Supplemental Figures and Captions for Supplemental Tables

Similar documents
Math 95--Review Prealgebra--page 1

Terms of Use. Copyright Embark on the Journey

Classification of Components

Lesson 24: True and False Number Sentences

& $ CORED mbsf SITE 932 HOLE A. Graphic Lith. Section Age. Sample. Disturb. Meter. Color. Description. Structure. CALCAREOUS CLAY and CLAY

1. The graph of a function f is given above. Answer the question: a. Find the value(s) of x where f is not differentiable. Ans: x = 4, x = 3, x = 2,

A A A A A A A A A A A A. a a a a a a a a a a a a a a a. Apples taste amazingly good.

Worksheets for GCSE Mathematics. Quadratics. mr-mathematics.com Maths Resources for Teachers. Algebra

Patterns of soiling in the Old Library Trinity College Dublin. Allyson Smith, Robbie Goodhue, Susie Bioletti

2mm Pitch 2 Piece Battery Connector for Litium-ion / Litium-polymer GF SERIES E-9

INTRODUCTION TO TEPHROCHRONOLOGY

Lesson 7: Linear Transformations Applied to Cubes

Eureka Lessons for 6th Grade Unit FIVE ~ Equations & Inequalities

Feet. Cape May Core #51 Start depth: 240 ft Stop depth: 245 ft Recovery (ft): 5.1 ft Date: 3/21/94 Described by: JVB, KGM, CL. 5.

Mrs. Charnley, J303 Mrs. Zayaitz Ruhf, J305

Lecture No. 1 Introduction to Method of Weighted Residuals. Solve the differential equation L (u) = p(x) in V where L is a differential operator

Appendix A: Core descriptions

Station A. 3. The amount of time it takes molten rock to cool and harden mainly affects the rock s. A. Color B. Mass C. Crystals D.

Detection of Late Pleistocene tephras and cryptotephras using major element chemistry of glass shards from Chikyu C9001C cores, NW Pacific Ocean

Atomic fluorescence. The intensity of a transition line can be described with a transition probability inversely

Big Bang Planck Era. This theory: cosmological model of the universe that is best supported by several aspects of scientific evidence and observation

GY 402: Sedimentary Petrology

" = Y(#,$) % R(r) = 1 4& % " = Y(#,$) % R(r) = Recitation Problems: Week 4. a. 5 B, b. 6. , Ne Mg + 15 P 2+ c. 23 V,

Classwork. Example 1 S.35

GSA Data Repository item

KENNESAW STATE UNIVERSITY ATHLETICS VISUAL IDENTITY

Geometry. A. Right Triangle. Legs of a right triangle : a, b. Hypotenuse : c. Altitude : h. Medians : m a, m b, m c. Angles :,

Chapter 5. The Sedimentary Archives

Quantitative Screening of 46 Illicit Drugs in Urine using Exactive Ultrahigh Resolution and Accurate Mass system

Bring a printed copy of this lab to your lab section. We will answer the lettered questions in class.

TSOKOS READING ACTIVITY Section 7-2: The Greenhouse Effect and Global Warming (8 points)

Laboratory#6 Sediment Particle Size Distribution and Turbidity Flows

SUPPLEMENTAL MATERIAL

Worksheets for GCSE Mathematics. Algebraic Expressions. Mr Black 's Maths Resources for Teachers GCSE 1-9. Algebra

Secondary 3H Unit = 1 = 7. Lesson 3.3 Worksheet. Simplify: Lesson 3.6 Worksheet

4º ESO BIOLOGY & GEOLOGY SUMMER REINFORCEMENT: CONTENTS & ACTIVITIES

A A. an at and April fat Ana black orange gray cage. A a A a a f A a g A N a A n N p A G a A g A n a A a a A g a. Name. Copy the letter Aa.

8D Series Common Section

NAME: GEL 109 Final Study Guide - Winter 2008 Questions 6-24 WILL be on the final exactly as written here; this is 60% of the test.


GEL 109 Midterm W05, Page points total (1 point per minute is a good pace, but it is good to have time to recheck your answers!

