The South Bay Salt Pond Restoration Project
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William Furmval, H. E. Falk and the Salt Chamber of Commerce, 1815-1889: "Ome Chapters in the Economic History of Cheshire
WILLIAM FURMVAL, H. E. FALK AND THE SALT CHAMBER OF COMMERCE, 1815-1889: "OME CHAPTERS IN THE ECONOMIC HISTORY OF CHESHIRE BY W. H. CHALONER, M.A., PH.D. Read 17 November 1960 N the second volume of his Economic History of Modern I Britain (p. 145), Sir John Clapham, writing of the chambers of commerce and trade associations which multiplied rapidly after 1860, suggested that between 1850 and 1875 "there was rather less co-operation among 'capitalist' producers than there had been in the more difficult first and second quarters" of the nineteenth century. He mentioned that in the British salt industry there had been price-fixing associations "based on a local monopoly" in the early nineteenth century, and added that after 1825 the industry "witnessed alternations of gentle men's agreements and 'fighting trade' " until the formation of the Salt Union in 1888. This combine has been called "the first British trust", but to the salt proprietors of the time it was merely "a new device, made easier by limited liability, for handling an old problem". (1) The purpose of this study is to examine in greater detail the business organisation of the natural local monopoly enjoyed by the Cheshire saltmakers in the nineteenth century and to trace the part played by "The Coalition" and the Salt Chamber of Commerce in fostering price regulation and output restriction between the end of the Napoleonic Wars and 1889.< 2 > 111 Op. cit., pp. 147-8; see also Accounts and Papers, 1817, III, 123, p. 22, and E. Hughes, Studies in Administration and Finance, 1558-1825 (1934), pp. -
The Changing Technology of Post Medieval Sea Salt Production in England
1 Heritage, Uses and Representations of the Sea. Centro de Investigação Transdisiplinar Cultura, Espaço e Memoría (CITCEM) Porto, Faculdade de Letras da Universidade do Porto, 20-22 October 2011. The changing technology of post medieval sea salt production in England Jeremy Greenwood Composition of seawater Sea water contains 3.5% evaporites of which salt (sodium chloride) comprises 77.8%. The remainder is known as bittern as it includes the bitter tasting, aperient and deliquescent sulphates of magnesium (Epsom salt) and sodium (Glauber’s salt) as well as about 11% magnesium chloride. 2 Successful commercial salt making depends on the fractional crystallisation of seawater producing the maximum amount of salt without contamination by bittern salts. As seawater is evaporated, very small amounts of calcium carbonate are precipitated followed by some calcium sulphate. This is followed by the crystallisation of sodium chloride but before this is complete, bitter Epsom salt appears; something that needs to be avoided.1 In Continental Europe, evaporation of sea water is achieved solely by the energy of the wind and sun but this is not possible in the English climate so other techniques were developed. 1 http://www.solarsaltharvesters.com/notes.htm SOLAR SALT ENGINEERING 3 Evaporation vessel Briquetage The earliest known English method of coastal saltmaking has been found in the late Bronze Age. This involved boiling seawater in crude clay dishes supported by clay firebars (briquetage) and was widespread in Europe. This technique continued into the Iron Age and into the Roman period with variations inevitably occurring in the industry, although the dating of saltworks is very problematical.2 Detailed interpretation continues to be a matter of dispute. -
A Survey of Inbenthic Macrofauna at a South San Francisco Bay Salt Marsh Brian T
San Jose State University SJSU ScholarWorks Master's Theses Master's Theses and Graduate Research 1996 A Survey of inbenthic macrofauna at a South San Francisco Bay salt marsh Brian T. Pittman San Jose State University Follow this and additional works at: http://scholarworks.sjsu.edu/etd_theses Recommended Citation Pittman, Brian T., "A Survey of inbenthic macrofauna at a South San Francisco Bay salt marsh" (1996). Master's Theses. 1398. http://scholarworks.sjsu.edu/etd_theses/1398 This Thesis is brought to you for free and open access by the Master's Theses and Graduate Research at SJSU ScholarWorks. It has been accepted for inclusion in Master's Theses by an authorized administrator of SJSU ScholarWorks. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript bas been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. -
Active Surface Salt Structures of the Western Kuqa Fold-Thrust Belt, Northwestern China
