Chapter 3K. Environmental Setting, Impacts, and Mitigation Measures - Cultural Resources
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Geologic Map of the Long Valley Caldera, Mono-Inyo Craters
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-1933 US. GEOLOGICAL SURVEY GEOLOGIC MAP OF LONG VALLEY CALDERA, MONO-INYO CRATERS VOLCANIC CHAIN, AND VICINITY, EASTERN CALIFORNIA By Roy A. Bailey GEOLOGIC SETTING VOLCANISM Long Valley caldera and the Mono-Inyo Craters Long Valley caldera volcanic chain compose a late Tertiary to Quaternary Volcanism in the Long Valley area (Bailey and others, volcanic complex on the west edge of the Basin and 1976; Bailey, 1982b) began about 3.6 Ma with Range Province at the base of the Sierra Nevada frontal widespread eruption of trachybasaltic-trachyandesitic fault escarpment. The caldera, an east-west-elongate, lavas on a moderately well dissected upland surface oval depression 17 by 32 km, is located just northwest (Huber, 1981).Erosional remnants of these mafic lavas of the northern end of the Owens Valley rift and forms are scattered over a 4,000-km2 area extending from the a reentrant or offset in the Sierran escarpment, Adobe Hills (5-10 km notheast of the map area), commonly referred to as the "Mammoth embayment.'? around the periphery of Long Valley caldera, and The Mono-Inyo Craters volcanic chain forms a north- southwestward into the High Sierra. Although these trending zone of volcanic vents extending 45 km from lavas never formed a continuous cover over this region, the west moat of the caldera to Mono Lake. The their wide distribution suggests an extensive mantle prevolcanic basement in the area is mainly Mesozoic source for these initial mafic eruptions. Between 3.0 granitic rock of the Sierra Nevada batholith and and 2.5 Ma quartz-latite domes and flows erupted near Paleozoic metasedimentary and Mesozoic metavolcanic the north and northwest rims of the present caldera, at rocks of the Mount Morrisen, Gull Lake, and Ritter and near Bald Mountain and on San Joaquin Ridge Range roof pendants (map A). -
Ephydra Hians) Say at Mono Lake, California (USA) in Relation to Physical Habitat
Hydrobiologia 197: 193-205, 1990. F. A. Comln and T. G. Northcote (eds), Saline Lakes. 193 © 1990 Kluwer Academic Publishers. Printed in Belgium. Distribution and abundance of the alkali fly (Ephydra hians) Say at Mono Lake, California (USA) in relation to physical habitat David B. Herbst Sierra Nevada Aquatic Research Laboratory, University of California, Star Route 1, Box 198, Mammoth Lakes, CA 93546, USA Key words: Ephydra, life cycle, development, distribution, Mono Lake, substrate Abstract The distribution and abundance of larval, pupal, and adult stages of the alkali fly Ephydra hians Say were examined in relation to location, benthic substrate type, and shoreline features at Mono Lake. Generation time was calculated as a degree-day model for development time at different temperatures, and compared to the thermal environment of the lake at different depths. Larvae and pupae have a contagious distribution and occur in greatest abundance in benthic habitats containing tufa (a porous limestone deposit), and in least abundance on sand or sand/mud substrates. Numbers increase with increasing area of tufa present in a sample, but not on other rocky substrates (alluvial gravel/cobble or cemented sand). Standing stock densities are greatest at locations around the lake containing a mixture of tufa deposits, detrital mud sediments, and submerged vegetation. Shoreline adult abundance is also greatest in areas adjacent to tufa. The shore fly (ephydrid) community varies in composition among different shoreline habitats and shows a zonation with distance from shore. The duration of pupation (from pupa formation to adult eclosion) becomes shorter as temperature increases. The temperature dependence of pupa development time is not linear and results in prolonged time requirements to complete development at temperatures below 20 ° C. -
Northern Paiute and Western Shoshone Land Use in Northern Nevada: a Class I Ethnographic/Ethnohistoric Overview