(Lecture 18) MAT FOUNDATIONS

Data supplement to. Villamor, P., Berryman, K.R., Nairn, I.A., Wilson, K., Litchfield, N., Ries, W., GSA Bulletin

7.3 The Jacobi and Gauss-Seidel Iterative Methods

Uncertain Compression & Graph Coloring. Madhu Sudan Harvard

A Posteriori Error Estimates For Discontinuous Galerkin Methods Using Non-polynomial Basis Functions

Clyde River Landslide

Piles of Fire Individual and Team Project Modified from

Recurrence Relations

Feet CLAY; silty, greenish gray and clayey fine sand; Color: 5Y 3/1

1. The timeline below represents time on Earth from the beginning of the Paleozoic Era Ato the present B.

Section I: Multiple Choice Select the best answer to each question. Mark your final answer on the answer sheet. (1 pt each)

SECTION 7: STEADY-STATE ERROR. ESE 499 Feedback Control Systems

GEOL 440 Sedimentology and stratigraphy: processes, environments and deposits Lectures 16 & 17: Deltaic Facies

Support Vector Machines. CSE 4309 Machine Learning Vassilis Athitsos Computer Science and Engineering Department University of Texas at Arlington

UltraWeatherBug3 HSPI User s Guide A HomeSeer HS3 plug-in to access live local weather conditions, forecasts and severe weather alerts

2.4 Error Analysis for Iterative Methods

ES120 Sedimentology/Stratigraphy

As compaction and cementation of these sediments eventually occur, which area will become siltstone? A) A B) B C) C D) D

Landscape Development

State the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks.

Math 171 Spring 2017 Final Exam. Problem Worth

The Geology of Sebago Lake State Park

Quantum state measurement

The Geology of Cobscook Bay State Park

The San Benito Gravels: Fluvial Depositional Systems, Paleocurrents, and Provenance

SUPPLEMENTAL INFORMATION DELFT 3-D MODELING: MODEL DESIGN, SETUP, AND ANALYSIS

Geology Stratigraphic Correlations (Lab #4, Winter 2010)

Free energy dependence along the coexistence curve

Lab Activity on Sedimentary and Metamorphic Rocks

Investigation #5 Position, speed, and acceleration

Lecture 3 Transport in Semiconductors

Geo 302D: Age of Dinosaurs. LAB 2: Sedimentary rocks and processes

Chapter 4. Eumeralla Formation Facies and Distribution

Chapter 8: Learning objectives

M.5 Modeling the Effect of Functional Responses

Final Exam. Running Water Erosion and Deposition. Willamette Discharge. Running Water

Definition: A sequence is a function from a subset of the integers (usually either the set

Haar Basis Wavelets and Morlet Wavelets

Field Trip Number One. By: Pat Dryer. Geography 360

TECHNICAL NOTE AUTOMATIC GENERATION OF POINT SPRING SUPPORTS BASED ON DEFINED SOIL PROFILES AND COLUMN-FOOTING PROPERTIES

PARTS MANUAL Gas Furnace F8MXN, F8MXL, G8MXN, G8MXL

LONG ISLAND CLAST ORIENTATIONS

Stratigraphy and structure of the Ganson Hill area: northern Taconic Allochthon

Enhanced Instructional Transition Guide

NVLAP Proficiency Test Round 14 Results. Rolf Bergman CORM 16 May 2016

B) color B) Sediment must be compacted and cemented before it can change to sedimentary rock. D) igneous, metamorphic, and sedimentary rocks

Pre-Lab Reading Questions ES202

GEL 109 Midterm W01, Page points total (1 point per minute is a good pace, but it is good to have time to recheck your answers!

LAB 2 IDENTIFYING MATERIALS FOR MAKING SOILS: ROCK AND PARENT MATERIALS

CEE 437 Lecture 10 Rock Classification. Thomas Doe

Structural Geology Lab. The Objectives are to gain experience

Vero Beach Elks Lodge # th Street Vero Beach, FL /

GLY 155 Introduction to Physical Geology, W. Altermann. Press & Siever, compressive forces. Compressive forces cause folding and faulting.

Variations. ECE 6540, Lecture 02 Multivariate Random Variables & Linear Algebra

Figure 1. Map of Feather River Basin in northern California. (A) Region straddles the northwestern Sierra Nevada and Sacramento Valley.