Active surface salt structures of the western Kuqa fold-thrust belt, northwestern China Jianghai Li1, A. Alexander G. Webb2,*, Xiang Mao1, Ingrid Eckhoff2, Cindy Colón2, Kexin Zhang2, Honghao Wang1, An Li2, and Dian He2,† 1The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China 2Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70803, USA ABSTRACT fold-thrust belt display a variety of erosion- dynamics of salt motion. Although geo scientists tectonics interactions, with nuances refl ect- have interpreted thousands of salt sheets in The western Kuqa fold-thrust belt of Xin- ing the low viscosity and high erodibility of more than 35 basins worldwide (Hudec and jiang Province, China, hosts a series of surface salt, including stream defl ections, potential Jackson, 2006, 2007), subaerial preservation of salt structures. Here we present preliminary tectonic aneurysm development, and even halite salt structures is rare (Talbot and Pohjola, analysis of the geometry, kinematics, and sur- an upper-crustal test site for channel fl ow– 2009; Barnhart and Lohman, 2012). A fraction face processes of three of these structures: the focused denudation models. of these subaerial salt structures occur in active Quele open-toed salt thrust sheet, Tuzima- settings, where boundary conditions of ongoing zha salt wall, and Awate salt fountain. The INTRODUCTION deformation can be geodetically characterized. fi rst two are line-sourced, the third appears The Kuqa fold-thrust belt of Xinjiang Prov- to be point-sourced, and all are active. The Among common solid Earth materials, salt is ince, northwestern China, offers a new prospect ~35-km-long, 200-m-thick Quele open-toed distinguished by uncommonly low density, low for subaerial investigation of a range of active salt thrust sheet features internal folding, viscosity, near incompressibility, high solubil- salt structures. -
Ventures in Salt: Compass Minerals International Rebecca M
08-064 July 10, 2009 Ventures in Salt: Compass Minerals International Rebecca M. Henderson, John Sterman, Ramana Nanda As Michael Ducey, the President and CEO of Compass Minerals International, looked out of his office in Overland Park, Kansas on the evening of December 11, 2003, he wondered how investors would react to his company going public. Ducey had joined Compass Minerals in April 2002 as CEO and strategic investor, a few months after the private equity firm Apollo Management had acquired it from IMC Global.1 Although salt companies were not typical candidates for IPOs, Compass Minerals had done very well in its two years as a stand-alone firm, and Ducey had encouraged his fellow investors to consider exiting via an IPO. With Goldman Sachs leading its IPO the following day, Ducey considered the response of investors and his strategy going forward. Where should he be focusing his attention? How could he ensure that the company lived up to the high expectations of its investors? A Short History of Salt Salt was one of the most widely used minerals in the world. Although it had thousands of applications, in the United States it was primarily used for highway deicing, and as an input into the chemicals, food-processing, water-treatment, and agricultural industries. 1 Although some parts of the current operations of Compass Minerals go back over a hundred years, its most recent structure arose from a series of ownership changes that began in 1998. On April 1, 1998 IMC Global purchased the salt and chemicals businesses of Harris Chemical Group ($450 MM in cash and $950 MM raised in debt), including the North American Salt Company, the Great Salt Lake Minerals Corp in the US, and Salt Union in the UK. -
Salt Marsh Harvest Mice, Urban Development, and Rising Sea Levels Author(S): Howard S
Society for Conservation Biology Salt Marsh Harvest Mice, Urban Development, and Rising Sea Levels Author(s): Howard S. Shellhammer Source: Conservation Biology, Vol. 3, No. 1 (Mar., 1989), pp. 59-65 Published by: Wiley for Society for Conservation Biology Stable URL: https://www.jstor.org/stable/2385990 Accessed: 19-11-2018 23:28 UTC JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms Society for Conservation Biology, Wiley are collaborating with JSTOR to digitize, preserve and extend access to Conservation Biology This content downloaded from 216.73.253.254 on Mon, 19 Nov 2018 23:28:28 UTC All use subject to https://about.jstor.org/terms Salt Marsh Harvest Mice, Urban Development, and Rising Sea Levels HOWARD S. SHELLHAMMER Department of Biological Sciences San Jose State University 1 Washington Square San Jose, California 95192-0100, U.S.A. Abstract: The salt marsh harvest mouse, Reithrodontomys Resumen: El roedor recolector de sal Reithrodontomys ra- raviventris, is endemic to the marshes of San Francisco Bay. viventris es endemico a las marismas de la Bahia de San Ultimate factors such as rising sea level and tectonic -
Regional Oral History Off Ice University of California the Bancroft Library Berkeley, California
