Community Water Supply List (June 2021)
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RECREATION GUIDE 2021 1 Your BUTTE FAMILY IS IMPORTANT to Our BUTTE FAMILY
2021 Kids Summer Fun Events Pg.27 Pg.8-9 Brought to you by BUTTE RECREATION GUIDE 2021 1 Your BUTTE FAMILY IS IMPORTANT TO our BUTTE FAMILY townpump.com 2 BUTTE RECREATION GUIDE 2021 BUTTE RECREATION GUIDE 2021 3 OUR MISSION e Butte-Silver Bow Parks and Recreation Department is committed to improving our community’s health, stability, beauty, and quality of life by providing outstanding parks, trails, recreational facilities and leisure opportunities for all of our citizens. Butte-Silver Bow Parks & Recreation at a glance: • More than two dozen parks (many with pavilions that can be reserved), numerous playgrounds, a 9 hole regulation golf course, a par-3 golf course, a clubhouse with golf simulators, two disc golf courses, a splash pad, and a wading pool • Ridge Waters: A family water park featuring two water slides, a lazy river, a zero depth entry children’s area, a climbing wall, a diving board, swimming lanes, rentable cabanas, and a concession stand • A new destination playground at Stodden Park • An extensive urban and rural trail system • ompson Park: e only dually managed municipal/National Forest Service park in the nation • Adult and youth programming, which include: volleyball, softball and pickleball and more • Two historic mine yards that are now event facilities • Community-wide special events CONTENTS Parks & Recreation Fast Facts…Page 6 Butte Arborist…Page 7 Ridge Waters…Page 8 We’re on the web! Stodden Park…Page 10 butteparksandrec.com ridgewaters.com Popular Urban Parks…Page 11 highlandviewgolf.com Recreational Facilities…Page 16 Find us on Facebook, Twitter and Instagram! Mine Yards…Page 18 Rural Parks & Recreation Near Butte…Page 20 Thompson Park Map…Page 22 Butte Urban Map…Page 23 @ButteParks @ButteSilverBow @ButteParksandRec Highland View Golf Course…Page 25 Summer Fun Youth Events…Page 27 Regional Outdoor Opportunities… On the cover: Page 29 Cyclist in Thompson Park. -
HIKING TRAILS SOUTH SUNSHINE COAST Sunshinecoastcanada.Com
HIKING TRAILS SOUTH SUNSHINE COAST sunshinecoastcanada.com Local Favourites ROBERTS CREEK heritage graveyard on the Sechelt First Nations band land at the east end. CLIFF GILKER PARK TRAILS ACCESS: From Highway 101 in Sechelt, access the walk- LENGTH & DIFFICULTY: 7 km of trails | 15 min to 2.5 hrs | way from Shorncliffe, Ocean, Trail, Inlet, or Wharf Avenues. GIBSONS Moderate Trails are colour coded and easy to follow and all loop back BURNETT FALLS GIBSONS SEAWALL to the parking lot. The park is a largely advanced second LENGTH & DIFFICULTY: 10-15 min one way | Very Easy LENGTH & DIFFICULTY: 20-30 min one way | Easy growth Douglas Fir forest. Roberts Creek and Clack Creek A short walk with a bit of an incline that ends at a spectacular Paved waterfront walkway with views of Gibsons Marina, flow through this park. The trails cross them at various view of the waterfall. points on rustic wooden bridges and the waterfall is a high- Gibsons Harbour, Keats Island and North Shore moun- ACCESS: 5396 Burnett Rd. From Sechelt, go north on light (especially in the winter time). Wheelchair accessible tains. Just steps away from shops and restaurants in Lower Wharf Ave. At the 4-way stop, turn right onto East Porpoise viewing platform. Gibsons. Bay Rd. Take a right turn on Burnett Rd. and park at the end. ACCESS: There are access points along Marine Drive and ACCESS: Follow Hwy 101 west from Gibsons for 10 km or Trailhead will be visible. Gower Point Road in Gibsons, including Armours Beach, drive east on Hwy 101 from Sechelt. -
Coastal Land Loss and Wktlanb Restoration
