District 2 Highways Project List
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September 30, 2009
Final Report Nez Perce National Air Toxics Program Characterization of Air Toxics Concentrations around a Kraft Pulp and Paper Mill Facility, Lewiston, Idaho EPA Assistance ID No. XA-97079001-3 Nez Perce Tribe Environmental Restoration and Waste Management Division Air Quality Program September 30, 2009 1 2 TABLE OF CONTENTS Section Page Purpose of Study………………………………………………………………………………… 5 Methods…………………………………………………………………………………………. 8 Monitoring and Network Design………………………………………………………… 8 Sampling Analysis Methods…………………………………………………………….. 10 Carbonyls Monitoring and Analysis…………………………………………….. 11 PM-10 Monitoring and Analysis………………………………………………… 11 Metals Monitoring and Analysis………………………………………………... 11 VOC Monitoring and Analysis………………………………………………….. 11 Formaldehyde Special Study (DOAS)………………………………………….. 11 Emission Tracking with a Mobile Laboratory (PTR-MS)………………………. 12 Emissions Inventory…………………………………………………………………….. 12 Modeling………………………………………………………………………………… 12 Data and Risk Analysis…………………………………………………………………. 12 Results…………………………………………………………………………………………… 13 Sample Analysis………………………………………………………………………… 13 Formaldehyde Special Study (DOAS)………………………………………………….. 13 Emission Tracking with a Mobile Laboratory (PTR-MS)……………………………… 13 Modeling………………………………………………………………………………… 14 CMAQ…………………………………………………………………………… 14 CALPUFF………………………………………………………………………. 17 Risk Analysis – BCEH/ATSDR………………………………………………………… 18 Acute and Chronic Risks………………………………………………………… 19 Cancer Risks…………………………………………………………………….. 19 Recommendations……………………………………………………………….. 22 Data Analysis -
ED046693.Pdf
DO,AMENT RESUME ED 046 693 SF 009 427 AUTHOR Parsons, Donna L. TITLE Idaho, An Outdoor Classroom. INSTITUTION Caldwell School District 132, Idaho. SPONS AGENCY Bureau of Plementary and Secondary education (DHEW/OE), Washington, D.C. PUB DATE Sep 68 GRANT 0FG-3-7-70457-4972(056) NOTE 224p. AVAILABLE FROM Donna L. Parsons, Caldwell School District 132, Idaho EDRS PRICE EDRS Price M7-$0.65 HC Not Available from EDRS. DESCRIPTORS Conservation Education, Ecology, Environment, *Environmental Education, *Field. Trips, Natural Resources, *Outdoor Education, *Teaching Guides IDENTIFIERS ESEA Title III ABSTRACT This field guide for public school teachers pinpoints special areas in Idaho where students can study and learn by direct experience in the outdoors. The guide divides the state into northern, southwestern, and southeastern districts. Environmental study trip guides complete with roadlogs, pictures, and maps of each area develop the three major districts. The guide concludes with a listing of indnstries, and guided tours of their facilities. This work was prepared under an FSRA Title III contract. [Not available in hardcopy due to marginal legibility of original document. ](PB) 11\1:' ' , t .1V-.Vj r.;1- '"c",;"; ,`,..; , c ",,, 7, ,',',4 F3F,1" 1 t i ;' ,z" f -',4`,",,''' V V <'''''.:`'i7"-''^C ) -';'0 fr, , 1 --',.-',. .7,:.:'..,:'` '' -- f,,.' ' .., -,-,. , t-I. /-,.. -,,,,,,. -1., 's, '-""'-, t.='''. Is ,1",".. ,,,' ,,_,,,-; ,-----4-----*------=';-,--",t,",t-7,-----.';'-7,, - AI ,,' ri , --, ,LS.,1.4L,4,4 ', ' ' i',( , 'I, .-1_,,r,-' ..: ,Y.,^- ''..,-.--',I.zr !..':. -0,0):,: '-''. .. ',.'' .. VI , '' ;,:''. ".r 1' .` ,'",,' "' _.,-. '' 1-Z, ,',,,, ',' ':,' nii' -, J'-' -:',;,..,,-,-,,--':.? , . U.S. DEPARTMENT OF HEALTH. EDUCATION - ', I & WELFARE OFFICE OF EDUCATION VI V " THIS DOCUMENT HAS BEEN REPRODUCED EXACTLY AS RECEIVED FROM THE PERSON OR ORGANIZATION ORIGINATING IT. -
GEOLOGIC MAP of the LEWISTON ORCHARDS NORTH QUADRANGLE and PART of the CLARKSTON QUADRANGLE, NEZ PERCE COUNTY, IDAHO CORRELATION of MAP UNITS Table 1
