AN ABSTRACT OF THE THESIS OF Karl C. Wozniak for the degree of Master of Science the Department cf Geology presented on February 8, 1982 Title: Geology of the Northern Part of the Southeast Three Sisters Quadrangle, Oregon Redacted for Privacy Abstract approved: E. M. Taylorc--_, The northern part of the Southeast Three Sisters quadrangle strad- dles the crest of the central High Cascades of Oregon. The area is covered by Pleistocene and Holocene volcanic and volcaniclastic rocks that were extruded from a number of composite cones, shield volcanoes, and cinder cones. The principal eruptive centers include Sphinx Butte, The Wife, The Husband, and South Sister volcanoes. Sphinx Butte, The Wife, and The Husband are typical High Cascade shield and composite vol- canoes whose compositions are limited to basalt and basaltic andesite. South Sister is a complex composite volcano composed of a diverse assem- blage of rocks. In contrast with earlier studies, the present investi- gation finds that South Sister is not a simple accumulation of andesite and dacite lavas; nor does the eruptive sequence display obvious evolu- tionary trends or late stage divergence to basalt and rhyolite. Rather, the field relations indicate that magmas of diverse composition have been extruded from South Sister vents throughout the lifespan of this volcano. The compositional variation at South Sister is. atypical of the Oregon High Cascade platform. This variation, however, represents part of a continued pattern of late Pliocene and Pleistocene magmatic diver- sity in a local region that includes Middle Sister, South Sister, and Broken Top volcanoes. Regional and local geologic constraints combined with chemical and petrographic criteria indicate that a local subcrustal process probably produced the magmas extruded fromSouth Sister, whereas a regional subcrustal process probably producedthe magmas extruded from Sphinx Butte, The Wife, and The Husband. All of the volcanoes in the field area are probably less than 720,000 years old. Sphinx Butte, The Wife, and The Husband are older than South Sister and have been subjected to at least two glaciations. Late Pleistocene glaciers covered all but the upper ridges and summit of South Sister; however, evidence for multiple glaciation is obscure and it is possible that the bulk of South Sister is younger than the second-to-last Pleistocene glaciation. Glaciated andesite lavas at the summit of South Sister are capped by a veneer of basaltic andesite lavas. The basaltic andesite lavas were extruded prior to 6840 yrs. B.P., but are probably of late Pleistocene rather than Holocene age. At some time between 12,000 and 2300 yrs. B.P., basaltic andesitelavas and cinders were extruded from the Le Conte vent at the southwest base of South Sister. The Le Conte lavas may bear only a spatial relation to South Sister. Between 2300 and 1900 yrs. B.P., a series of rhyoda- cite domes and block flows were extruded frcm flank vents on SouthSis- ter. Future eruptive activity is likely at this volcano. Geology of the Northern Part of the Southeast Three Sisters Quadrangle, Oregon by Karl C. Wozniak A THESIS submitted to Oregon State University in partial fullfillment of the requirements for the degree of Master of Science- Completed February 8, 1982 Commencement June 1982 APPROVED: Redacted for Privacy Associate Professor of Gstblaky in charge of major Redacted for Privacy Chairman, Department of; Ge logy Redacted for Privacy Dean of Graduate S0ol Date thesis is presented February 8, 1982 Typed by J. A. Rebekah Wozniak-Gelzer for Karl C. Wozniak ACKNOWLEDGMENTS The author wishes to express his gratitude for partial financial support for field and analytical work provided by generous grantsfrom the Geological Society of America (Penrose Research Grant No. 2758=80) and the Oregon Department of Geology and Mineral Industries (1980). Special thanks must go to the author's major professor, E. M. Tay- lor, who suggested the present study and provided assistance and en- couragement throughout its course.W. H. Taubeneck and H. E. Enlows contributed much in editing the manuscript and were influential in developing the geologic background of the author. Discussions with fellow graduate students S. Hughes and D. Sarewitz were of much benefit. During part of the field season Christian Gelzer accompanied the author as a field assistant; his companionship and assistance weregreatly appreciated. The completion of this thesis would not have been possible without the assistance of the author's wife, J. A. Rebekah Wozniak-Gelzer. In addition to improving the quality of this manuscript by editing the numerous drafts, she typed the manuscript, colored maps, and spent many nights and weekends entertaining herself while the author"worked on the thesis". Above and beyond this she provided essential financial support, continual encouragement, and abundant moral support. For these reasons, the author is most grateful and indebted to her. TABLE OF CONTENTS Page INTRODUCTION 1 Purpose of Study 1 Location and Access 2 Previous Studies 2 REGIONAL GEOLOGY AND VOLCANIC HISTORY 5 Early