Kenai River Recreation Study Major Findings and Implications
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Erosion and Sedimentation in the Kenai Fiver, Alaska
Erosion and Sedimentation in the Kenai fiver, Alaska By KEVIN M. SCOTT GEOLOGICAL SURVEY PROFESSIONAL PAPER 1235 Prepared in cooperation with the U.S.Fish and Wildlife Service UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1982 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Scott, Kevin M.I 1935- Erosion and sedimentation in the Kenai River, Alaska. (Geological Survey professional paper ; 1235) Bibliography: p. 33-35 Supt. of Docs. no.: I19.16:1235 1. Sediments (Geology)--Alaska--Kenai River watershed. 2. Erosion-- Alaska--Kenai River watershed. I. U.S. Fish and Wildlife Service. 11. Title. 111. Series: United States. Geological Survey Professional Paper 1235. QE571. S412 553.7'8'097983 81-6755 AACR2 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract ........................................ 1 Bed material-Continued Introduction ........................................ 1 Gravel dunes in channel below Skilak Lake - - - - - - - - - - - - - - 17 The Kenai River watershed - - -- -- - - - - - - -- - - - - - - - - - _- - - - - - - 3 Armoring of the channel ............................. 18 Climate ........................................ 3 Possible effects of armoring on salmon habitat ---_------- 19 Vegetation ........................................ 3 Surficial deposits of the modern flood plain ------------- 19 Hydrology-------------------------------------------_ -
Resurrection River Landscape Assessment Area
United States Resurrection River Department of Agriculture Landscape Assessment Forest Service Seward Ranger District, October 2010 Chugach National Forest Exit Glacier, courtesy of Kenai Fjords National Park. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual's income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA's TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410, or call (800) 795-3272 (voice) or (202) 720- 6382 (TDD). USDA is an equal opportunity provider and employer. Landscape Assessment Table of Contents Introduction ........................................................................................................................................................1 Purpose ............................................................................................................................................................1 The Analysis Area ...........................................................................................................................................2 -
Russian River Landscape Assessment
Russian River Landscape Assessment Brown Bear, Lower Russian River Prepared by the U.S. Department of Agriculture Chugach National Forest Seward Ranger District August 2004 Russian River Landscape Assessment August 2004 RUSSIAN RIVER LANDSCAPE ASSESSMENT August 2004 Prepared by: Team Leader s Mary Ann Benoit Eric Johansen Recreation Karen Kromrey, Bill Jackson Minerals Sherry Nelson Cultural Resources Tony Largaespada Shannon Huber Hydrology Bill MacFarlane Soils Ricardo Velarde Fire Brian Sines Fisheries Eric Johansen Wildlife Mary Ann Benoit, Jeff Selinger, Bill Shuster Vegetation/Ecology Elizabeth Bella GIS Trey Schillie Lands Karen O’Leary, Bill Jackson Approved by: _____________________________ ____________ Deb Cooper, Seward District Ranger Date US Forest Service ii August 2004 Russian River Landscape Assessment August 2004 TABLE OF CONTENTS 1.0 INTRODUCTION .......................................................................................1 2.0 WATERSHED CHARACTERIZATION......................................................2 2.1 Lands .................................................................................................................. 2 2.2 Geology, Minerals, and Soils .............................................................................. 1 2.2.1 Geology ................................................................................................ 1 2.2.2 Minerals ................................................................................................ 1 2.2.3 Soils ..................................................................................................... -
The Harding Icefield: a Shrinking Landscape on the Kenai Peninsula by John Morton
Refuge Notebook • Vol. 19, No. 47 • November 24, 2017 The Harding Icefield: A shrinking landscape on the Kenai Peninsula by John Morton The Harding Icefield, named after President Warren Harding who visited the Territory of Alaska in 1923, straddlesthe Kenai Mountains between Kenai National Wildlife Refuge and Kenai Fjords National Park. There’s something as big as the island of Mauion than 30 glaciers that feed off the Harding Icefield. the Kenai Peninsula that many locals have not seen One of four icefields remaining in the U.S., the or not seen well. Unless you’re a pilot, your expo- Harding Icefield is the largest wholly within U.S. sure to this mystery blob has likely been constrained to boundaries. It covers over 700 square miles, stretching the hiking trail at Exit Glacier, or perhaps to viewing more than 50 miles from the Resurrection River south- the tidewater glaciers in Northwestern Fjord from a ward to the divide in the Kenai Mountains between commercial tour boat, or perhaps to the edge of Skilak Bradley Lake and Nuka Bay. The icefield embraces Glacier if you’re hunting sheep or goat. These glaciers, Truuli Peak, the highest point in the Kenai Mountains as big as they seem, are three slivers among the more at 6,612 feet above sea level, suggesting that the Hard- USFWS Kenai National Wildlife Refuge 95 Refuge Notebook • Vol. 19, No. 47 • November 24, 2017 ing is likely a mile deep in some places. gae germinate in response to increased light and melt- We need all that ice. -
Kenai Mountains to Sea