COASTAL LAND LOSS AND WKTLANB RESTORATION tSI R. E. Turner estuaryare causallyrelated to the landlosses this sealevel ri se,climate change~, soil type,geomorphic century." I then comparethe strengthof this frameworkand age, subsidence or tnanagement. hypothesisto someof theother hypothesized causes of land loss on this coast, There are laboratoryand Four Hypotheses small-scale field trials that support various hypotheses,It seemsto me thatthe mostreliable Four hypothesesabout the causes of indirect interpretationsare basedon what happensin the wetlandlosses in BaratariaBay will be addressed field, andnot on the resultsof computermodels, here adapted from Turner 1997!: laboratorystudies or conceptualdiagrams. H l. i ct n ences of The test results discussed herein are derived t !tin oil banks v d solelyfrom data derived at a landscapescale. The 'ori of 1 loss sin h data set is restricted to a discussion of the Barataria watershed. This watershed is a significant H2. componentof theLouisiana coastal zorie 14,000 lv ha!and there are a varietyof habitatdata available i tl on it. Its easternboundary is the MississippiRiver from whichoccasional overflowing waters are v n.vi hypothesizedto deliver enoughsediinents and on 1 v tno I freshwaterto significantlyinfluence the balanceof rit f i land lossor gain in the receivingwatershed, and whosere-introduction would restore the estuary's wetlands. Improvingour understandingof the H4. w rin si ecologicalprocesses operating in this watershed h ' ' of mightassist in the managementof others. The effect of geologicalsubsidence and sea DIrect and Indirect Causes of Wetland Loss level rise are not included in this list because both factorshave remained relatively stablethis century Wetlandloss is essentiallythe same as land loss when the land-loss rates rose and fell, Local on thiscoast Baurnann and Turner 1990!. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Gulf of California - Sea of Cortez Modern Sailing Expeditions
Gulf of California - Sea of Cortez Modern Sailing Expeditions November 24 to December 4, 2019 Modern Sailing School & Club Cpt Blaine McClish (415) 331 – 8250 Trip Leader THE BOAT — Coho II, 44’ Spencer 1330 Coho II is MSC’s legendary offshore racer/cruiser. She has carried hundreds of MSC students and sailors under the Golden Gate Bridge and onto the Pacific Ocean. At 44.4 feet overall length and 24,000 pounds of displacement, Coho II is built for crossing oceans with speed, seakindly motion, and good performance in both big winds and light airs. • Fast and able bluewater cruiser • Fully equipped for the offshore sailing and cruising experience TRAVEL ARRANGEMENTS You are responsible for booking your own airfare. Direct flights from SFO to La Paz, and Los Cabos to SFO are available but are limited. Flights with layovers in San Diego or Los Angeles will cost less than direct flights. If you would like to use a travel agent to book your flights, we suggest Bob Entwisle at E&E Travel at (415) 819-5665. WHAT TO BRING Luggage Travel light. Your gear should fit in a medium duffel bag and small carry-on bag. Your carry-on should be less than 15 pounds. We recommend using a dry bag or backpack. Both bags should be collapsible for easy storage on the boat in small space. Do not bring bags with hard frames as they are difficult to stow. Gear We have found that people often only use about half of what they bring. A great way to bring only what you use is to lay all your items out and reduce it by 50%. -
South Carolina Landform Regions (And Facts About Landforms) Earth Where Is South Carolina? North America United States of America SC
SCSouth Carolina Landform Regions (and facts about Landforms) Earth Where is South Carolina? North America United States of America SC Here we are! South Carolina borders the Atlantic Ocean. SC South Carolina Landform Regions Map Our state is divided into regions, starting at the mountains and going down to the coast. Can you name these? Blue Ridge Mountains Landform Regions SC The Blue Ridge Mountain Region is only 2% of the South Carolina land mass. Facts About the Blue Ridge Mountains . ◼ It is the smallest of the landform regions ◼ It includes the state’s highest point: Sassafras Mountain. ◼ The Blue Ridge Mountains are part of the Appalachian Mountain Range Facts About the Blue Ridge Mountains . ◼ The Blue Ridge Region is mountainous and has many hardwood forests, streams, and waterfalls. ◼ Many rivers flow out of the Blue Ridge. Blue Ridge Mountains, SC Greenville Spartanburg Union Greenwood Rock Hill Abbeville Piedmont Landform Regions SC If you could see the Piedmont Region from space and without the foliage, you would notice it is sort of a huge plateau. Facts About the Piedmont Region . ◼ The Piedmont is the largest region of South Carolina. ◼ The Piedmont is often called The Upstate. Facts About the Piedmont Region . ◼ It is the foothills of the mountains and includes rolling hills and many valleys. ◼ Piedmont means “foot of the mountains” ◼ Waterfalls and swift flowing rivers provided the water power for early mills and the textile industry. Facts About the Piedmont Region . ◼ The monadnocks are located in the Piedmont. ◼ Monadnocks – an isolated or single hill made of very hard rock. -