U.S. DEPARTMENT OF THE INTERIOR Bureau of Land Management NEVADA NORTHERN PAIUTE AND WESTERN SHOSHONE LAND USE IN NORTHERN NEVADA: A CLASS I ETHNOGRAPHIC/ETHNOHISTORIC OVERVIEW Ginny Bengston CULTURAL RESOURCE SERIES NO. 12 2003 SWCA ENVIROHMENTAL CON..·S:.. .U LTt;NTS . iitew.a,e.El t:ti.r B'i!lt e.a:b ~f l-amd :Nf'arat:1.iern'.~nt N~:¥G~GI Sl$i~-'®'ffl'c~. P,rceP,GJ r.ei l l§y. SWGA.,,En:v,ir.e.m"me'Y-tfol I €on's.wlf.arats NORTHERN PAIUTE AND WESTERN SHOSHONE LAND USE IN NORTHERN NEVADA: A CLASS I ETHNOGRAPHIC/ETHNOHISTORIC OVERVIEW Submitted to BUREAU OF LAND MANAGEMENT Nevada State Office 1340 Financial Boulevard Reno, Nevada 89520-0008 Submitted by SWCA, INC. Environmental Consultants 5370 Kietzke Lane, Suite 205 Reno, Nevada 89511 (775) 826-1700 Prepared by Ginny Bengston SWCA Cultural Resources Report No. 02-551 December 16, 2002 TABLE OF CONTENTS List of Figures ................................................................v List of Tables .................................................................v List of Appendixes ............................................................ vi CHAPTER 1. INTRODUCTION .................................................1 CHAPTER 2. ETHNOGRAPHIC OVERVIEW .....................................4 Northern Paiute ............................................................4 Habitation Patterns .......................................................8 Subsistence .............................................................9 Burial Practices ........................................................11 -
Insights Into Rhyolite Magma Dome Systems Based on Mineral and Whole Rock Compositions at the Mono Craters, Eastern California
ABSTRACT INSIGHTS INTO RHYOLITE MAGMA DOME SYSTEMS BASED ON MINERAL AND WHOLE ROCK COMPOSITIONS AT THE MONO CRATERS, EASTERN CALIFORNIA The Mono Craters magmatic system, found in a transtensional tectonic setting, consists of small magmatic bodies, dikes, and sills. New sampling of the Mono Craters reveals a wider range of magmatic compositions and a more complex storage and delivery system than heretofore recognized. Space compositional patterns, as well as crystallization temperatures and pressures taken from olivine-, feldspar-, orthopyroxene-, and clinopyroxene-liquid equilibria, are used to create a new model for the Mono Craters magmatic system. Felsic magmas erupted throughout the entire Mono Craters chain, whereas intermediate batches only erupted at Domes 10-12 and 14. Mafic magmas are spatially restricted, having erupted only at Domes 10, 12 and 14. Data from the new whole rock analyses illustrates a linear trend. Fractional crystallization does not replicate this trend but rather the linear trend indicates magma mixing. This study also analyzes samples from the Mono Lake Islands and the June Lake Basalts and compares them to the Mono Craters. Although the Mono Lake Islands fall into the intermediate to felsic group, they contain distinctly higher Al2O3 and Na2O at a given SiO2. Therefore, this study concludes that the Mono Craters represent a distinct magmatic system not directly related to the magmatic activity that created the Mono Lake Islands. Michelle Ranee Johnson May 2017 INSIGHTS INTO RHYOLITE MAGMA DOME SYSTEMS BASED -
A Diatom Proxy for Seasonality Over the Last Three Millennia at June Lake, Eastern Sierra Nevada (Ca)
University of Kentucky UKnowledge Theses and Dissertations--Earth and Environmental Sciences Earth and Environmental Sciences 2019 A DIATOM PROXY FOR SEASONALITY OVER THE LAST THREE MILLENNIA AT JUNE LAKE, EASTERN SIERRA NEVADA (CA) Laura Caitlin Streib University of Kentucky, [email protected] Digital Object Identifier: https://doi.org/10.13023/etd.2019.291 Right click to open a feedback form in a new tab to let us know how this document benefits ou.y Recommended Citation Streib, Laura Caitlin, "A DIATOM PROXY FOR SEASONALITY OVER THE LAST THREE MILLENNIA AT JUNE LAKE, EASTERN SIERRA NEVADA (CA)" (2019). Theses and Dissertations--Earth and Environmental Sciences. 