SOUTH CERRO AZUL STRATIGRAPHIC SECTION. Upper Cerro Azul flow of the Servilleta Basalt (Tsbcau) Lower Sandlin unit (Tsl)

Geology 12 FINAL EXAM PREP. Possible Written Response Exam Questions

Labels Thermal Transfer Label Materials

CS Lecture 8 & 9. Lagrange Multipliers & Varitional Bounds

Transcription:

Kuehn, S.C. and Negrini, R. M., 2010, A 250 k.y. record of Cascade arc pyroclastic volcanism from late Pleistocene lacustrine sediments near Summer Lake, Oregon, USA. Geosphere, Vol. 6, No. 4 (August), Pages 397-429. DOI: 10.1130/GES00515.1 Supplemental Figures and Captions for Supplemental Tables Site F sandy bed J3 sandy bed K bed L sandy major unconformity bed K Site E unconformity sand bed L bed L sand major unconformity major unconformity bed O bed Q bed P bed N bed M Figure S1. Major unconformity at sites C, E, and F. White card in photos is 15 cm high. Yellow and black scale bar is marked in 10 cm intervals. Only beds visible in the photographs are labeled. 1

Site F bed R bed S bed T bed T1 sand sand minor unconformity? bed W bed R bed S Site E bed T bed T1 sandy minor unconformity? bed V minor unconformity? bed V bed W bed W bed Z Figure S2. Unconformity between beds T1 and U at sites C, E, and F. White card is 15 cm high. Yellow and black scale bar is marked in 10 cm intervals. Only beds visible in the photographs are labeled. 2

Site E bed J3 sand and granules bed K bed L possible unconformity sandy sand over carbonate unconformity major unconformity sand Site F bed J3 sand and granules possible unconformity sand over carbonate = unconformity at site E Figure S3. Unconformity that cuts deformed beds K and L at site E and probable unconformity below bed J3 at sites E and F. White card is marked in 1 cm intervals. 3

bed NN Figure S4. Tephra bed NN at site C. Scale is marked in 10 cm intervals. bed LL3? bed MM bed MM1 Figure S5. Tephra beds MM, MM1, and possible bed LL3 at site C. Scale is marked in 10 cm intervals. 4

bed LL2 Figure S6. Tephra bed LL2 at site C. Scale is labeled in 1 cm intervals. bed LL bed LL1 Figure S7. Tephra beds LL and LL1 at site C. White card in photos is 15 cm high. 5

laminated, redeposited tephra bed KK) (primary graded bed) bed KK1 Figure S8. Tephra beds KK and KK1 at site C. White card in photo is 15 cm high. Beds KK and KK1 are present at all three sites and are the lowermost two tephras in the site E exposure. KK, KK1, and the fine, laminated sediments above KK together form a distinctive and easily recognized set. SPG core A bed JJ1 bed JJ1 bed JJ1 Figure S9. Tephra bed JJ1 at site C and in the SPG-A core. Scales are labeled in 1 cm intervals. White card is 15 cm high. 6

bed II1 bed JJ bed JJ bed JJ bed JJ 0.2 bed JJ 0.4 Figure S10. Tephra beds JJ0.4 through II1 at site C. Scale is labeled in 1 cm intervals. 7

bed II Figure S11. Tephra bed II at site C. Scale is labeled in 1 cm intervals. bed HH Figure S12. Tephra bed HH at site C. Scale is labeled in 1 cm intervals. 8

bed EE1 bed EE2 bed GG bed FF bed EE2 bed FF bed GG Figure S13. Tephra beds EE1 through GG at site C. Scale is labeled in 1 cm intervals. 9

bed DD1 bed EE Figure S14. Tephra beds DD1 and EE at site C. Scale is labeled in 1 cm intervals. bed DD Figure S15. Tephra bed DD at site C. Scale is labeled in 1 cm intervals. 10

bed CC Figure S16. Tephra bed CC at site C. Scale is labeled in 1 cm intervals. Site E bed BB bed BB1 bed BB Figure S17. Tephra beds BB and BB1 at site C and BB at site E. Scale is labeled in 1 cm intervals. 11

Site E bed AA Figure S18. Tephra bed AA at site E. Scale is labeled in 1 cm intervals. carbonate bed Y bed X bed Z Figure S19. Tephra beds X, Y, and Z at site C. Scale is marked in 10 cm intervals. 12

sand sand bed W Figure S20. Tephra bed W at site C. Scale is marked in 10 cm intervals. carbonate bed U bed V Figure S21. Tephra beds U and V at site C. White card is 15 cm high and is labeled in 1 cm intervals. 13

