m gry
sh.
1150-1170
SANDSTONE AND SILTSTONE--ss It gry; grains f-crse,
p sorted, subang; qtz; calc cem, fri. Slst It-m
gry and It brn gry.
1170-1180
SANDSTONE--aa.
Jcs/Js ( ? )
1180-1250
SANDSTONE AND SILTSTONE--ss aa. Sltst m gry and
It brn gry.
1250-1260
SILTSTONE--m
1260-1400
SANDSTONE--1t brn gry; grains
f, mod sorted, srd;
qtz; calc cem, fri. Little m andIt gry silty sh.
1400-1410
SANDSTONE--1t brn gry; grains
f, mod sorted, srd;
qtz; calc cem.
1410-1420
SANDSTONE--aa.
gry.
Jt
1420-1450 LIMESTONE--1t gry, finely crystalline,
unfossiliferous.
gry;
20
1450-1470 SANDSTONE--ss It gry; grains f - m , mod sorted,
srd; qtz. Little sh m gry; calc.
1470-1480Missing
1480-1610 SANDSTONE--mod or pd; grains m-c, mod sorted, srd;
qtz; calc cem. Tr m gry sh.
21
Well No:
1 6 T - 5 9 7( S m i t hL a k e# 2 )
Location:
Sec. 1 7T, 1 5 N ,
Sampled I n t e r v a l :
TD:
0-1939
RL2W, McKinley C o . ,
N.M.
ft.
1939 f t .
Described by:
R.
Jackson ( 1 2 / 7 9 )
Depth ( f t )
Km
-
0-400
SILTY SHALE--m
400-500
SILTY
SHALE--aa;
500-510
SANDSTONE--1t
g r y ; mica.
calc.
gry; g r a i n s f-m, p s o r t e d , s r d ;
q t z ; c a l c cem.
510-610
SILTYSHALE--aa.
K
d
-
610-660
SANDSTONE AND SILTY SHALE--SS I t gry; g r a i n s f - m ,
p s o r t e d , srd; q t z ; c a l c cem, i n d .
S h aa.
660-770
SANDSTONE AND SILTYSHALE--aa
770-780
SILTY SHALE--m
780-790
SILTYSHALE--dk.
790-800
SANDSTONE AND SILTYSHALE--aa.
800-810
SANDSTONE AND SHALE--ss It gry; g r a i n s f-m,
p sorted, subang; q t z ; c a l c , i n d .
Sh m gry.
810-820
SANDSTONE AND SANDY SHALE--SS
Sh m gry.
T r coal.
820-840
SILTYSHALE--lt
840-850
SANDSTONE AND SILTY SHALE--SS I t g r y ; g r a i n s
f-m, mod s o r t e d ; q t z ; i n d . S h m g r y .
but
SS
not
CalC.
gry.
gry; v carb.
aa; g r a i n s crse.
and m gry.
Jmbb
and m gry.
850-880
SILTYSHALE--1t
880-900
SAhiDSTONE AND SHALE--ss It b r n g r y ; g r a i n s f ,
mod s o r t e d , subang; q t z ; i n d . Sh m g r y .
22
Smith
Lake#2 continued
Depth
(ft)
900-910
SANDSTONE--It gry; grainsf, mod sorted, subang;
qtz; ind. Tr m gry sh.
910-930
SHALE--1t and'm gry.
Tr vcrse
ss.
Jmwc
__
930-940
SHALE AND SANDSTONE--sh aa.
vcrse, srd; qtz.
940-960
SANDSTONE--1t brn; grains vcrse, srd; qtz.
960-980
SANDSTONE AND SHALE--ss aa. Sh m gry.
980-1000
SANDSTONE--aa.
1000-1050
SANDSTONE AND SHALE--1t brn gry; grains f-m,
p sorted; qtz. Sh m gry.
1050-1070
SHALE--m.
Ss
It gry; grains
Tr m gry sh.
.
gry
SHALE AND SANDSTONE--sh aa. Ss It gry; grains
f-m, p sorted, srd;qtz.
SANDSTONE
AND
SHALE--aa.
