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• writ vi\
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• OtWG' all
wl\la trwa a p
1\7 ...
. (
•
oUtta
15 o 3S ·\era. lutta t riM 10 \o 2S ..tva h'a tAe YaUt17
• iri.~:re Ooa.ael.Sne the watftl'll 1Ja1t. of \be be •
tbe pne ot the coe.-'&1 c:l1tta the ~fa t Y1
IRlFt Gb alopea cr-llil .......... wiNA:I~
JJa 60 90 1
•
ia-ftr..n ucept bT n.riftea --~
"
• Or n the Rirlbr r. be
of t • JaltftWt.au~~t at el &tiona ot 400 to 600
t. B ri
he
boYe H& level.
In their higher waterah cia • oh or th .. etr rn.. a a.all
nial new ~ b7 apring d r. • tlw . p in.&-te4 tlow ot tlw Rinere
r 1a all iY rt. tor irription ~~ th4t dl7 • et
inga ot
er lT of J 1,
tor ~1 • In be1r .-.-....
URI"~ lena riDU 111
can'7 larp tlaab n
• a.t: ra a Or
._ ...... ....,~ t t.he publJA
~~-now 1a ci1Y•
...._. an lat.end.'
raiat..U.. ·---l'd.DT .......
•
•
u
a
la
_,_
au
a , tlveq
•
ott. t
of of
tin
t .. •
~
__, ... ......... . •••••••• ••••• 123.?
d
t.bl J.-.1....,_
\e
• t
tiM ' is J" PW17 ._., !ll
t
; lJorlcDi b - ..s. •• • Sat all
July • •••• ••• • 72.2 u,q.t • ••••• • l26. 7 ~ .. . .. 139.7 Oe\Ober • • •••• l56.9
y 77.9 .~ .. ~ ...... . 26.5
•••••• ' lor
•
ot
•
...
polopo .... !be old..t a of the
a bl"fttl bualt.. wit.h -- ifttei'II~Mel aaad-
et«1es, liiV"
e of outc
., .1n the toothUld ot th
r iuea tot
T e U
pl.ace
teristic
t
P• Oth r t.cropa not obMrved
ast ot tho h adwaters of the Rid"
rock d an in
litUe or no
)'OWl er rock • .. ~ Upper Cret ceaua t"'Oka a and
late • • Th rocks crop out
r to .U. or
rt c ill the
•• tb•
o!t • la s.no ret ro tb priJlCipal •
fhey dip •out rd &l ot 15 t.o 30 de
• or the Ja •
1n the 1 i pitt t 1CIIl.
, t e joint& an bedding • ot tho rook -la edby cU.s olu 1 ot 1"Colat1n r which in pl. •
a
r
,
- s -
al10 to axtena1ve tu'b•lar aolut1 . PMKP•• Tbroqb w.. .. • in tbe upper looce U.st.ca tb_.. 1a ~17 aot1ve eirala-
ti ot wui wa.ter. &wnr&l •PI'iDI• o1 udeft\e \o 1arp tlJnr -•
t ell opm1naa ill upper &oo.- U..at.eD• 1A t.be 1111*'-'-- ot tbe
n•n clea Oranpn the · lvDl"e lleJ'•r• the llpriDca riM Sr1 deep
rav111 a or ~· tt. liMa\cDia ,_.....u,- at. ., .uptq ~·
the CCilt.aot with the uaderq1n. Dpel"fiOU Uppw Cnt..._. I'OCh•
0Yerl.71na upper locme rocka to tM ~ ot J.--1 are INKfi
lHI'lts ot . liecene age which crop ~ at the Mll'f&P in a belt alMI& the
R1•Ure ohe. !hie belt extends southaas\ '\o tbeltn "ao.a.une
bout 3 kU~era orth ot Jaaael.. ...-the . or the ltl..Ure Oeuabe
aDd al B the Bivi re aoa .. une the Pl!oa.. HCI~a com~i.t. pr:I.M1pal•
)¥ ot . .consol1d.at.ed .cCQglaMrat•• unclnm•• aUtatcmea; aad llaJ'la.
