Geology and Ground Water :N Napa and Sonoma Valleys Napa and Sonoma Counties California
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Geology and Ground Water :n Napa and Sonoma Valleys Napa and Sonoma Counties California By FRED KUNKEL and J. E. UPSON "EOLOGICAL SURVEY WATER-SUPPLY PAPER 1495 Prepared in cooperation with the California Department of W^ater Resources UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1960 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library catalog card for this publication appears after page 252 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract.. ________________________________________________________ 1 Introduction._____________________________________________________ 2 Location and extent of the area_________________________________ 2 Purpose and scope of the report-________________________________ 2 Earlier work-_-_---_-_-_________--___-__-__-________-_-_--__-- 3 Acknowledgments _____________________________________________ 3 Geography_ _.___-___-___-___-_______________--__-__-____-___-_-- 4 Topographic features.._____________-__--_______-___-___-_-_---- 4 Climate--____--__-_--_______________-___-___________------_-- 5 Culture. _-.---------------_-------------_---_-_-------------- 8 Well-numbering system. _______________________________________ 10 Geology._________________________________________________________ 11 Geologic formations and their water-bearing properties-____________ 11 Consolidated sedimentary and metamorphic rocks _____________ 11 Petaluma and Merced formations...------------------------- 15 Sonoma volcanics._________________________________________ 15 General features.__-___________._-_____-_-____------_-- 15 Lithology and water-bearing properties.__________________ 19 Sonoma volcanics, undifferentiated-__-_-_-_---------- 19 Diatomaceous member.____________________________ 22 St. Helena rhyolite member.._______________-_-----_ 24 Unconsolidated deposits of late Pliocene (?) to Recent age_____ 25 Glen Ellen formation_________-______________--_---_-- 25 Huichica formation.____.______-._-_-___.______--------- 26 Older alluvium._______._______..__________-_-...------ 29 Terrace deposits and older alluvial fans__________________ 32 Younger alluvium_____________________________________ 33 Geologic history._--___________________..-_-__--.___-_._-__----- 35 Ground water.-_---__---__-._____________-.___-___-___-__.-__----- 37 Napa Valley._________________________________________________ 38 Water in the younger and older alluvium.____________________ 38 Water in the Sonoma volcanics______.-____________---_-_---_ 41 Milliken-Tulucay Creeks area- _________________________ 41 Suscol area___--___-_________-______-_________-_--__-- 43 Calistoga area______________-_-____-___-___--_--_---- 44 Water in the Huichica formation____________________________ 45 Pumpage.________________________________________________ 45 Fluctuations of water levels________---________-_------------ 47 Quality of water.._______________--___-_-_____-.__-_----_-- 51 Younger and older alluvium_____________________________ 53 Sonoma volcanics..._________.-_-_-_________---._------ 56 Huichica formation___._______._____-_________-_------_ 60 Marine formations____-___--__-_-_------_----_--------- 60 Ground-water storage capacity-____-__--_-_-__--___--------- 61 Methods of computation____.-___--__-________--_------ 62 Limitations of the methods- ___--_____--_______-__-_---- 67 Limitations on usability of ground-water storage capacity.- 69 m IV CONTENTS Ground water Continued Sonoma Valley._______________________________________________ 70 Water in the younger and older alluvium.____________________ 70 Water in the Huichica and Glen Ellen formations ard Sonoma volcanics ____________-__ _ _-_ -'--._ _ 71 Pumpage._ ___-_--_____________-__-_-___---_----_----_-.__ 73 Fluctuations of water levels.._________-__-_--_-__-_--_-_____ 74 Quality of water..____ _ _ __ _-_ _ -- -_ _ 75 Unconfined water in the younger and older alluvium___.___ 75 Confined water..___--__-__-____---_----_----_--------_ 76 Ground-water storage capacity.__-____---__----------_-_-___ 78 Methods of computation.-_-___-_-__------------------_ 78 Limitations on usability of ground-water storage capacity. _ _ 84 References cited.______---_-_____-__-_____-__---------------_-----. 84 Tables of basic data___-_______________-__---__---_-------___-__- 87 Index.__._____-_-__-_-_--____________-_-_-__--_-_----_--_-_-.-- 249 ILLUSTRATIONS [Plates in pocket] PLATE 1. Map showing areas of ground-water investigations. 2. Map and sections of Napa and Sonoma Valleys showing geology and location of wells and springs, Napa and Sonoma Counties, Calif. 3. Geologic sections through Napa and Sonoma Valleys 4. Map of Napa and Sonoma Valleys showing water-level contours. 