GEOTECHNICAL REPORT Big Bend Hot Springs Project Big Bend, Shasta County, California

Total Page:16

File Type:pdf, Size:1020Kb

GEOTECHNICAL REPORT Big Bend Hot Springs Project Big Bend, Shasta County, California GEOTECHNICAL REPORT Big Bend Hot Springs Project Big Bend, Shasta County, California Prepared For: Big Bend Hot Springs Project, LLC TABLE OF CONTENTS GEOTECHNICAL REPORT BIG BEND HOT SPRINGS PROJECT BIG BEND, SHASTA COUNTY, CALIFORNIA 1.0 GENERAL................................................................................................................................................................. 1 1.1 PROJECT UNDERSTANDING............................................................................................................................ 1 1.2 STUDY PURPOSE ................................................................................................................................................. 1 1.3 PREVIOUS WORK PERFORMED ....................................................................................................................... 1 1.4 SCOPE OF SERVICES........................................................................................................................................... 2 2.0 FINDINGS ................................................................................................................................................................ 2 2.1 FIELD INVESTIGATION..................................................................................................................................... 2 2.2 SITE CONDITIONS.............................................................................................................................................. 3 2.2.1 Surface Conditions................................................................................................................................................... 3 2.2.2 Subsurface Conditions............................................................................................................................................... 3 2.3 GEOLOGIC CONDITIONS ................................................................................................................................. 4 2.3.1 Regional Geology ..................................................................................................................................................... 4 2.3.2 Local Geologic Setting .............................................................................................................................................. 5 2.3.3 Groundwater .......................................................................................................................................................... 5 3.0 GEOLOGICAL HAZARDS...................................................................................................................................... 6 3.1 GEOLOGIC HAZARD ZONES............................................................................................................................ 6 3.2 FAULTING & SEISMICITY .................................................................................................................................. 6 3.2.1 Seismic Setting ........................................................................................................................................................ 6 3.2.2 CBC Design Recommendations .................................................................................................................................. 7 3.3 LANDSLIDES........................................................................................................................................................ 7 3.4 LIQUEFACTION AND LATERAL SPREADING................................................................................................ 7 3.5 EXPANSIVE POTENTIAL ................................................................................................................................... 8 3.6 SOIL CHEMISTRY ................................................................................................................................................ 8 4.0 ENGINEERING PROPERTIES OF SIGNIFICANT EARTH MATERIALS................................................ 10 4.1 TERRACE DEPOSITS (ALLUVIUM).................................................................................................................. 10 4.2 COLLUVIUM....................................................................................................................................................... 10 5.0 CONCLUSIONS AND RECOMMENDATIONS............................................................................................... 11 5.1 GENERAL ........................................................................................................................................................... 11 5.2 FAULTING .......................................................................................................................................................... 11 5.3 LANDSLIDES...................................................................................................................................................... 11 5.4 LIQUEFACTION POTENTIAL.......................................................................................................................... 11 5.5 EXPANSIVE POTENTIAL ................................................................................................................................. 11 5.6 SITE PREPARATION AND GRADING ............................................................................................................ 11 5.6.1 Stripping.............................................................................................................................................................. 11 5.6.2 Existing Utilities, Wells, and/or Foundations ............................................................................................................ 12 5.6.3 Scarification and Compaction................................................................................................................................... 12 5.6.4 Keying and Benching .............................................................................................................................................. 12 5.6.5 Wet/Unstable Soil Conditions................................................................................................................................. 12 5.6.6 Site Drainage ...................................................................................................................................................... 13 5.6.7 Excavation Characteristics & Bulking...................................................................................................................... 13 5.6.8 Temporary & Permanent Slopes............................................................................................................................... 13 5.6.9 Overexcavation & Subdrains................................................................................................................................... 14 5.6.10 On-Site Soil Materials ....................................................................................................................................... 14 5.6.11 Imported Fill Materials - General......................................................................................................................... 14 5.6.12 Materials - Granular......................................................................................................................................... 15 5.6.13 Placement & Compaction ................................................................................................................................... 15 5.7 UTILITY TRENCHS AND TRENCH BACKFILL.............................................................................................. 15 5.7.1 Trenches and Dewatering......................................................................................................................................... 15 5.7.2 Pipe Zone Backfill................................................................................................................................................ 16 5.7.3 Trench Zone Backfill............................................................................................................................................. 16 5.7.4 Controlled Low Strength Backfill............................................................................................................................. 16 CGI: Copyright 2011 i CG11GR033 TABLE OF CONTENTS (continued) GEOTECHNICAL REPORT BIG BEND HOT SPRINGS PROJECT BIG BEND, SHASTA COUNTY, CALIFORNIA 5.7.5 Placement & Compaction ...................................................................................................................................... 16 5.7.6 Trench Subgrade Stabilization ................................................................................................................................. 17 5.7.7 Trench Plugs......................................................................................................................................................... 18 5.8 FOUNDATIONS ................................................................................................................................................. 18 5.8.1 Minimum Footing Embedment and Dimensions .......................................................................................................... 18 5.8.2 Allowable Bearing Capacity....................................................................................................................................