In t ia vicinity the beds dip aogthwat at. ana:» • ot about 10 to as depoe e. S1a11 r Pliocene MC:U.JMh\a pro q ut · beneath J--..1. aD4
the wat.em part ot tbl Jacldl-KQ'er beach but al*e largU, covered b7
701m· r Ple1.tocene aDd ecet. depoaite. !he t1ner gra.IDed .taolee ot
the Pli en. a(t(l :ta such ae the sUtatot.s .md .W ban low pei"M&•
bU1t7 and Utt.la OaJ*)1t7 t .tore v tran•it. vatAr. er. ._. ot
\be coqlo.er •• :t4l1T perMable •
pna ill t. • zcme 01 lf' }t tt. -r p . pod pelU ot w ur to
well•· p&I"Clt}7 weU. ave aa 7ft bee clrillect iDto the P'U . e
~t.e ill the Juael area. aprlap that la-. Ira theM
aed1Jie • .- obeel'ftd darfAa t · reo aiaii8Doe.
'tbe J~ '*aob 18 ~ u:nderldll bT aariDe and
en , d Uppe Cretaoeou rocka. •1
-ot the Jaael ~ b th.• Pl~e oen uu
lltoMa arw aodent•l¥ o HA.I!Ii~
ot aaturatioD ,Ulcl .IIDIII!ei'A
th
t ur t.o wUa. t · atne d..a ill J OJMl., w1l No. 1 ( ... ac
p) \aiDe a COOd 71•U t rated •tena.l thia type
ot to be MGl.rG-
ot
• :region aN aec~
-........~a ...... al cr....w.
1Y1 re O&ucbe
ean4a 1n the 1 p a ot the v.U ot t
1..-Un a• CU"17
undart'L that could e nadil7 tapped rr U• ot IIDderate to la - pi'Oduot1vif¥. leoct alludal a
&leo tldllq 1.e PlelAooene " a oL parb ot t.h• I i]....,er _,.. ..
~ al.-c • •~ t tM U n d.ee 0 ..,.. the 1"Y1A
• 1•
Kqer. KQWftJ'• theJ 8ft . Ml'al.q no _.. tUft a f, -'en tht•
d an .ProbabJT · abcmt the .-e of ·aat.urat1<a.
The u1tillate 80\ll"C4t ot around wat.r 1n ·the rooks of t.h Jaael
qer belch and ot the 8tU'l"'UDCl1Dc area 1e ra1ntall. Ko& ot th.U naa
b7 traaepirat.iaa ot plmta. Hawner, a. coaalct.nbl. part ... ,. _.
arouact .... pel'lltitltle roen erop ·c:.Nt at the IRU"taoe. Ill 't.hia --
tbe principal aqtdt • ot tn Nl1oa are npl.wtbed cb par d\ui.q
r~ .... . • • swm aqu1t n aut.drl ~ ckT ....... tlowa ot t
tPriD&••
vw•uuc. to the div nS: 7 ot \he rook P.nact\tna and ~ the I"'CCI(
' '"' ot • n&i«l, tlan !a pi'Obabq aon than aae •-'• ot &'J"NRRl ..
n er clroul.at1oa. ODe c qetea ap an to uiat 1n the 1q)per K.-' ••ae
larp areal extAn
Upper Cnt&oeoua roaka, .-. ot thia w er 1s Ntumed to the aur1" ee '
in aprinp euob aa thoM ot the ltiY.i re dea Ora.ngera
Mqv. Howver, a OO'IlG.derabl.e quaDtit.7 ot the JtN...W(.,
llOYta do1Cl dip 4 aGQt.bwaJrd thrott&b the und.ieaeot...t l~u paaaift&
_,_
0
p · ble Pliocene ·or P1•1~• ..,.,..,.
crop out at the ~ tbe PlJGHAe and Plalatoo •
• 1ta also ro e1ve V&ter b7 Utratiz :tJQa raiarall or tr.
•t • r tlnaa ..._lwd ~·• 1Die throucb • DeJ"MJIWl.e
d di•charge at the •de• ol t.be ... 01' sa Mdaar1u iDa•·
Ov r 14 the area of tiM J.-.1.,.....,._ ch t.be reaJ.ou tv
t. ble · Ue t oonaJ.derable ct.pth bolow t.ba .artace. South ot t •
<r road 1t 18 p ~ liON thaD 20 (tl-S below
be £~• excopt. i.nlatadi-.e]¥ alaac the coaat.. BowYer • the pei tric
t J.e ot the bench.