Regional Oral History Off ice University of California The Bancroft Library Berkeley, California California Land-Use Planning Series SAVE SAN FRANCISCO BAY ASSOCIATION, 1961-1986 with an Introduction by Harold Gilliam and an Afterword by Me1 Scott Interviews with Barry Bunshoft Esther Gulick Catherine Kerr Sylvia McLaughlin Interviews conducted by Malca Chall 1985 and 1986 Copyright @ 1987 by The Regents of the University of California This manuscript is made available for research purposes. No part of the manuscript may be quoted for publication without the written permission of the Director of The Bancroft Library of the Univer- sity of California at Berkeley. Requests for permission to quote for publication should be addressed to the Regional Oral History Office, 486 Library, and should include identification of the specific passages to be quoted, anticipated use of the passages, and identification of the user. It is recommended that this oral history be cited as follows: To cite the volume: Save San Francisco Bay Association, 1961-1986, an oral history conducted in 1985 and 1986 by Malca Chall, Regional Oral History Office, The Bancroft ~ibrar~, University bf calif ornia, Berkeley, 1987. To cite individual interview: Barry Bunshoft, "Save San Francisco Bay Association and the Courts," an oral history conducted in 1986 by Malca.Chal1, Regional Oral History Office, The Bancroft Library, University of California, Berkeley, 1987. Copy No. DEDICATION THE SAVE SAN FRANCISCO BAY ASSOCIATION DEDICATES THIS ORAL HISTORY TO THE MEMORY OF DOROTHY -
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M E M O R A N D U M TO: South Bay Salt Pond Restoration Project Management Team FROM: EDAW DATE: August 24, 2005 RE: Final Cultural Resources Assessment Strategy Memorandum 1. EXECUTIVE SUMMARY This memorandum describes the cultural resources assessment strategy for the South Bay Salt Pond (SBSP) Restoration Project. Since the 1980s, a new movement within the historic preservation field has focused on protection of cultural landscapes, in addition to individual sites or buildings. The cultural landscape approach considers multiple types of resources—structures as well as landscape features like roads, vegetation patterns, and land uses—as forming an integrated whole, representing the continuing interaction between people and place. The SBSP Restoration Project, aimed at restoring up to 15,000 acres of managed industrial salt production ponds in the San Francisco Bay to a more natural mix of tidal wetland habitats and managed ponds, involves a similar approach to incorporating cultural and historic resource issues into a project otherwise dominated by biological and hydrological variables. By providing a holistic overview of the area's changing historic character, the cultural landscape assessment can help members of the public better understand the need for the project, and provide a context for the proposed changes. It also will provide information for historic and cultural interpretation along the trails, even as the landscape shifts toward its original ecological form and function through marshland restoration. 2. INTRODUCTION This memorandum presents a strategy for integrating cultural resources into the SBSP Restoration Project. It draws on historical material presented in the attached Historic Context Report. -
Abundance and Distribution of Shorebirds in the San Francisco Bay Area
WESTERN BIRDS Volume 33, Number 2, 2002 ABUNDANCE AND DISTRIBUTION OF SHOREBIRDS IN THE SAN FRANCISCO BAY AREA LYNNE E. STENZEL, CATHERINE M. HICKEY, JANET E. KJELMYR, and GARY W. PAGE, Point ReyesBird Observatory,4990 ShorelineHighway, Stinson Beach, California 94970 ABSTRACT: On 13 comprehensivecensuses of the San Francisco-SanPablo Bay estuaryand associatedwetlands we counted325,000-396,000 shorebirds (Charadrii)from mid-Augustto mid-September(fall) and in November(early winter), 225,000 from late Januaryto February(late winter); and 589,000-932,000 in late April (spring).Twenty-three of the 38 speciesoccurred on all fall, earlywinter, and springcounts. Median counts in one or moreseasons exceeded 10,000 for 10 of the 23 species,were 1,000-10,000 for 4 of the species,and were less than 1,000 for 9 of the species.On risingtides, while tidal fiats were exposed,those fiats held the majorityof individualsof 12 speciesgroups (encompassing 19 species);salt ponds usuallyheld the majorityof 5 speciesgroups (encompassing 7 species); 1 specieswas primarilyon tidal fiatsand in other wetlandtypes. Most speciesgroups tended to concentratein greaterproportion, relative to the extent of tidal fiat, either in the geographiccenter of the estuaryor in the southernregions of the bay. Shorebirds' densitiesvaried among 14 divisionsof the unvegetatedtidal fiats. Most species groups occurredconsistently in higherdensities in someareas than in others;however, most tidalfiats held relativelyhigh densitiesfor at leastone speciesgroup in at leastone season.Areas supportingthe highesttotal shorebirddensities were also the ones supportinghighest total shorebird biomass, another measure of overallshorebird use. Tidalfiats distinguished most frequenfiy by highdensities or biomasswere on the east sideof centralSan FranciscoBay andadjacent to the activesalt ponds on the eastand southshores of southSan FranciscoBay and alongthe Napa River,which flowsinto San Pablo Bay. -
Identification and Evaluation of the South San Francisco Bay Solar Salt Industry Landscape (Alameda, Santa Clara, and San Mateo Counties, California)