Recommended publications
  • CMS Serving American Indians and Alaska Natives in California
    Centers for Medicare & Medicaid Services Serving American Indians and Alaska Natives in California Serving American Indians and Alaska Natives Centers for Medicare & Medicaid Services (CMS) staff work with beneficiaries, health care providers, state government, CMS contractors, community groups and others to provide education and address questions in California. American Indians and Alaska Natives If you have questions about CMS programs in relation to American Indians or Alaska Natives: • email the CMS Division of Tribal Affairs at [email protected], or • contact a CMS Native American Contact (NAC). For a list of NAC and their information, visit https://go.cms.gov/NACTAGlist Why enroll in CMS programs? When you sign up for Medicaid, the Children’s Health Insurance Program, or Medicare, the Indian health hospitals and clinics can bill these programs for services provided. Enrolling in these programs brings money into the health care facility, which is then used to hire more staff, pay for new equipment and building renovations, and saves Purchased and Referred Care dollars for other patients. Patients who enroll in CMS programs are not only helping themselves and others, but they’re also supporting their Indian health care hospital and clinics. Assistance in California To contact Indian Health Service in California, contact the California Area at (916) 930–3927. Find information about coverage and Indian health facilities in California. These facilities are shown on the maps in the next pages. Medicare California Department of Insurance 1 (800) 927–4357 www.insurance.ca.gov/0150-seniors/0300healthplans/ Medicaid/Children’s Health Medi-Cal 1 (916) 552–9200 www.dhcs.ca.gov/services/medi-cal Marketplace Coverage Covered California 1 (800) 300–1506 www.coveredca.com Northern Feather River Tribal Health— Oroville California 2145 5th Ave.
    [Show full text]
  • Pit River and Rock Creek 2012 Summary Report
    Pit River and Rock Creek 2012 summary report October 9, 2012 State of California Department of Fish and Wildlife Heritage and Wild Trout Program Prepared by Stephanie Mehalick and Cameron Zuber Introduction Rock Creek, located in northeastern California, is tributary to the Pit River approximately 3.5 miles downstream from Lake Britton (Shasta County; Figure 1). The native fish fauna of the Pit River is similar to the Sacramento River and includes rainbow trout (Oncorhynchus mykiss sp.), sculpin (Cottus spp.), hardhead (Mylopharadon conocephalus), Sacramento sucker (Catostomus occidentalis), speckled dace (Rhinichthys osculus) and Sacramento pikeminnow (Ptychocheilus grandis; Moyle 2002). In addition, the Pit River supports a wild population of non-native brown trout (Salmo trutta). It is unknown whether the ancestral origins of rainbow trout in the Pit River are redband trout (O. m. stonei) or coastal rainbow trout (O. m. irideus) and for the purposes of this report, we refer to them as rainbow trout. The California Department of Fish and Wildlife Heritage and Wild Trout Program (HWTP) has evaluated the Pit River as a candidate for Wild Trout Water designation since 2008. Wild Trout Waters are those that support self-sustaining wild trout populations, are aesthetically pleasing and environmentally productive, provide adequate catch rates in terms of numbers or size of trout, and are open to public angling (Bloom and Weaver 2008). The HWTP utilizes a phased approach to evaluate designation potential. In 2008, the HWTP conducted Phase 1 initial resource assessments in the Pit River to gather information on species composition, size class structure, habitat types, and catch rates (Weaver and Mehalick 2008).