IDAHO GEOLOGICAL SURVEY DIGITAL WEB MAP 40 MOSCOW-BOISE-POCATELLO GARWOOD AND BUSH GEOLOGIC MAP OF THE LEWISTON ORCHARDS NORTH QUADRANGLE AND PART OF THE CLARKSTON QUADRANGLE, NEZ PERCE COUNTY, IDAHO CORRELATION OF MAP UNITS Table 1. Major oxide and trace element chemistry of basalt samples collected on the Lewiston Orchards North and Clarkston quadrangles. Disclaimer: This Digital Web Map is an informal report and may be Normalized major elements in weight percent Unnormalized trace elements in parts per million revised and formally published at a later time. Its content and format Artificial Surficial Clarkston Columbia River Basalt Group Sample Map Compiled and Mapped by may not conform to agency standards. Deposits Deposits Gravels number Latitude Longitude Unit name unit SiO2 Al2O3 TiO2 FeO* MnO CaO MgO K2OPNa2O 2O5 Ni Cr Sc V Ba Rb Sr Zr Y Nb Ga Cu Zn Pb La Ce Th m HOLOCENE BRY 46.38124 -117.01616 Lewiston Orchards Twl 49.68 14.35 2.543 12.15 0.190 11.41 6.24 0.44 2.41 0.589 49 259 44 323 499 8 242 184 44 20.5 21 50 121 3 15 74 1 Dean L. Garwood and John H. Bush Qal CL1 46.46259 -117.00107 Asotin Taw 50.58 16.04 1.413 9.16 0.156 11.41 8.23 0.51 2.33 0.167 130 284 35 251 156 8 242 105 24 11.5 19 92 75 4 6 44 1 Qls Ql QUATERNARY 2005 PLEISTOCENE CL2 46.46269 -117.00573 Lewiston Orchards Twl 49.49 15.08 2.170 10.84 0.205 11.13 7.71 0.40 2.47 0.507 74 269 39 274 382 3 249 153 37 19.9 16 50 103 6 13 59 3 CL3 46.4577 -117.01966 Grande Ronde R2 Tgr2 55.43 13.86 2.554 11.97 0.192 7.33 3.26 1.86 3.08 0.466 2 27 24 386 890 48 323 191 40 14.8 -
Nez Perce County Comprehensive Plan: Forward ______
Nez Perce County Comprehensive Plan: Forward _________________________________________________________ THE COMPREHENSIVE PLAN This comprehensive plan is a community developed document which, through goals and policies, strives to maintain the living qualities of the Nez Perce County area—a responsibility shared jointly by elected officials, citizens and businesses. The comprehensive plan is an official policy guide for the preferred 20-year vision for the community. Nez Perce County’s first comprehensive plan was adopted in July 1980. Nez Perce County initiated the process of updating the comprehensive plan in July 1997 and appointed a citizen advisory group to lead discussions concerning the future of Nez Perce County. The values, visions, goals and policies that follow in this document represent a consensus of the Nez Perce County community. The Nez Perce County Comprehensive Plan has projected a study area population of over 46,367 by the year 2020. This represents a .85% annual increase in population over the next 22 years. The Nez Perce Comprehensive Plan document contains goals and policies that address physical land use and public facilities that are of concern to planning for this future growth. PURPOSE OF THE PLAN This plan applies to all geographic areas within Nez Perce County’s jurisdiction. The comprehensive plan is the document through which Nez Perce County has stated how land development and redevelopment should occur and how it will be managed. Basic goals of the plan are intended to guide future growth in a manner consistent with the reasons people enjoy living and working in Nez Perce County. The purpose of this updated plan may be best summarized in the following points: To comply with state legislative requirements under the Idaho Local Planning Act. -
Surficial Geologic Map of the Lewiston Orchards North Quadrangle and Part of the Clarkston Quadrangle, Nez Perce County, Idaho
IDAHO GEOLOGICAL SURVEY DIGITAL WEB MAP 8 MOSCOW-BOISE-POCATELLO OTHBERG, BRECKENRIDGE, AND WEISZ Disclaimer: This Digital Web Map is an informal report and may be revised and formally published at a later time. Its content and format SURFICIAL GEOLOGIC MAP OF THE LEWISTON ORCHARDS NORTH QUADRANGLE AND PART OF THE CLARKSTON QUADRANGLE, may not conform to agency standards. NEZ PERCE COUNTY, IDAHO Kurt L. Othberg, Roy M. Breckenridge, and Daniel W. Weisz 2003 CORRELATION OF MAP UNITS is comprised of approximately fifty percent non-basalt clasts. Our observations suggest more complex facies in the unit, reflecting interaction of mainstream Surficial Latah Columbia River and side-stream sources. Part of the colluvium unit mapped by Hooper and Deposits Formation Basalt others (1985) is an alluvial-fan facies of all