Site F bed S bed T bed T0.5 bed T1 Figure S22. Tephra beds S through T1 at site F. S, T, and T1 form a recognizable set at all three sites. White card is 15 cm high and is labeled in 1 cm intervals. 14

Site F bed R bed R filled burrows bed R1 bed R1 bed R2 Site E bed R1 bed R1 bed R3 bed R2 bed R3 bed R2 ostracode sand ostracode sand Figure S23. Tephra beds R through R3 at sites C, E, and F. White card is 15 cm high and is labeled in 1 cm intervals. 15

Site F bed O bed P bed Q Figure S24. Tephra beds O, P, and Q at site F. Scale is labeled in 1 cm intervals. bed N2 bed N2 bed O Figure S25. Tephra bed N2 at site C. Scale is labeled in 1 cm intervals. 16

bed L1 ostracode sands over major unconformity Figure S26. Tephra bed L1 and unconformity at site C. Scale is labeled in 1 cm intervals. bed K bed L Figure S27. Tephra beds K and L at site C. Scale is marked in 10 cm intervals. 17

Site E bed J1 bed J1 bed J2 bed J2 bed J3 Figure S28. Tephra beds J1 through J3 at site E. White card in photo is 15 cm high. 18

bed I bed J Site E bed I1 bed I1 bed J bed J Figure S29. Tephra beds I, I1, and J at sites C and E. Yellow and black scale bar is marked in 10 cm intervals. White card is 15 cm high and is labeled in 1 cm intervals. 19

Site F bed 2 Figure S30. Tephra bed 2 at site F. Scale is labeled in 1 cm intervals. 20

bed 8 bed 4 bed 6 Site E bed 8 bed 6 bed 4 Site F Figure S31. Tephra beds 8, 6, 4, and H0.4. bed 8 White card in photo is 15 cm high and bed 4 bed 6 is labeled in 1 cm intervals. Beds 8, 6, 4, and 2 are among those found in both outcrop and the Wetland Levee core (Negrini et al., 2000). bed H0.4 21

additional eruption or redeposited tephra bed H0.2 Figure S32. Tephra bed H0.2 at site C. Scale is labeled in 1 cm intervals. 22

Site F bed 12 bed 12 bed H bed H bed H Figure S33. Tephra beds 12 and H. White card in upper photo is 15 cm high. Scale in lower photo is labeled in 1 cm intervals. 23

Site F bed 12 bed 12 bed 12 Figure S34. Tephra bed 12 at sites C and F. Scale in upper photo is labeled in 1 cm intervals. Scale in lower photos is marked in 10 cm and 1 cm intervals. 24

erosion sandy bed F sandy bed F sandy Site E bed F silt bed G Site F Figure S35. Tephra beds F, F1, and G. Scale in top and bottom photos is labeled in 1 cm intervals. Scale bed F silt bed F1 in middle photo is marked in 10 cm and 1 cm intervals. bed G 25

Site E bed D reworked tephra bed 18 bed E bed E1 bed E Figure S36. Tephra beds D, 18, E, and E1 at site E. Scale is labeled in 1 cm intervals. Note the cross-bedding in the reworked tephra at the top of bed 18. 26

Site E bed B bed C bed C bed C1 bed C1 bed C2 bed C2 bed D Figure S37. Tephra beds B, C, C1, C2, and D at site E. Scale is marked in 10 cm and 1 cm intervals. 27

Site E bed B bed A bed C bed B bed B1 bed B2 bed B1 bed C Figure S38. Tephra beds A, B, B1, B2, and C at the top of the section at site E. Scale is marked in 10 cm and 1 cm intervals. 28

Table S1 Tephrostratigraphy for site C Table S2 Tephrostratigraphy for site E Table S3 Tephrostratigraphy for site F Table S4. Complete microprobe data organized by bed and sample. Data points which appear as obvious outliers on bivariate plots are listed separately from the dominant population(s). Means calculated from multiple data points on a single shard are indicated in the far right column. Note also that the smaller data sets obtained for some samples may not fully capture the range of compositions present, especially for the more heterogeneous tephra beds. Together with limitations in the precision of EPMA data, this results in some variability in the range of values reported for individual samples. Mean values, which are based on a larger number of data points, tend to be less variable than compositional ranges. 29