70. https://uknowledge.uky.edu/ees_etds/70 This Master's Thesis is brought to you for free and open access by the Earth and Environmental Sciences at UKnowledge. It has been accepted for inclusion in Theses and Dissertations--Earth and Environmental Sciences by an authorized administrator of UKnowledge. For more information, please contact [email protected]. STUDENT AGREEMENT: I represent that my thesis or dissertation and abstract are my original work. Proper attribution has been given to all outside sources. I understand that I am solely responsible for obtaining any needed copyright permissions. I have obtained needed written permission statement(s) from the owner(s) of each third-party copyrighted matter to be included in my work, allowing electronic distribution (if such use is not permitted by the fair use doctrine) which will be submitted to UKnowledge as Additional File. I hereby grant to The University of Kentucky and its agents the irrevocable, non-exclusive, and royalty-free license to archive and make accessible my work in whole or in part in all forms of media, now or hereafter known. -
Biogeography and Physiological Adaptations of the Brine Fly Genus Ephydra (Diptera: Ephydridae) in Saline Waters of the Great Basin
Great Basin Naturalist Volume 59 Number 2 Article 3 4-30-1999 Biogeography and physiological adaptations of the brine fly genus Ephydra (Diptera: Ephydridae) in saline waters of the Great Basin David B. Herbst University of California, Mammoth Lakes and University of California, Santa Barbara Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Herbst, David B. (1999) "Biogeography and physiological adaptations of the brine fly genus Ephydra (Diptera: Ephydridae) in saline waters of the Great Basin," Great Basin Naturalist: Vol. 59 : No. 2 , Article 3. Available at: https://scholarsarchive.byu.edu/gbn/vol59/iss2/3 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Great Basin Naturalist 59(2), ©1999, pp. 127-135 BIOGEOGRAPHY AND PHYSIOLOGICAL ADAPTATIONS OF THE BRINE FLY GENUS EPHYDRA (DIPTERA: EPHYDRIDAE) IN SALINE WATERS OF THE GREAT BASIN David B. Herbst1 ABSTRACf.-Four species of the genus Ephydra are commonly found in saline waters within the hydrologic Great Basin: E. hians, E. gracilis, E. packardi, and E. auripes. Though none of these brine flies is endemic (distributions also occur outside the Great Basin), they all inhabit distinctive habitat types and form the characteristic benthic insect fauna ofinland saline-water habitats. The affinities ofeach species for different salinity levels and chemical compositions, and ephemeral to perennial habitats, appear to form the basis for biogeographic distribution patterns. -
Full Issue, Vol. 59 No. 2
Great Basin Naturalist Volume 59 Number 2 Article 16 4-30-1999 Full Issue, Vol. 59 No. 2 Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation (1999) "Full Issue, Vol. 59 No. 2," Great Basin Naturalist: Vol. 59 : No. 2 , Article 16. Available at: https://scholarsarchive.byu.edu/gbn/vol59/iss2/16 This Full Issue is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. T H E GREAT baslBASIBASIN naturalistNATURALI ST mot A VOLUME 59 NO 2 APRIL 1999 ML BEAN LIFE SCIENCE MUSEUM BRIGHAM YOUNG university GREAT BASIN naturalist httpwwwlibbyueduhttpwwwlibbyuedunmsamsnms FAX 8013783733801 378 3733 editor assistant editor richardwbaumannrighardRICHARD W BAUMANN NATHAN M SMITH 290 MLBM 190 MLBM PO box 20200 PO box 26879 brigham young university brigham young university provo UT 84602020084602 0200 provo UT 84602687984602 6879 8013785492801 378 5492 8013786688801 378 6688 emailE mail richarclbaumannbyuedurichardriehard baumannbyuedu emailE mail nathan smithbyuedu associate editors JAMES C CALLISON JR JERRY H SCRIVNER department of environmental technology department of biology utah valley state college ricks college orem UT 84058 redburgrexburgRexburg ID 83460110083460 1100 JEFFREY R JOHANSEN STANLEY D SMITH department of biology john carroll university -
Kutsavi, a Great Basin Indian Food