1'be ~d-v er \Bidertlow in t.he 1leo.rt alluv11aa ot the Tallqa
of th Rivi res CJo line d O.Ucbe and the Or.nde ivUr. ct. Jacael
1s derived e;ssentitllly trcm the intlltra.tion ot those .treNU. In .t
1ow r parte ~ t.heM vallqa tbe wat.• table 1 probabl;y w1 lWl a t
t.e ot tbe aurt ca. · ..
lf.U and Spi"!Ap
well -was obaernd du1.a& the r - .. a ••an-• Apparet.lJ h
ot tbe cb lurre little n at.tap\ to cin'el.op H _. hGa well•
wen tor ~lo or at.ock u • Bp.rin&a &N UMd U.at u.ol*d
- l' MQ9U. • •
tor
_,_
U o. l ( aea aap) t Ua• Uat.ne M m Ja 11 l.ooAit...t
~ 50 meten tu n line 3 .-... abGn .. lwel.
18 ) ileten 1n dla..t.r Sa dq, aevbed to a cs.pUa .t
n m cav moua Pl o • 1'he Rll\le
1• 2. _.t ... _. ..q 0.4 .ner abcwe
e vell 11 pped· ld\b a pl.t.cm 7ielde about
9 li~era per 8.0 with a ralfd ol q 0. 10 • .,..
:t I' t ar :t. n 1 26 ct. a C.-1tiar a , d the tar 1• ot
in 1944 bat in Mn or 1 • -
use 1n tb.en ith no nid ce or Mlt- ter cont. tiOil
• o. 21 pert.& due Jn P'reo oolcnial a, 1a l'l
oav o tilled d dJ7 at a ot S .n.en. The w1l u .n.~ lT
ue&l~aUt~l8 l.t 1a now used
wll located a th
bone leYal.
3 wu dll& ill t lonial peri 1a
110re 150 Je&l'l old. well 1e 3 Mter• 1n ds.-t.er
it at • It e dJ'7 at a &8\IJ"ed ot 18. 7 ..ter•
t n d or tUlad 1n & w 1a
N l.e•el t:e ooo.tec! ab 300 ere .t-
u o. 2.
•• -tho• ot the liYilN des Onna re d t .. ot 8 R
~,.r an ita tribGt n.a.
· 10·
Spr!IJ&e Ne. l - S ar •• 0 r anpn riM al.GD& U.. 8Dftel
t t BivU" ct.a Oranpra ,_l/2 ku.c-krs raetheut ot .J.-.1..
eprinp all 1atrue t ~ meu or Jein\ed upper u..t.ou.
TW'f~r1.0U Upper em. bual Ol"'ppt eM. a tlbDr\ clUt.aM• ..,.
ortJa &lope ot \he O!iiJI'CII' o1 t.be !U.YDn •• nqen-... t.q
that. er 1D the \\~)per _ • la lOI'Oed te tu tac v..L~'lr vi\h t cal.clw ""*.. Then ..,.. t1w prta...
c .o~ ll'l'lllillt an ., leb an t.4Ml w1Udn
a t 200 Mt.er• of
tb 00b41Nt.e bGic, and the Q of 1• W !ato & OGW .... IG
a fllto a ...U coaoNt.e ..U.nift& U... A
12- lock Jolllt p l.1ne lver• \be W&\eJ' tl'Ga \hta )Mdnt o
~u~,. mM t.be ~ i• clo..S aU ot .naa • et"ell' oown , t.. "'-1. t t.w el1'Y
J
•r ol _. oped apr!Dga l.a.,. tra t.h• uppel'
eno I'OCka 1ft till enl vieinit7 u Sounea Or n . the
agngate di7 ... now of tb ...,. 20 0 30 lit. ... JMt"'"
CGnd &1.1 ot ich "* dift tor he ion ot • &1GD4
......... .a.vn <lee 0rangeJ"8.-
....,.__ eprita
--.- tlow •t
VieUl.e
tr. th• o.balllt.t ot JU.w:Ure ~ ..