    [Show full text]
  • Shasta Lake Unit
    Fishing The waters of Shasta Lake provide often congested on summer weekends. Packers Bay, Coee Creek excellent shing opportunities. Popular spots Antlers, and Hirz Bay are recommended alternatives during United States Department of Vicinity Map are located where the major rivers and periods of heavy use. Low water ramps are located at Agriculture Whiskeytown-Shasta-Trinity National Recreation Area streams empty into the lake. Fishing is Jones Valley, Sugarloaf, and Centimudi. Additional prohibited at boat ramps. launching facilities may be available at commercial Trinity Center marinas. Fees are required at all boat launching facilities. Scale: in miles Shasta Unit 0 5 10 Campground and Camping 3 Shasta Caverns Tour The caverns began forming over 250 8GO Information Whiskeytown-Shasta-Trinity 12 million years ago in the massive limestone of the Gray Rocks Trinity Unit There is a broad spectrum of camping facilities, ranging Trinity Gilman Road visible from Interstate 5. Shasta Caverns are located o the National Recreation Area Lake Lakehead Fenders from the primitive to the luxurious. At the upper end of Ferry Road Shasta Caverns / O’Brien exit #695. The caverns are privately the scale, there are 9 marinas and a number of resorts owned and tours are oered year round. For schedules and oering rental cabins, motel accommodations, and RV Shasta Unit information call (530) 238-2341. I-5 parks and campgrounds with electric hook-ups, swimming 106 pools, and showers. Additional information on Forest 105 O Highway Vehicles The Chappie-Shasta O Highway Vehicle Area is located just below the west side of Shasta Dam and is Service facilities and services oered at private resorts is Shasta Lake available at the Shasta Lake Ranger Station or on the web managed by the Bureau of Land Management.
    [Show full text]
  • Area Adventure Hat Creek Ranger District Lassen National Forest
    Area Adventure Hat Creek Ranger District Lassen National Forest Welcome The following list of recreation activities are avail- able in the Hat Creek Recreation Area. For more detailed information please stop by the Old Station Visitor Information Center, open April - December, or our District Office located in Fall River Mills. Give Hat Creek Rim Overlook - Nearly 1 million years us a call year-around Mon.- Fri. at (530) 336-5521. ago, active faulting gradually dropped a block of Enjoy your visit to this very interesting country. the Earth’s crust (now Hat Creek Valley) 1,000 feet below the top of the Hat Creek Rim, leaving behind Subway Cave - See an underground cave formed this large fault scarp. This fault system is still “alive by flowing lava. Located just off Highway 89, 1/4 and cracking”. mile north of Old Station junction with Highway 44. The lava tube tour is self guided and the walk is A heritage of the Hat Creek area’s past, it offers mag- 1/3 mile long. Bring a lantern or strong flashlight nificent views of Hat Creek Valley, Lassen Peak, as the cave is not lighted. Sturdy Shoes and a light Burney Mountain, and, further away, Mt. Shasta. jacket are advisable. Subway Cave is closed during the winter months. Fault Hat Creek Rim Fault Scarp Vertical movement Hat Creek V Cross Section of a Lava Tube along this fault system alley dropped this block of earth into its present position Spattercone Trail - Walk a nature trail where volca- nic spattercones and other interesting geologic fea- tures may be seen.
