Geology and water resources of a portion of the Missouri river valley in northeastern Nebraska . ^ o<a 0 bc-S 0 P 1 ^ g, : g , , g , , : : :g . be -000 - ^Rcooc .M^^cc;^ 0 0 0 0 0 0 0 0 0 s o_- i cePC : ; : ec : : :^ t: 1 0: ?t-1 1 c- II XJ-O ?s 1 • • e; t3^ 1 :| Mill ;1 ,oi»C^OJ«»c«oocoooocoM«»-o<oc<oooio-^(NOi ooxo-^oooiociooiooooccio 00 fel 00 O 00 to O CO CV| Q I© ?*-^ C» 00 N «0 CO •* CD •^ ?^ to •* <0 C<l <0 C<l CO C* e<5 CO 00 iC <0 O CO 00 00 CO 00 C<I(N CO OO <U M rl CO f-l CO r-H S CC M (N rH (N .-H eC CO (N CO ococos;eo . .coco CO . .CO . . ^i-ir-ic^
Geology and water resources of a portion of the Missouri river valley in northeastern Nebraska . ^ o<a 0 bc-S 0 P 1 ^ g, : g , , g , , : : :g . be -000 - ^Rcooc .M^^cc;^ 0 0 0 0 0 0 0 0 0 s o_- i cePC : ; : ec : : :^ t: 1 0: ?t-1 1 c- II XJ-O ?s 1 • • e; t3^ 1 :| Mill ;1 ,oi»C^OJ«»c«oocoooocoM«»-o<oc<oooio-^(NOi ooxo-^oooiociooiooooccio 00 fel 00 O 00 to O CO CV| Q I© ?*-^ C» 00 N «0 CO •* CD •^ ?^ to •* <0 C<l <0 C<l CO C* e<5 CO 00 iC <0 O CO 00 00 CO 00 C<I(N CO OO <U M rl CO f-l CO r-H S CC M (N rH (N .-H eC CO (N CO ococos;eo . .coco CO . .CO . . ^i-ir-ic^c^coe^.-iese^<MCST--( ,-H ? ,-1 CO J~^ ^ rr\ CO ^ -^^ 5 CO CO CO ^ ^5 ;^ . , . CO 1M MMOTCCCO en CQ02 CO MJ CO CO03 cc CO CC02OQ CC CO CC !Z; JZI CO :8gS^ • . ^ . !Zo2<z;co?;co co^ H^CO .cs-^co coZcn Kg !2;co ^4 -•* •< . ^% 00-I com. 38 MISSOURI VALLEY, NOETHEASTERN NEBRASKA. Arfciiian ictlh.—All of Boyd County is underlain by Dakota sand-stone containing artesian water, but only a limited area is low enoughfor surface Hows. Strong wells can be obtained along the Missouribottom and along the Ponca Valley at least as far west as heavy pressure in the deep well recently finished at Lynch dem-onstrates that there is a deeper and stronger flow^ th^re, and prob-ably that artesian wells can be had farther up Ponca Creek and Nio-brara Kiver than was formerly supposed. A deep flow w^as reachedat Lynch, which has sufficient pressure to raise water to an alti-tude of 1,51)0 feet. This indicates that a surface flow can be obtainedin the valley below Spencer, at a depth of about 1,065 feet. If thel^ressure increases westward across Boyd County a flow may be hadin the valley below^ Anoka at a depth of about 1,170 feet, and as farwest along the Niobrara bottom as the Badger Bridge and probablyfarther. Wells far to
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Keywords: ., bookcentury1900, bookdecade1900, booksubj, booksubjectwatersupply