APPENDIX E: Identification and Evaluation of the South San Francisco Bay Solar Salt Industry Landscape (Alameda, Santa Clara, and San Mateo Counties, California) For the Don Edwards San Francisco Bay National Wildlife Refuge and California Department of Fish and Game Archimedes Screw pumps, Oliver Salt Works, Eden Landing, view to S (2007-12-01:57). By Lou Ann Speulda-Drews and Nicholas Valentine U.S. Fish and Wildlife Service Region 8 Sacramento, California March 9, 2009 Introduction The South Bay Salt Pond Restoration Project’s (SBSPRP) goal is to convert the heavily modified environment of the solar salt industry back to native salt marsh. The restoration is focused on portions of San Mateo, Santa Clara, and Alameda Counties, and comprises approximately 15,100 acres of former salt ponds located around the edge of South San Francisco Bay. The SBSPRP encompasses property managed by the U.S. Fish and Wildlife Service (USFWS) and the California Department of Fish and Game (DFG). The agencies are working together along with the California State Coastal Conservancy (Conservancy) and U.S. Army Corps of Engineers (USACE) to develop a cohesive approach to restoration and complying with Section 106 of the National Historic Preservation Act (NHPA). The project overlaps five USGS 7.5’ topographical quadrangle maps: Newark, Redwood Point, Palo Alto, Milpitas, and Mountain View. The SBSPRP’s goal is to restore the industrial salt production ponds in South San Francisco Bay to a more natural mix of tidal wetland habitats and managed ponds. The SBSPP is composed of three noncontiguous units, including Eden Landing on the east side of the Bay near the San Mateo bridge; the Alviso unit at the southern end of the bay; and the West Bay-Ravenswood unit located on the west side of the Bay near the Dumbarton Bridge (Figure 1 and Appendix A). -
1. Introduction: Salt, Sodium Chloride, Has Probably Been with Us from The
1. Introduction: Salt, sodium chloride, has probably been with us from the beginnings of geologic time, and has been necessary directly or indirectly through all stages of evolution of living things. The first oceans undoubtedly contained traces of salt, and our unicellular ancestors first appeared and thrived in this salty marine environment. In the process of evolution, these unicellular ancestors became multi-cellular, and some left their salty marine environment but still required salt. Our herbivorous ancestors used salt licks, and our carnivorous ones obtained their salt form the flesh and blood of their prey. This demand is necessity of/or all living for things for salt in one form or another continues today.Our bodies contain relatively large quantities of salt, as we may infer from the taste of “blood, sweat, and tears.”(Dalf.w.Knutmann, 1971) Salt, NaCl, is a chemical compound made of sodium and chloride which has been exceptionally important to humans for thousands of years, because it is one of the substances upon which all of life evolved to depend. Humans, like all life, need a supply of salt in order to simply survive. Salt's ability to preserve food was a foundation of civilization. It helped to eliminate the dependence on the seasonal availability of food and it allowed travel over long distances. However, salt was difficult to obtain, and so it was a highly valued trade item to the point of being considered a form of currency by certain peoples. Many salt roads, such as via salaria in Italy, had been established by the Bronze Age. -
The Rise and Fall of the Marshalls of Northwich, Salt Proprietors: a Saga of the Industrial Era in Cheshire, 1720-1917
THE RISE AND FALL OF THE MARSHALLS OF NORTHWICH, SALT PROPRIETORS: A SAGA OF THE INDUSTRIAL ERA IN CHESHIRE, 1720-1917 BY D. A. IREDALE, M.A., PH.D. HEN Thomas Marshall from the Hartford Beach, near WNorthwich, appeared before a parliamentary committee in London in 1817, he proudly proclaimed himself the largest salt proprietor in the kingdom. The wealthiest merchant in mid-Cheshire, Marshall determined that his family should one day sit on committees and at table with the greatest in the land. To this end he sent his son to Eton, Cambridge, and the Middle Temple. And his grandson did indeed climb towards the highest levels of society. I FOUNDING THE FAMILY FORTUNE During the seventeenth century the Marshalls lived in Nant- wich. They began business as shoemakers, then as framework knitters. By hard work they grew prosperous, so that when Richard Marshall died in 1692 the family owned a fine "dwelling house in the welshrow" and valuable textile machinery. But living in one of Cheshire's salt towns, the family naturally acquired a "wich-house & twelve leads walling", that is, equip ment for raising and boiling brine to produce salt. Salt had long been valued as a preservative and seasoner of food by the fisheries and the navy, by dairy farmers and every housewife, but during the industrial age it was to become an important raw material in the glass, soap, and chemical industries. To invest in salt, therefore, was to plan sensibly for future prosperity. The Marshalls sent much of their cloth and, probably, small loads of salt overland to Northwich, and then by river or road to Liverpool.