    [Show full text]
  • Aspects of Pit River Phonology
    ASPECTS OF PIT RIVER PHONOLOGY Bruce E. Nevin A DISSERTATION in Linguistics Presented to the Faculties of the University of Pennsylvania in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy 1998 _____________________________ Supervisor of Dissertation _____________________________ Graduate Group Chairperson iii iv To the Pit River people In memory of Yámá·litwí·daá Dísdí sí·sá·dumá má céá suwí tús dit·é·wi, amxágam táxábáà tól·ím dáx cú wíc stíjéuwí?à Qa ßís ßú wóá dis·i ßuwá·géá ß tyánuwí,á toljana winá·ji·wíní. iii iv Abstract Aspects of Pit River Phonology Bruce Nevin Eugene Buckley Until recently, it has seemed that the Pit River language (“Achumawi”) was reasonably well documented by de Angulo & Freeland (1930), Uldall (1933), and Olmsted (1956, 1957, 1959, 1964, 1966). My own fieldwork in 1970-74 disclosed fundamental inadequacies of these publications, as reported in Nevin (1991). We substantiate this finding, investigate its probable bases, and establish why my own data are not subject to the same difficulties. After this cautionary tale about the perils of restating a published grammar, we define a phonemic representation for utterances in the language and introduce Optimality Theory (OT). We then apply OT to a series of problems in the phonological patterning of the language: features of syllable codas, restrictions and alternations involving voiceless release and aspiration, and reduplicative morphology. Appendix A describes the physiology and phonetics of laryngeal phenomena in Pit River, especially epiglottal articulation that has in the past been improperly described as pharyngeal or involving the tongue radix (the feature RTR).
    [Show full text]
  • From Valley to Valley
    From Valley to Valley DP 23 DP 24 DP 22 DP 21 ~ 48 ~ Emigration in Earnest DP 25 ~ 49 ~ Section 5, Emigration in Earnest ValleyFrom to Valley Emigration in Earnest Section 5 Discovery Points 21 ~ 25 Distance ~ 21.7 miles eventually developed coincides he valleys of this region closely to the SR 44 Twere major thoroughfares for route today. the deluge of emigrants in the In 1848, Peter Lassen and a small 19th century. Linking vale to party set out to blaze a new trail dell, using rivers as high-speed into the Sacramento Valley and to transit, these pioneers were his ranch near Deer Creek. They intensely focused on finding the got lost, but were eventually able quickest route to the bullion of to join up with other gold seekers the Sacramento Valley. From and find a route to his land. His trail became known as the “Death valley to valley, this land Route” and was abandoned within remembers an earnest two years. emigration. Mapquest, circa 1800 During the 1800s, Hat Creek served as a southern “cut-off” from the Pit River allowing emigrants to travel southwest into the Sacramento Valley. Imagine their dismay upon reaching the Hat Creek Rim with the valley floor 900 feet below! This escarpment was caused by opposite sides of a fracture, leaving behind a vertical fault much too steep for the oxen teams and their wagons to negotiate. The path that was Photo of Peter Lassen, courtesy of the Lassen County Historical Society Section 5, Emigration in Earnest ~ 50 ~ Settlement in Fall River and Big Valley also began to take shape during this time.
    [Show full text]
  • Land Stewardship Proposal for •Hat Creek Planning Unit • Organization
    Land Stewardship Proposal for •Hat Creek Planning Unit • Organization Pit River Tribe Part I. Organizational Information 1. Contact Information Proposal Contact First Name: Sophia Last Name: Villarruel Title: Environmental Coordinator Address: 36970 Park Ave City: Burney State: CA ZIP: 96013 Primary Telephone: (530) 335-1118 Secondary Telephone: (530) 335-5421 E-mail address: [email protected] 2. Executive Summary The Pit River Tribe is a Federally-recognized Tribe consisting of the original eleven autonomous bands that comprise the “100-mile square” ancestral boundary of the Pit River Nation, which is located in Shasta, Siskiyou, Modoc, and Lassen Counties, as stated in the Pit River Docket No. 347, (7 ICC 815 at 844), Indian Claims Commission, and Constitution of the Pit River Tribe, adopted by the Secretary of the Interior on August 16, 1964. Through this constitution, the Pit River Tribe has inherent sovereign governmental powers to protect and promote the health, safety, and/or general welfare of the people of the Pit River Tribe. For all Federal, State, and private agencies whose projects pertain to and are within the Tribe’s 100 square mile Ancestral Boundary; Pursuant to Section 2 of the Tribal Constitution: “The jurisdiction of the Tribe under this Constitution shall extend throughout its territory. Nothing in this Article shall be construed to limit the ability of the Pit River Tribe (Ajumawi-Atsugewi Nation) to exercise its jurisdiction to the fullest extent permitted by Federal law, including but not limited to lands, waters, properties, air space, fish and wildlife and other resources." The Fall River Mills, Fall River Valley is wholly inclusive in this boundary, and was the ancestral home from time immemorial of the Ajumawi Band; while the Hat Creek and Lake Britton planning units lie within the ancestral home of the Illmawi Band.