5. Map of Napa and Sonoma Valleys showing ground-wter storage units. Page FIGURE 1. Well-numbering system...._____-_____--____-__--___-_____ 10 2. Hydrograph of well 6/4-22P2 in Napa Valley and rainfall at the Napa State Hospital...___-____----_-----__--_-_-_-- 49 3. Hydrographs of wells 7/5-16B1 and 8/6-10Q1 in Nr.oa Valley. 50 4. Water-analysis diagram of surface water and vater from younger and older alluvium in Napa Valley.-_____________ 52 5. Water-analysis diagram of water from the Sonoim. volcanics in Napa Valley..__-______-__-_-_----__--__-____-___-_- 57 6. Hydrographs of wells 5/5-28N1 and 5/6-14G1 in Sonoma Valley-. - -- - - 74 7. Water-analysis diagram of ground water from Sono*na Valley. 76 TABLES Page TABLE 1. Annual precipitation at representative stations in Napa and Sonoma Valleys._-_______.______-_______-__-______-_-_- 6 2. Stratigraphic units distinguished in Napa and Sonor^a Valleys. 12 3. Estimate of total pumpage from wells in Napa Valley for the year ended March 31, 1950 ___._.__________.______ 45 CONTENTS V Page TABLE 4. Pumpage from the Suscol wells, Napa Valley, for years ending March 31, 1946-52...___________________________________ 46 5. Estimates of pumpage from wells in Napa Valley for irrigation for the years ending March 31, 1946-50.________._._._____ 47 6. Area of younger and older alluvium in Napa Valley, in acres, at 0, 10, 50, and 100 feet below land surface--_--.-_-__-___ 64 7. Estimated volume of younger and older alluvium in Nap? Valley, in acre-feet, for depth zones of 10-50, 50-100, anc1 100-200 feet.-----.-.-.-...-------.-----------.-------- 64 8. Average specific yield of depth zones and ground-water storage units, Napa Valley-----------.--------.---- ----------- 66 9. Estimated gross ground-water storage capacity of the younge~ and older alluvium in Napa Valley, in acre-feet..-.____--.._ 68 10. Water pumped in Sonoma Valley, from wells equipped with pumps of 5 horsepower or more, for the years ending March 31, 1946-50---..--------------_--.-.-----------.----.--.. 73 11. Average specific yield of depth zones and ground-water storage units, Sonoma Valley__-________-_-___ _---------_-_-- 79 12. Estimated gross ground-water storage capacity in Sonoma Valley, in acre-feet.----------.-.._.____.._._.______--__. 83 13. Description of water wells in Napa Valley.--._____-__.._.- 88 14. Water levels in Napa Valley-,.- ------------------------ 131 15. Chemical analyses of water in Napa Valley _.. ___.__-__- 154 . 16.>Partial chemical analyses of water in Napa Valley -_---._--__ 158 17. Drillers'logs of water wells in Napa Valley...______________ 163 18. Description of water wells in Sonoma Valley_._...____.__._ 210 19. Water levels in Sonoma Valley...._-_____________-_..-_-. 229 20. Chemical analyses of water in Sonoma Valley_____.___-_-_ 232 21. Partial chemical analyses of water in Sonoma Valley_ --_-_-.- 234 22. Drillers' logs of water wells in Sonoma Valley___-_-------.- 235 GEOLOGY AND GROUND WATER IN NAPA AND SONOMA VALLEYS, NAPA AND SONOMA COUNTIES, CALIFORNIA By FRED KTJNKEL and J. E. UPSON ABSTRACT Napa and Sonoma Valleys are adjacent alluvium-filled valleys about 40 miles northeast of San Francisco. They occupy alined and structurally cortrolled depressions in the northern Coast Ranges physiographic province and drain south into San Pablo Bay. The valleys are surrounded and underlain by un- consolidated marine and continental sediments and volcanic rocks of Pliocene and Pleistocene age, which are water bearing in large part and togethe:- make up relatively extensive ground-water basins. Napa Valley, the eastern valley, is the larger and has a valley-floor area of about 85 square miles. Sonoma Valley has a valley-floor area of about 35 square miles; in addition, al out 10 square miles is unreclaimed tidal marsh. The rock units of Napa and Sonoma Valleys are divided into four classes on the basis of their distribution and relative capacity to yield water: (a) Con solidated virtually non-water-bearing chiefly sedimentary (some metamorphic) rocks that range in age from Jurassic (?) to Pliocene; (b) marine shale and sand of the Petaluma formation (Pliocene) and the Merced formation (Plio cene and Pleistocene?) that do not crop out within Napa or Sonoma Valleys but perhaps are penetrated by some deep wells drilled in Sonoma Valley; (c) Sonoma volcanics of Pliocene age, parts of which are non-water-bearing and parts of which locally yield large quantities of water; and (d) unconsoMdated alluvial deposits mainly of Quaternary age. The deposits of classes (c) and (d) contain the most important aquifers in the area. Most of the water used in these valleys is pumped from wells in the younger and older alluvium, in the Huichica and Glen Ellen formations,