1100-1110
SHALE--m
1110-1190
SANDSTONE AND SHALE--ss It brn gry; grains
f-crse, p sorted, srd; qtz. Sh m gry.
gry.
Jmr
-
1190-1290
SANDSTONE AND SHALE--ssIt gry; grainsf, mod
sorted, srd; qtz. Sh m gry and mod red.
1290-1310
SANDSTONE--aa.
1310-1320
SHALE--m
1320-1330
SANDSTONE AND SHALE--ssIt gry, aa. Sh m gry, aa.
1330-1350
SHALE AND SANDSTONE--sh m gry, mod red. aa.
S s It gry, aa.
1350-1500
SHALE--v sh m gry.Little ss; It gry; f-m,
p sorted, srd; qtz;calc. Tr gry red purple sh.
gry
aa.
1500-1550 SHALE--m gry; calc. Tr:.gry
red
purple
sltst.
23
Smith
Lake# 2 continued
Depth
(ft)
JS
1550-1690
SHALE AND SANDSTONE--sh m gry; calc.S s It brn;
grains f-m, mod sorted, srd; qtz.
1690-1720
SANDSTONE AND SHALE--Ss
It brn; grains f-m, p
sorted, srd; qtz. Sh, m gry; calc.
1720-1740
SHALE--aa.
Jt
1740-1760
SHALE--1t and m gry; calc. Tr gypsum.
1760-1780
SHALE AND GYPSUM--shIt and m gry; calc. Gypsum wh.
1780-1800
SHALE--m gry; calc.
Je/Trw ( ? 1
1800-1820
SHALE AND SANDSTONE--Sh m gry; CalC.S S It brn;
grains f-m, mod sorted, srd; qtz.
1820-1830
SANDSTONE
1830-1840
SHALE--m gry; calc.
1840-1850
SHALE
1850-1920
SANDSTONE'AND SHALE--Ss It brn; grains f-m, mod
sorted, srd; qtz; calc
cem. Sh m gry.
AND
AND
SHALE--aa.
SANDSTONE--aa.
Trc ( ?)
"
1920-1939
SHALE AND SANDSTONE--aa.
24
*
Appendix
KEY TO SYMBOLS AND TER!G
USED
Abundance T e r m s Used f o r Minor C o n s t i t u e n t s :
trace:
little:
some:
much:
0-5% .sf t o t e 1 sample
5-15% o ft o t a l
sample
15-30% o f t o t a l sample
30% of t o t a l sample
S t r a t i g r a p h i cU n i t s( n o ti n t e n d e d
Symbol
as completegeologiccolumn):
Age
Rock U n i t
Kmf
Menefee Fm.
Km Cretaceous
Mancos Sh.
Kd
Dakota S s .
Jm
Morrison Fm.
Jmbb
BrushyBasin Mbr.
Jmwc
Westwater Canyon' Mbr.
Jmr
Recepture Mbr.
Jcs
Cow S p r i n g s S s .
Js
Summervilie
TIW
Winsate S s .
Trc
C h i h e Fm.
~~
"
-
~m.
'
0
Triassic
Abbreviations:
aa
an 9
blk
brn
calc
carb
cem
crse
dk
f
fis
fri
ft
grn
9rY
ind
lit
It
mat
m
e
Jurassic
mod
as above
angular
black
brown/brownish
calcareous/calcite
carbonaceous/carbon
cement
coarse (0.5-lmm)
dark
f i n e ( p . 125-0.25mm)
f i s s i l e( p l a t y )
f r i a b l e( c r u m b l y )
feet
green/greenish
gray/grayish
i n d u r a t e d( h a r d e n e d )
little
light
matrix
medium (0.25-0.5 mm
i f t e x t u r a l term)
moderate,moderately
01
or
P
Pk
qtz
rd
ss
sh
slt
siltst
spher
subang
srd
TD
tr
V
vcrse
vf
W
wh
Ye1
olive
orange/orangish
poorly
pink
quartz
rounded
sandstone
shale
silt
siltstone
spherical
subangular
subrounded
total depth
trace
very
v e r y coarse ( 1 . 0 - 2 . O m m )
v e r yf i n e
(0.0625-0.125mm)
w e l l ..
white-whitish
yellow-yellowish
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