    [Show full text]
  • California Department of Forestry and Fire Protection Cal Fire
    CALIFORNIA DEPARTMENT OF FORESTRY AND FIRE PROTECTION CAL FIRE SHASTA – TRINITY UNIT FIRE PLAN Community Wildfire Protection Plan Mike Chuchel Unit Chief Scott McDonald Division Chief – Special Operations Mike Birondo Battalion Chief - Prevention Bureau Kimberly DeSena Fire Captain – Pre Fire Engineering 2008 Shasta – Trinity Unit Fire Plan 1 Table of Contents 1. EXECUTIVE SUMMARY.................................................................... 4 Unit Fire Plan Assessments and Data Layers................................................ 5 Fire Plan Applications...................................................................................... 6 Community Wildfire Protection Plan............................................................. 6 Unit Fire Plan Responsibilities........................................................................ 6 Key Issues .......................................................................................................... 7 2. STAKEHOLDERS................................................................................. 8 Fire Safe Organizations.................................................................................... 8 Resource Conservation Districts..................................................................... 9 Watershed Contact List ................................................................................... 9 Government Agencies..................................................................................... 13 3. UNIT OVERVIEW .............................................................................
    [Show full text]
  • Heritage Rank Status Factors
    Heritage Rank Status Factors Elcode IMGASG3110 Gname FLUMINICOLA SEMINALIS Gcomname NUGGET PEBBLESNAIL Number of Occurrences C = 21- 80 Comments Fluminicola seminalis is moderately common in the Pit and McCloud Rivers and their tributaries. Frest and Johannes collected it from 32 sites, in a confined portion of the Pit drainage. However, in a recent survey of 231 sites in the potential area of occurrence, Frest and Johannes (1995c) reported that they could not locate it in the Upper Sacramento system. Presumably, this species was recently extirpated by the Cantara Bend herbicide spill. Number of Occurrences with Good Viability B = Very few (1-3) occurrences with good viability Comments Frest and Johannes (1995c) recorded densities for Fluminicola seminalis at 2000-3000 per square mile in the Pit and McCloud Rivers. Under such circumstances, it may constitute the major invertebrate biomass at a site (Furnish and Monthey, 1999). Population Size F = 10,000-100,000 individuals Comments Frest and Johannes (1995c) recorded densities for Fluminicola seminalis at 2000-3000 per square mile in the Pit and McCloud Rivers. Under such circumstances, it may constitute the major invertebrate biomass at a site (Furnish and Monthey, 1999). Range Extent D = 1,000-5,000 km2 (about 400-2,000 square miles) E = 5,000-20,000 km2 (about 2,000-8,000 square miles) Comments Currently found in the Pit and McClound rivers, California. Formerly known from the mainstem Sacramento River in California, from its mouth upstream to Pit River, including large spring-fed tributaries (Taylor, 1981). Likely extinct from the mainstem Sacramento River (Hershler and Frest, 1996).
    [Show full text]
  • Achumawi, Achomawi, Or the Pit River People
    Zachary Berger Questionnaire—Antrho 2340 1. Description 1.1 Name of society, language, and language family: o Name: Achumawi, Achomawi, or the Pit River People. o Language: Achomawi. o Language family: Palaihnihan language family. 1.2 ISO code (3 letter code from ethnologue.com): o acv 1.3 Location (latitude/longitude): o Northeastern California: N40°38’51.36” W121°32’48.48” 1.4 Brief history: o The Achumawi—or Pit River People as they have come to be called—live in Northeastern California. Although they are now almost fully Westernized, they used to be seasonal nomads who dispersed to hunt, gather, and forage in the warmer seasons, and would congregate into villages during the winter. There are from 10 to 12 separate groups of Achumawi, all of whom are loosely associated through familial ties and trade. As were many other California hunter-gatherer tribes, the Achumawi were an easy going people and were not very warlike. This changed as Western settlers increased inter-tribe tensions, and the Achumawi came to have a bitter relationship with their neighbors at the end of the nineteenth century, especially the Modoc tribe (1p21). Unfortunately, most studies on the Achumawi only occurred after they had become at least partially Westernized. In fact, the most popular source over the Achumawi refers to them as “the Indians in overalls.” For that reason, any information in this questionnaire regarding the Achumawi prior to contact with the West was either recorded from the memory of older Achumawi in the early twentieth century or spread by word of mouth amongst the tribe.