.... ( •• 6) riM~ 10 ...........
.WW'IAA. 11le •rSaa
.. ~&tolatle• · 1\e -1/2•
. u .
nm"'"" 504~·• U..toae at the OCIIltaot with blperri.oua Upper Crvt.aoec:Na
be •Prill< d1 bar vas .t.iMt d at t.o Ut.era per ~~eccmd.
The t rature of the w er u 23 clesne• C..t.i.&ftde.
~ w (Wo. 7) alao 1utd8 tr. a •lut.laa paaaap SO
c ntiMtere to 1 or ill di...t ~" 1n upper Boom• U..atane appanll•
t.~ not above the oonta.ct with the Opper CNt.ao reolca . t
e rill& 1a located 1D the bot ot a dHp I'&T1De near the bead of a
triwta17 ot the ivUr. .,.... !he •Priaa cliaob.&rp • eat.U.
70 li\ere Pft" • • 'I'M vater • a t.
c
f SoUJ."Cft euve. eprinc - .... • troa a plae and a joint
1n us iw upp.r 600- u...tcae ~1¥ avon w tbenid blp4Jrvi
Upp r Cnt.a eoua tio • 'l'be diaobara• ot the eprin& waa
eat.J.aa d at ) Ut.era I' aeocad. ! t tu:re of the vat ie
25 d II""• Cmticr'..S..
All the epriqa ot the R1 re Hqer are NpOJ'tecS t inc
flow dar1Aa tha raiJl7 aeasou. The tl 1a dlY !'ted t t.ba Gfta11l1UU
ot the riv r tor t • 1rr ation of 1
ryer.
other aprlngeJ Souroe D Source La ou.Me, are
reported t.o ri .. 1n t.be de-s» ravine ext eaat of the beadwaten oL the
1Y1 re r. TbeM ueecl tor t.h• irri&ation ot land~ in the eaatem
rt ·ot t b-.oh.
-12·
!be pra.-t w rer euppq ot Ja-.1 obt&!ftttd tJ"C* the 8aw'cle•
Onngera ia iadequate frsr tbt •ecSa of tbe 41t.7 • .,..,.u7. ~
-:\eldaat.ed t... UM ~· tiM _.,
.... w.t..
ot J gel
60 to 80 aet.eJ!'a 1n 'P'lelatoaene or PU.OO.. aed ta. Ia
p . • o1
sa then 20
·in& to Mtpp]q the h
..Uwt .
& ~uta ~tal npp~
trca lou.Jae.a OJ'...,..
lid t . RecClt. &lluri:
I tbe !ty.
v.a
-13-
Duiq 1rrlp\iaft ot part• ott J .. lal.·-MtrJrer
_.,"" 1a ~ b7 cllwnla ot \ tlewa ot epriftp ot t. 8.1: n
• OftD&Wa• aDd tile B1YDn ...,.... 111Mt ot \be Soue•• .&1&11-no
La R • ,_ nilable tlw 1a to 4Mnr GlllJ- ..U •
ot e 1rr!plWt UN. Witll tt.. preset prJaltlye IJII\c- et irriga-
t.i: OGI\.sderable w r 1• 'tiUtAd aeepe wq ill wltMd dlt a
~ tcmt it oaD lMI applJ ed t.o t.bl • ~ tht water 1oM
NOOftncl biT wlaa eli ..... ..u. u by !lip iJ"''iptiGil
i.e••·
indio that t~ .trata 11Utt'1eict.]7 pNduct1•• tor 1rr!
tioa abnld be preacmt. .. t.n the J ~qer benoh. It 1a bel1eftd
t ott t...t well.• to apl t. atrata 'WOUld jua\Uiecl.
Sqpa l oal1t1• 1 drl1l are 2. 4 6 ~
ot J al · tbe J..-.1.-M react. fh. Ua dri. t.o
-s11waa ot 80 \o 100 en tv lllleqaate dplor~ttiaa. U t
ot Ma clr:lll.q piVft taY~ t1 vella t
Gt. 't' pu\1 ot t.be ~ •
,~ •• 1
J 13. 1 ~9