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Sedimentation in area of Diversion Dam, Figueredo Wash, New Mexico PDF

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SEDIMENTATION IN AREA OF DIVERSION DAM, FIGUEREDO WASH, NEW MEXICO A Thesis Presented To The Faculty of the Department of Geology University of Southern California In Partial Fulfillment of the Requirements for the Degree Master of Science By James E. Slosson June 1950 UMI Number: EP58432 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMI Dissertation Publishing UMI EP58432 Published by ProQuest LLC (2014). Copyright in the Dissertation held by the Author. Microform Edition © ProQuest LLC. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106 - 1346 This thesis, written by ......Jame s.. Edward.. Slo.s s on....... under the guidance of h%JSi... Faculty Committee, and approved by all its members, has been presented to and accepted by the Council on Graduate Study and Research in partial fulfill­ ment of the requirements for the degree of Master of Science Faculty Committee hairman NOTE: The author wishes to explain that the ideas and conclusions put forth in this paper are his own and do not, in any way, reflect those of any govern­ mental agency* It should also be understood that the auther did the actual writing of this report after his official service with the United States Geological Sur­ vey had been completed. TABLE OF CONTENTS Page Abstract...................... . ........... 1 Introduction ........................ 1 Acknowledgements ........... 3 Geography and Physiography • • • • • • • • • • • 5 General Geology............ 5 Stratigraphy. • • • • • • • • • • • • • • • . 6 Historical Geology............ 9 Climate and Vegetation . . . . . ............. 10 Methods........... 11 Field................................... 11 Laboratory............................... 13 Distribution of Grain Sizes............ 18 Effect of Vegetation on Deposition . ....... 26 Relationship to Deposition in Larger Areas . . . 27 Conclusions. . . . . . . . . . . . 28 Bibliography . . . ....... • • • • • • • • • • 30 LIST OF TABLES Page Table No. 1. Summary of Data - Size Analysis 45, 46, 47, 4& Table No. 2. Probable Error of Estimate, Wetted and Dried, 6 Hour-10 Minute. . . . . 49 Table No. 3. Probable Error of Estimate, Wetted and Dried, 40 Second . . . . . . . . 5 0 Table No. 4. Probable Error of Estimate, Natural State, 6 Hour-10 Minute............ 51 Table No. 5* Probable Error of Estimate, Natural State, 40 Second .......... 52 Table No. 6. Least-square Trend Line, Wetted and Dried, 6 Hour-10 Minute......... • 53 Table No. 7* Least-square Trend Line, Wetted and Dried, 40 Second ......... . . . . 5 4 Table No. &. Least-square Trend Line, Natural State, 6 Hour-10 Minute............ 55 Table No. 9• Least-square Trend Line, Natural State, 40 Second . . . . . . . . . . 5 6 Table No. 10. Standard Deviation • * ............57 Table No. 11. Suspended Samples. .............5# Table No. 12. Size Analysis for Surface Samples. . 59 Table No. 13* Profile Gradients. • ............ 60 LIST OF FIGURES Page Figure No- 1. Soil auger disassembled. . . . . . 3# Figure No. 2. Soil auger in use................. 3$ Figure No. 3* Integrated stream sampler assembled........................ 39 Figure No. 4* Integrated stream sampler disassembled ......... . . . . . 39 Figure No. 5- Area of dam fill................. 40 Figure No. 6. Photograph taken from old Figueredo Wash channel, looking toward the dam...................40 Figure No. 1* Photograph taken from dam looking downstream in old channel......... 41 Figure No. 3. Photograph taken near Station 140. 41 Figure No. 9* Pediment remnant located in vicinity 42 Figure No. 10. Photograph taken from old Figueredo Wash channel approximately one mile downstream from dam. . . . . . . . 1+2 Figure No. 11. Photograph of downstream portion of the old Figueredo channel • • • • . 43 Figure No. 12. Mud cracks formed after flood in present channel...................43 Figure No. 13. Round mud balls formed in meander­ ing portion of new channel . . . . 44 Figure No. 14 Oblong mud ball formed in straight portion of new channel . . . . . . 44 LIST OF GRAPHS Page Graph 1 Correlation of Air-dry Moisture and Percent in Suspension for Wetted Samples 61, 62 Graph 2 Correlation of Air-dry Moisture and Percent in Suspension for Samples in Natural State........... 63, 64 Graph 3 Graphic Presentation of Table No. 1* • • 65, 66, Graph 4 Profile Down Channel, Stratification Overlay. •• ................. . . • . 6& Graph 5 Profile A-A,tf and Profile South of Dam, Stratification Overlay ............... 69 Graph 6 Profile 11, Profile B-Bf11 and Profile C-Cff,, Stratification Overlay ....... 70 Graph 7 Profile 7 and 9, Stratification Overlay. 71 Graph 8 1 Suspended Samples. . . . . . . . . . . . 7 2 LIST OF MAPS Map No. 1. Topographic and Index Map. . . in folder Map No. 2. Planimetric Map. • • • • • • • in folder SEDIMENTATION IN AREA OF DIVERSION DAM FIGUEREDO NASH, NEW MEXICO By James.E* Slosson ABSTRACT This report describes a large diversion dam on one of the intermittent streams in New Mexico and attempts to out­ line the type of alluvial deposition that has and is taking place. It is pointed out that due to various local conditions the deposition here is not identical to that of large alluvial fans. Of these local conditions, the type and direction of stream flow together with the lithology of the source area seems to be the most important. A rapid but accurate method for sed­ iment analysis is discussed. This method entails using the per­ centage of moisture retained by each of the sediment samples for calculating the percent of sand, silt, and clay* INTRODUCTION Since 1880 there has been considerable wasting away of valuable range and agricultural lands in the southwest portion of the United States, and in 1933 the United States Soil Conservation Service began a series of investigations to determine the causes of the problem. In order to deter­ mine methods of reducing the rapid removal of valuable soils, the Soil Conservation Service established one of its first experiment stations at Mexican Springs, New Mexico, located in the southeastern portion of the Navajo Indian Reservation.

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