    [Show full text]
  • PATTERNS of PREHISTORY on the Mccloud RIVER Elaine
    PATTERNS OF PREHISTORY ON THE McCLOUD RIVER Elaine Sundahl Shasta College Archaeology Laboratory Redding, California 96049-6006 ABSTRACT The lower McCloud River is well-known in the archaeological literature for its contribution to the definition of the "Shasta Complex," the archaeological assemblage and traits of the late-prehistoric Wintu. Recent archaeological investigations on the middle and upper McCloud by the Shasta-Trinity National Forest have revealed a much more diverse picture of prehistory along the river, covering at least a 5000 year period. This paper provides an introduction to the area and summarizes recent excavations. INTRODUCTION more impervious geologic formations of the Klamath Mountains, the underground reservoir The McCloud River is a major tributary to the bubbles to the surface in numerous springs to Sacramento-Pit River system, the confluence of form the upper McCloud River. The very cold. which is now inundated within Shasta Lake (Figure constant waters produced by the springs attracted 1). Much of the McCloud River has remained large runs of anadromous fish (Macdonald 1966; relatively undeveloped as large tracts of land are Haski ns 1993). owned by private fishing clubs, the Nature Conservancy, and timber companies. The term "upper McCloud" will be used in the Consequently. until the last decade, there has following paper to describe that portion of the river been very little archaeological investigation. The which primarily flows east to west along the contact major exception is the lowest portion of the river between the Cascades and Klamath Mountains; which was investigated in the early 1940s in the "middle McCloud" is that part that flows preparation for the construction of Shasta Dam.
    [Show full text]
  • Rosten, Lyn, K. True, E. Wiseman, K
    National Wild Fish Health Survey California-Nevada Fish Health Center Annual Report for fiscal year 2005 National Wild Fish Health Survey Annual Progress Report FY 2005 Prepared by Lyn Rosten and Kimberly True California-Nevada Fish Health Center Center staff conducted the National Wild Fish Health Survey (NWFHS) in the 2004/2005 fiscal year by collecting fish tissue samples and performing laboratory tests for major fish pathogens in accordance with standardized procedures (NWFHS Laboratory Procedures Manual – 2005, ). This data is entered into a national database and is accessible to the public and resource managers, via the web, and can be viewed at: http://wildfishsurvey.fws.gov/ or http://www.esg.montana.edu/nfhdb/ Kimberly True, Assistant Project Leader Lyn Rosten, Biological Science Technician Eric Wiseman, Fishery Biologist Ken Nichols, Fishery Biologist Scott Foott, Project leader Ron Stone, Fishery Biologist Also assisted with field collections and lab work. 2 Abstract The National Wild Fish Survey (NWFHS), conducted by the U.S. Fish and Wildlife Service’s Fish Health Centers, assesses the prevalence and distribution of major fish pathogens in wild fish populations. In 2004-2005, the California-Nevada Fish Health Center (Ca-Nv FHC) focused on disease monitoring in the upper Klamath River basin. Pathogens associated with diseased fish in the Klamath River include bacteria (Flavobacterium columnare and motile aeromonad bacteria), digenetic trematode (presumptive Nanophyetus salmincola) and myxozoan parasites (Parvicapsula minibicornis and Ceratomyxa shasta). The incidence of two parasites Ceratomyxa shasta and Parvicapsula minibicornis in juvenile chinook salmon is of special concern. Another focus in 2004-2005 was done in collaboration with Nevada Division of Wildlife’s regional biologists.
    [Show full text]