KUTSAVI, A GREAT BASIN INDIAN FOOD Robert F. Heizer When one becomes preoccupied with a topic or an area he ti apt to accumulate formidable piles of notee and references on cultural traits which are intriguing, but not highly significent. Often these accumu- lations evade utilization In the student's published works. The present note ts a by-product of a long and continuing interest in the archaeology and ethnology of the Great Basin, and because these data will probably never, to me have any particular significance, I offer them here in the hope that some other student may benefit from my literary gleanings. One of the most Interesting foods of tho Indians of the Intermon- tane-Platepu was kuteavi, the larva of a small fly (Ephydra hians Say) which was to be found from northern Neveda to Mono Lake on the eastern border of Celifornia. Native exploitation of this oconomic resource has been discusod by 0. Esslg (1) and J, Steward.(2) The present note will show the essential distribution of the use of Ephydra larvae ae. food. Among the earliest references to kutsavi collecttng at Mono Lake is that of Zenas Leonard in 1833. He BesY:k3) The water in ¾ihs lelke becomes stagnant and very disagreeable -- its surfece being covered with a green substence, similar to a. stagnant frog pond. In warm weether there is a. fly, about the size and similar to a grain of wheat, on this lake, in great num- bers. ... IWhen the wind rolls the waters onto the shore, these flies are left on the beech -- the female Indiens then carefully gether them into beekets made of willow .branches, and lay them exposed to the sun until they become perfectly dry, when theyg are laid away for winter provender. -
An Environmental History of the Mono Basin
Eastern Sierra History Journal Volume 2 Article 1 3-24-2021 Sheep Replace Pronghorn: An Environmental History of the Mono Basin Robert B. Marks Whittier College, [email protected] Follow this and additional works at: https://scholarship.claremont.edu/eshj Part of the Animal Studies Commons, Indigenous Studies Commons, Nature and Society Relations Commons, and the United States History Commons Recommended Citation Marks, Robert B. () "Sheep Replace Pronghorn: An Environmental History of the Mono Basin," Eastern Sierra History Journal: Vol. 2, Article 1. Available at: https://scholarship.claremont.edu/eshj/vol2/iss1/1 This Article is brought to you for free and open access by the Journals at Claremont at Scholarship @ Claremont. It has been accepted for inclusion in Eastern Sierra History Journal by an authorized editor of Scholarship @ Claremont. For more information, please contact [email protected]. Marks: Sheep Replace Pronghorn Sheep Replace Pronghorn: An Environmental History of the Mono Basin Robert B. Marks1 Environmental history examines the relationships of humans to the natural environment. It is concerned with understanding the environmental circumstances that condition the ways in which humans are able to obtain their subsistence, and the extent to which the ways they do so changes the environment. Sometimes humans have a very light, and ultimately sustainable, touch on the environment, and sometimes their environmental impact is heavy and not sustainable, threating the environmental underpinnings of human societies. To gauge the history of human impact on the environment, a major task is reconstructing past environments. Written sources are useful, but when they are missing or silent, archeological and paleobotanical findings can be used. -
Study Area Description Page 1 of 9
Study Area Description Page 1 of 9 Study Areas The pinyon-juniper and cheatgrass risk models were developed for 14 ecological provinces encompassing southeastern Oregon, southwestern Idaho, western Utah, all of Nevada, northeastern California, and a small portion of northwestern Arizona (fig. 1; Suring et al. 2005). The province boundaries, adapted from Bailey (1980) and Anderson et al. (1998), reflect attributes such as geologic age, lithology, regional climate, and potential natural communities (Anderson et al. 1998, West et al. 1998). We focused our initial model evaluation on the John Day and Mono Basin provinces, because they represent important but contrasting regions with respect to land ownership patterns, sagebrush and pinyon-juniper communities, and associated threats. Figure 1─Ecological provinces in the Intermountain West, adapted from Bailey (1980) and Anderson et al. (1998). John Day Ecological Province The John Day province extends across much of central and eastern Oregon, encompassing 3.5 x 106 ha of diverse habitats ranging from coniferous forests to expansive shrubsteppe (fig. 6). The