and Middle Cenozoic 7 Late Cenozoic 8 LITHOLOGY AND STRATIGRAPHY 10 Rock Classification 10 Representation of Mapped Units 11 Field Descriptions and Age Relations 12 The Husband 16 The Wife 18 Sphinx Butte 20 Middle Sister 22 South Sister 23 Summit Sequence 29 Comments on an Unusual South Sister Unit 36 Pleistocene Glaciation 44 Holocene Glaciation 47 SUMMARY OF PETROGRAPHIC FEATURES 48 Basalts of Sphinx Butte, The Wife, and The Husband 48 Basaltic Andesites of Sphinx Butte, The Wife, and 48 The Husband South Sister Basaltic Andesites 50 South Sister Andesites and Dacites 50 South Sister Rhyodacites 57 Discussion 61 PETROLOGY 64 Analytical Techniques 64 Characterization of the Suite 64 Petrogenesis 72 SUMMARY AND CONCLUSIONS 80 BIBLOGRAPHY 82 APPENDIX 1. Petrography and Descriptions of Mapped Units 86 APPENDIX 2. Chemical Analyses of Rocks from S.E. Three 95 Sisters Quadrangle LIST OF FIGURES Figure Page 1. Index map showing location of thesis area. 3 2. Cascade volcanic province. 6 3. Glaciated dacite flow (PsDaLa7) on south flank of 17 Middle Sister. 4. The Husband volcano. 17 5. Geologic sketch map of The Wife volcano. 19 6. Sphinx Butte volcano. 21 7. Rhyodacite lavas of Goose Creek chain and Devils Hill 30 chain of domes. 8. View of the west flank of South Sister. 30 9. View of the north flank of South Sister. 31 10. View of Prouty Glacier on the east flank of South 31 Sister. 11. North flank summit sequence, South Sister. 32 12. West flank summit sequence, South Sister. 33 13. Skyward-projecting, truncated east margin of summit 35 basaltic andesite lava (PsB1La9), South Sister. 14. Summit and east prominence, South Sister. 35 15. Chaotic assortment of reddish-brown pumice of PsDaLa3. 38 16. Ribboned glass and pumice of PsDaLa3. 38 17. Pods and lenses of pumice enclosed in an anastomosing 39 network of opaque glass in PsDaLa3. 18. Pods and lenses of opaque glass in an anastomosing 39 network of pumiceous glass in PsDaLa3. 19. Photomicrograph showing nature of transition between 40 opaque glass and pumiceous glass in PsDaLa3. 20. Photomicrograph of a clear, euhedral osumilite crystal 45 in a small cavity in a rhyodacite xenolith. Figure, Page 21. Photomicrograph showing subophitic texture in 49 basalt lava of PsBsLa3. 22. Photomicrograph of olivine and orthopyroxene 51 phenocrysts in high silica basaltic andesite lava of PsBALa2. 23. Photomicrograph of rounded and embayed olivine 52 phenocryst in South Sister basaltic andesite lava (PsBALa8). 24. Photomicrograph of plagioclase-clinopyroxene- 54 magnetite glomerocryst in South Sister andesite lava (PsAnLa3). 25. Photomicrograph of incipiently rounded olivine 55 xenocryst in South Sister dacite lava (PsDaLa4). 26. Photomicrograph showing ragged margin of olivine 56 xenocryst in South Sister dacite lava(PsDaLa4). 27. Photomicrograph of oxidized hornblende phenocrysts 58 in South Sister dacite lava (PsDaLa4). 28. Photomicrograph of plagioclase phenocryst that has 59 rounded internal and euhedral external margins. 29. Photomicrograph of basaltic andesite xenolith in 60 South Sister dacite lava (PsDaLa2). 30. Photomicrograph of oxyhornblende phenocrysts in 62 South Sister rhyodacite lava (PsRdLa2). 31. Total alkalies vs silica. Alkaline-subalkaline plot. 65 32. AFM diagram. 66 33. Total alkalies and lime vs. silica (Peacock index). 68 34. Silica variation diagram. TiO2 and A1203 vs Si02. 69 35. Silica variation diagram. Fe0* and Mg0 vs Si02. 70 36. Silica variation diagram. CaO, Na20, and K20 vs Si02. 71 37. Total alkalies vs silica. Alkalic-tholeiitic plot. 73 38. Total alkalies vs silica. Alkalic-high-alumina- 74 tholeiitic plot. LIST OF TABLES Table Page I. Chemical analyses of rocks from PsDaLa3 and 41 PsDaLa5. Chemical analyses of rocks from Le Conte 78 Crater and average analyses of basaltic andesites from the field area. Geology of the Northern Part of the Southeast Three Sisters Quadrangle, Oregon INTRODUCTION Purpose of Study A complete understanding of the natural history of theearth must include knowledge of the origin and evolution of the igneousrocks. To facilitate this understanding we must study present day igneousenviron- ments as a basis for the interpretation of pastigneous activity. The major facts come from the rocks themselves, geophysicalevidence, and experimental petrologic evidence. The last two categories of informa- tion are only useful in terms of the first. Detailed field observa- tions are a necessary prerequisite to any comprehensiveunderstanding of igneous processes. "The days are past when study of random samples of rock of unknown structural and time relationship canbe of much real value to petrology" (MacDonald and Katsura, 1964). The Oregon High Cascades offer an outstanding opportunityfor the study of recent calc-alkaline volcanism within the contiguousUnited States. Structural deformation has not masked the basic field rela- tions and Pleistocene glaciers have dissected the pile invarious localities, providing excellent three-dimensional views. Yet there is a paucity of detailed field data uponwhich to build an understanding of the geologic history of the range.