basalt clasts that interfingers with Qac and partly caps the Clearwater-source mainstream facies. These deposits Qp Qac m Qac Qac Qam Qac Qp Qac Qoam Qas Qac HOLOCENE and their stratigraphic relationships can be seen in exposures uphill from Qp Qac the site described by Kuhns (1980), in the POE Asphalt gravel in north Qp Qad Qls Qcb Qp Qm 13,000 years Lewiston, and three miles to the east in a gravel pit adjacent to Groundcovers, Qac Qp Ql QUATERNARY Incorporated. As described by Kehew (1977), Webster and others (1982), Qp 14,500 years Qb Qag and Hooper and others (1985), the Clearwater Gravel, and its downstream Qp Qp Qp correlative Clarkston Heights Gravel, represent a major aggradational event Qp PLEISTOCENE Qp in which an ancestral valley was filled to about an elevation of 1,150 feet Qp Qac (alluvial-fan facies extend higher on old valley-side remnants). -
Geological Society of the Oregon Country: Lewiston Basin Field Trip
Geological Society of the Oregon Country: Lewiston Basin Field Trip Dean L. Garwood Roy M. Breckenridge Idaho Geological Survey University of Idaho Staff Report 14-2 875 Perimeter Drive MS 3014 August 2014 Moscow, Idaho 83844-3014 www.IdahoGeology.org Geological Society of the Oregon Country: Lewiston Basin Field Trip Dean L. Garwood Roy M. Breckenridge Staff Reports present timely information for public distribution. This publication may not conform to the agency’s standards. Idaho Geological Survey University of Idaho Staff Report 14-2 875 Perimeter Drive MS 3014 August 2014 Moscow, Idaho 83844-3014 www.IdahoGeology.org Stop 1: Lewiston basin overview Lewiston, Idaho, and Clarkston, Washington, are at the confluence of the Snake and Clearwater rivers in the Lewiston basin. Hells Canyon stretches to the south of Lewiston on the Snake River. This is the lowest point in Idaho at 720 feet (220 m) elevation. Lewiston is Idaho’s seaport, a result of slack water created by several dams and locks on the Columbia- Snake River system. The east-west trending trough-shaped Lewiston basin occurs along the northern edge of the Clearwater embayment, a broad swath of Columbia River basalt flows less than 1 km thick that cover much of the accreted Wallowa island arc terrane, suture zone, and outboard plutons of the Idaho batholith. The geology of this region is outlined in Kauffman and others (2006). The basin is strongly structurally controlled. Lewiston Hill below is underlain by an east-west trending asymmetrical anticline that includes a steeply dipping south limb that forms a dip slope along much of the exposed hillsides. -
Palouse Subbasin Management Plan
Palouse Subbasin Management Plan FINAL DRAFT ~ May 2004 Project Lead: Palouse-Rock Lake Conservation District Trevor Cook, Project Manager PO Box 438 St. John WA 99171 (509) 648-3680 Prepared by: Shelly Gilmore Resource Planning Unlimited, Inc. 1406 East F Street Moscow, ID 83843 Palouse Subbasin Management Plan FINAL DRAFT ~ May 2004 Project Lead: Palouse-Rock Lake Conservation District Trevor Cook, Project Manager PO Box 438 St. John WA 99171 (509) 648-3680 Prepared by: Shelly Gilmore Resource Planning Unlimited, Inc. 1406 East F Street Moscow, ID 83843 Palouse Subbasin Management Plan: Table of Contents i. Introduction i 1. Assessment 1.1 The Palouse Subbasin Of The Past 1-1 1.2 The Present Day Palouse Subbasin 1-2 1.2.1 General Description 1-2 1.2.2 Land Use and Land Ownership 1-3 1.2.3 Jurisdictional Authorities 1-4 1.2.4 Water Resources 1-7 1.2.5 Water Quality 1-9 1.3 Anthropogenic Disturbances 1-13 1.4 Wildlife and Fish Resources 1-14 1.4.1 Historic Habitats 1-14 1.4.2 Current Habitat Types 1-15 1.4.3 Wildlife Resources 1-30 1.4.4 Palouse Subbasin Fauna and Responses to Habitat Changes 1-43 1.4.5 Focal Species 1-50 1.4.6 Fish Resources 1-64 1.4.7 Fish Habitat 1-72 1.5 Limiting Factors 1-75 1.5.1 Agricultural Conversion 1-79 1.5.2 Exotic Vegetation Encroachment 1-86 1.5.3 Timber Harvest 1-88 1.5.4 Fire Suppression 1-88 1.5.5 Urban Development 1-89 1.5.6 Hydropower Development 1-92 1.5.7 Other Limiting Factors 1-92 2.