Brief History Timeline 2018 (PDF)
TIMELINE ~ BRIEF HISTORY OF SUGARLOAF COVE, SICA, AND SUGARLOAF: THE NORTH SHORE STEWARDSHIP ASSOCIATION 10,000 P.C. Scattered archeological finds indicate Paleo-Indians occupy the area around Lake Superior’s North Shore after the final retreat of glaciers in the last Ice Age (Pleistocene Epoch). A variety of indigenous peoples inhabit the area over thousands of years. 1600s French explorers have the first contact with indigenous peoples in the area in the early to mid-1600s. Fur trade between native tribes and the French, British, and Dutch flourishes in the 1700s and early 1800s. 1854 The Ojibwe, who were established by then as the primary native tribe in northeastern Minnesota, cede substantially all the Arrowhead region, including Sugarloaf Cove, to the federal government in the Second Treaty of La Pointe, opening the area to European settlement. Settlers, mostly Scandinavian, flock to the North Shore and began commercial fishing and logging operations. 1880s Extensive logging begins in Cook County, including depletion of old growth red and white pine around Sugarloaf Cove. 1899 The John Gunderson family from Norway homesteads Sugarloaf Cove property. 1902 Consolidated Water Power & Paper Company of Wisconsin (“Consolidated”) begins a pulp paper business in Rhinelander (name changed to Consolidated Papers in 1962). 1909 The Superior National Forest is established. 1920s In 1923, Consolidated begins harvesting wood from Canada and rafting pulpwood logs across Lake Superior to Ashland for transport to Rhinelander for processing. In 1925, Consolidated acquires a large tract of timberland in Cook County from which to harvest pulpwood (mostly spruce, jack pine, and balsam fir). -
Poquetanuck Cove Canoe and Kayak Trail Anne T
U.S. Fish and Wildlife Service Poquetanuck Cove Canoe and Kayak Trail Anne T. Roberts-Pierson Anne T. Poquetanuck Cove – A Very Special Place Poquetanuck Cove is a two mile Beginning in 2008, a three year Phragmites control effort was initiated long tidal estuary located between in Poquetanuck Cove. This effort involved the cooperation of more than the towns of Preston and Ledyard, 20 different entities which included members of the Thames River Basin Connecticut. State Department of Partnership and a variety of funding sources. Phragmites australis is an Energy and Environmental Protection introduced, invasive plant species that had taken root along the fringe areas experts describe the cove as the of the cove’s marsh system. The high quality brackish water marshes of the largest and highest quality brackish cove have been documented to contain plant species rare to Connecticut. water meadow and cattail marsh on the This project would not have been possible without the numerous volunteers Thames River. who participated in gathering important data as part of this effort. For more information about Partnering to Protect Poquetanuck Cove, please visit the An important extension of the Long Thames River Basin Partnership website at www.trbp.org. Island Sound ecosystem, the cove is a State of Connecticut designated bird sanctuary and it provides shelter Royal Oaks Drive, Ledyard: Take Always let friends or family know for significant flocks of wintering Route 2A to Cider Mill Road (Avery where you will put in, take out, and waterfowl each year. Bald eagles are Hill). Then take the second right onto when you expect to return. -
Guillemot Cove Trail
