Quake ? 3

[Manley Hubbell]

"HUB"pub#JD=2450962.9:13 A.M. PSt 13 CAUAC 17 ZIP
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A first attempt at cross corelation of ?
`MAJOR' EPOSODIC "UPLIFTs" in the Pacific Northwest
possible elevations (for referance mostly) | beach
date alvord | Valley Plains | terris
east west | Vancouver Lake Twalitin Valley | sands
2000 4000 4000 | sea0 tide flats 120 Jackson bottom| sea
00 4020 4020 | 80? 200' north plains | 150
-2000 4040 4040 | 160' :::::::::::::::::?| 350
-???? 4080 4080 | 240' fourth plains |
/////////////////////////////////////////////////////////?
4200 300' Mill plains 750
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Alvord lake flats EAST "artifacts"
2000 4000 ALVORD DESERT
000 4020 SailorJack Springs 11 & R34S | R35S
-2000 4040 "TULE SPRINGS" 5
???? 4080 corner sections 5,6,7,8
//// BENCH MARK 4117
\\\\ Little Sand Gap 36S35E8 118.25.42 42.26
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date Alvord lake flats WEST "artifacts"
2000 4000 ALVORD DESERT
000 4020 on A line between T34E | T35E
-2000 4040 springs
???? 4080 road bed
////
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date Valley plains farmlands LOW
2000 SEA TIDAL FLATS VANCOUVER LAKE T2N R2E S26
000 80 ?
-2000 150? ?
???? 250 FOURTH PLAINS
//// 300 MILL PLAINS
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date Valley plains farmlands HI
2000 120 JACKSON BOTTOM
000 200 NORT PLAINES T1N R3W
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coastal terris sands
2000 sea
000 150
-2000 350 seven devils mine seven devils road t27S R14W S33 123.00.00
45.36
???? 750
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"use your head women this 1st effort cannot be relied on for anything"
" search for the following instead "
Anadarko Petroleum Corporation (1995, p. 23) reports that "the
geothermal reservoir..... in Section 22 occurs in highly fractured
volcanic formations and interstratified sediments underlying 1,087
feet or more of post-volcanic sediments." The thermal aquifer host
rocks consist of unwelded and welded crystal, lithic, and ash tuffs.
"Thick basalt" was intersected "in only one observation well,
25-22A,
at a depth of 2,400 ft." Anadarko Petroleum Corporation (1995)
suggests that the welded and unwelded tuffs of the thermal aquifer
correlate with the tuffs exposed in the Tule Springs Rims mapped by
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