KENAI MOUNTAINS TO SEA A Land Conservation Strategy to Sustain Our Way of Life on the Kenai Peninsula Kachemak Heritage Land Trust Audubon Alaska Cook Inletkeeper Kenai Watershed Forum Pacific Coast Joint Venture U.S. Fish and Wildlife Service February 2015 (updated Nov 2016) EXECUTIVE SUMMARY The 6 million-acre Kenai Peninsula is a spectacular place to call home. Much of our economy is based on the Kenai’s abundant natural resources that support commercial, recreational and subsistence fishing, charter services for hunting and wildlife viewing, tourism and other derivative benefits. However, the downside of this natural bounty is that the Kenai is one of the fastest-growing and most visited areas in Alaska. Although almost three-fourths of the peninsula is managed in three Federal conservation units by the U.S. Forest Service, U.S. Fish and Wildlife Service and National Park Service, road and home building, groundwater withdrawal, logging practices, recreational activities, loss of salmon habitat and increasing human-wildlife conflicts fray at the ecological and cultural integrity of the peninsula. There is a need for a peninsula-wide land conservation strategy to sustain our way of life by promoting natural resource-based community assets. The Kenai Mountains to Sea partnership proposes to leverage existing land conservation by focusing on interjurisdictional anadromous stream corridors that pass from the Federal conservation estate through nonfederal lands (including private parcels) to reach the sea. Our goal is to build a broad-based partnership to support and strengthen long-standing and effective private-public partnerships dedicated to voluntarily conserving and enhancing fish and wildlife habitats for the continuing economic, recreational and cultural benefits to residents and visitors of the Kenai Peninsula Borough. -
A Guide to the Late Quaternary History of Northern and Western Kenai Peninsula, Alaska
A GUIDE TO THE LATE QUATERNARY HISTORY OF NORTHERN AND WESTERN KENAI PENINSULA, ALASKA by R.D. Reger, A.G. Sturmann, E.E. Berg, and P.A.C. Burns Guidebook 8 Published by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS 2007 A GUIDE TO THE LATE QUATERNARY HISTORY OF NORTHERN AND WESTERN KENAI PENINSULA, ALASKA by R.D. Reger, A.G. Sturmann, E.E. Berg, and P.A.C. Burns Division of Geological & Geophysical Surveys Guidebook 8 Cover photo: Granitic erratic, measuring 15 m (50 ft) high by 30 m (100 ft) long, was probably carried southward at least 160 km (100 mi) from the Talkeetna Mountains by ice of the Moosehorn stade of the last major glaciation and deposited in the southwest quarter of Kenai C-3 SW Quadrangle. This huge block is one of a series of granitic monoliths that form a north-trending block train across northeastern Kenai Peninsula lowland. STATE OF ALASKA Sarah Palin, Governor DEPARTMENT OF NATURAL RESOURCES Tom Irwin, Commissioner DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Robert F. Swenson, State Geologist and Acting Director Division of Geological & Geophysical Surveys publications can be inspected at the following locations. Address mail orders to the Fairbanks offi ce. Alaska Division of Geological University of Alaska Anchorage Library & Geophysical Surveys 3211 Providence Drive 3354 College Road Anchorage, Alaska 99508 Fairbanks, Alaska 99709-3707 Elmer E. Rasmuson Library Alaska Resource Library University of Alaska Fairbanks and Information Services (ARLIS) Fairbanks, Alaska 99775-1005 3150 C Street, Suite 100 Anchorage, Alaska 99503 Alaska State Library State Offi ce Building, 8th Floor 333 Willoughby Avenue Juneau, Alaska 99811-0571 This publication released by the Division of Geological & Geophysical Surveys was produced and printed in Anchorage, Alaska at a cost of $25.00 per copy. -
Chapter 2: Background Information
Kenai River Comprehensive Management Plan December 1997 CHAPTER 2 BACKGROUND INFORMATION 1.0 Introduction The Kenai River, its tributaries, and the hydrauli- cally connected wetlands are complex ecological and hydrological systems resilient to external pressures to some unknown degree. However, individual im- pacts together can cause cumulative impacts that Photo not will harm the system and jeopardize its continued included health. It is important to understand the attributes of this system, the factors that may be affecting its continued integrity, and the degree to which the system has been harmed by external influences. This chapter provides background information on the most important attributes of this system. Included are descriptions of the seven principal river segments, information on the amount and distribution of fish and wildlife resources, upland and water recreation activities, and the results of the ADF&G 309 Cumulative Impact Study. This study identi- fied critical habitat locations for the rearing period of the Chinook salmon, identified by ADF&G as an indicator species for the Kenai River. 2.0 Natural Conditions The Kenai River drains more than 2,000 square miles of diverse landscape, including glaciers, icefields, large lakes, high mountains and extensive lowlands. From headwaters in the Kenai Mountains, numer- ous tributary rivers - including the Snow and Trail rivers - flow into Kenai Lake. From the western end of Kenai Lake at Cooper Landing, the upper Kenai River flows 18 miles before emptying into Skilak Lake. From the lakes outlet, the lower Kenai River flows 50 miles before emptying into Cook Inlet. The Kenai River is an underfit river. -
Snow River Landscape Assessment
Snow River Landscape Assessment Prepared by the U.S. Department of Agriculture Chugach National Forest Seward Ranger District August 2005 SNOW RIVER LANDSCAPE ASSESSMENT August 2005 Prepared by: Team Leader s Mary Ann Benoit Recreation Karen Kromrey Geology Carol Huber Minerals Sherry Nelson Cultural Resources Leslie Schick Tessa Villalobos Hydrology Bill MacFarlane Soils Ricardo Velarde Fire Brian Sines Dave Lockwood Fisheries Eric Johansen Ruth D’Amico Wildlife Mary Ann Benoit Michelle Dragoo Vegetation/Ecology Elizabeth Bella GIS Trey Schillie Lands Karen O’Leary Josh Milligan Approved by: _____________________________ ____________ Deb Cooper, Seward District Ranger Date Snow River Landscape Assessment August 2005 TABLE OF CONTENTS 1 Introduction .............................................................................................................. 1 1.1 Purpose ............................................................................................................ 1 1.2 The Analysis Area ............................................................................................. 2 2 Watershed Characterization ..................................................................................... 3 2.1 Lands ................................................................................................................ 3 2.2 Geology, Minerals, and Soils ............................................................................. 4 2.2.1 Geology ......................................................................................................