area is mostly rural, with human populations centered at Bend, John Day, Madras, and Prineville. Two primary communities, intermix and interface, have been identified as part of the Wildland Urban Interface (WUI), defined as the area where structures and other human development meet or intermingle with undeveloped wildland (Radeloff et al. 2005). In the John Day province, intermix communities1 compose 1.7% (59,600 ha), whereas interface communities2 are less 1 Intermix communities are defined as places where housing and vegetation intermingle. In intermix, wildland vegetation is continuous, >50% vegetation, in areas with >1 house per 16 ha. -
Ecological Physiology of the Larvel Brine Fly Ephydra
AN ABSTRACT OF THE THESIS OF David Bruce Herbst for the degree of Master of Science in Zoology presented on May 22, 1980 Title: Ecological Physiology of the Larval Brine Fly Ephydra (Hydropyrus) hians, an Alkaline-Salt Lake Inhabiting Ephydrid (Diptera). Redacted for Privacy Abstract approved: (I, Anrr. Frank P. Conte Dipterans of the family Ephydridae (shore and brine flies) are well known for their ability to tolerate and thrive in a wide variety of physically harsh circumstances. The immature stages of one such species of this family, Ephydra hians, are characteristically limited in distribution as benthic inhabitants of highly alkaline salt lakes in the arid regions of western North America. In order to examine the nature of this habitat specificity, the intraspecific comparative physiologyof osmotic and ionic regulation, energy metabolism and survival was examined in two populations of brine fly larvae which differ inthe historical-environmental stability of their native habitats. The population at Mono Lake, California, has, until recent times, been evolving under relatively stable conditions of water chemistryand habitat availablility (i.e., little fluctuation in salinity or littoral benthic habitat due to stable lake level). Since 1940 however, the lake level has been steadily dropping and the dissolved salt content increasing due to diversion of tributary water. The population at Abert Lake, Oregon, has by contrast been subject to severeshort-term changes in salinity and habitat availability throughout its history.Larvae were exposed to both alkaline andnon-alkaline brines. While both populations displayed hyposmotic regulation in alkalinesalt media, Mono Lake larvae consistently showed more effective maintenanceof homeostasis. -
Mono and Southeastern Great Basin
3 •. .,• .{ • ,l<. • --• - • • •• 4:"."".. • 116 •,. California’s Botanical Landscapes - 3 chapter five Mono and Southeastern Great Basin The eastern fringe of California slices The crest of the Sierra Nevada defines Above: The crest of the Sierra off a thin strand at the edge of a vast the western hydrologic edge of the Great Nevada defines the western edge of interior biome, the Great Basin. Often Basin, within which waters drain into the Great Basin in central eastern California. The Mono Basin, characterized as an immense and homo interior basins. The entirety of the Sierra with its crown jewel Mono Lake, geneous sagebrush (Artemisia sp.) sea, Nevada was built by similar geologic exemplifies the character of the this region in fact encompasses great forces that created the Great Basin. The California part of this province, topographic, geologic, climatic, and vege narrative for vegetation in this chapter with expansive cold-adapted tative diversity, haunting in expansiveness starts with the lower montane (~2,500 m sagebrush steppe intermixed with hardy forbs and grasses. of landscape, surprising in richness of at the latitude of Mono Lake) and basin Robert Wick hidden canyons and wetlands. Long lines bottom environments of the eastern Opposite: A winter evening of basin and range draw the eye outward Sierra Nevada, and goes on to embrace along Hot Creek, with rubber to where land meets sky; wave after wave the entire elevation gradients from basin rabbitbrush and sagebrush of mountain ranges pounding the sage to summits of the mountain ranges east spread over rolling hills of the surf. If only a slice, California is fortunate ward to the California-Nevada state Long Valley Caldera.