Stavis Bay Road GC01 GC02 Gate GC03 GC04 GC06 GC05 Plateau Loop Trail GC23 GC22 GC07 GC21 GC20 GC19 GC18 GC08 Boyce Creek GC13 0.1 mi GC11 GC09 GC17 GUILLEMOT COVE NATURE RESERVE GC12 GC16 GC10 Stump House GC14 GC15 Copyright OpenStreetMap and contributors, under an open license http://openstreetmap.org Trails Plateau Loop Trail (0.4 mi) Breaks off Guillemot Cove Rules from the upper part of the River Loop The trails in the Guillemot Cove Nature Trail and soon climbs steeply up the ridge 1. Guillemot Cove Nature Reserve has Reserve are all natural surface trails. a “Pack it in – Pack it out” policy. to a plateau in a quiet, open forest. Main Access Trail (0.2 mi.) Begins across Continue around the loop and return the Please bring a bag or other container the road from the parking lot. This trail way you came to the River Loop Trail. for trash and take it when you leave. winds through an evergreen forest with 2. Park in designated areas only. huckleberry underbrush. Watch for dead Beach House Trail (0.25 mi) From the 3. Help protect reserve habitat by snags with Pileated Woodpecker holes. It is kiosk, go across the meadow, cross Boyce staying on trails and off habitat roughly a mile long and sloping downhill. Creek on a wooden bridge and a small areas. One can follow the access road through an footbridge to the hillside. Keep right 4. The reserve, including the beach, is alder and big leaf maple tree forest or across a meadow, by an old orchard, and bordered by private property. -
Nature-Based Coastal Defenses in Southeast Florida Published by Coral Cove Dune Restoration Project
Nature-Based Coastal Defenses Published by in Southeast Florida INTRODUCTION Miami Beach skyline ©Ines Hegedus-Garcia, 2013 ssessments of the world’s metropolitan areas with the most to lose from hurricanes and sea level rise place Asoutheast Florida at the very top of their lists. Much infrastructure and many homes, businesses and natural areas from Key West to the Palm Beaches are already at or near sea level and vulnerable to flooding and erosion from waves and storm surges. The region had 5.6 million residents in 2010–a population greater than that of 30 states–and for many of these people, coastal flooding and erosion are not only anticipated risks of tomorrow’s hurricanes, but a regular consequence of today’s highest tides. Hurricane Sandy approaching the northeast coast of the United States. ©NASA Billions of dollars in property value may be swept away in one storm or slowly eroded by creeping sea level rise. This double threat, coupled with a clearly accelerating rate of sea level rise and predictions of stronger hurricanes and continued population growth in the years ahead, has led to increasing demand for action and willingness on the parts of the public and private sectors to be a part of solutions. Practical people and the government institutions that serve them want to know what those solutions are and what they will cost. Traditional “grey infrastructure” such as seawalls and breakwaters is already common in the region but it is not the only option. Grey infrastructure will always have a place here and in some instances it is the only sensible choice, but it has significant drawbacks. -
Street Names - in Alphabetical Order
Street Names - In Alphabetical Order District / MC-ID NO. Street Name Location County Area Aalto Place Sumter - Unit 692 (Villa San Antonio) 1 Sumter County Abaco Path Sumter - Unit 197 9 Sumter County Abana Path Sumter - Unit 206 9 Sumter County Abasco Court Sumter - Unit 821 (Mangrove Villas) 8 Sumter County Abbeville Loop Sumter - Unit 80 5 Sumter County Abbey Way Sumter - Unit 164 8 Sumter County Abdella Way Sumter - Unit 180 9 Sumter County Abdella Way Sumter - Unit 181 9 Sumter County Abel Place Sumter - Unit 195 10 Sumter County Aber Lane Sumter - Unit 967 (Ventura Villas) 10 Sumter County SE 84TH Abercorn Court Marion - Unit 45 4 Marion County Abercrombie Way Sumter - Unit 98 5 Sumter County Aberdeen Run Sumter - Unit 139 7 Sumter County Abernethy Place Sumter - Unit 99 5 Sumter County Abner Street Sumter - Unit 130 6 Sumter County Abney Avenue VOF - Unit 8 12 Sumter County Abordale Lane Sumter - Unit 158 8 Sumter County Acorn Court Sumter - Unit 146 7 Sumter County Acosta Court Sumter - Unit 601 (Villa De Leon) 2 Sumter County Adair Lane Sumter - Unit 818 (Jacaranda Villas) 8 Sumter County Adams Lane Sumter - Unit 105 6 Sumter County Adamsville Avenue VOF - Unit 13 12 Sumter County Addison Avenue Sumter - Unit 37 3 Sumter County Adeline Way Sumter - Unit 713 (Hillcrest Villas) 7 Sumter County Adelphi Avenue Sumter - Unit 151 8 Sumter County Adler Court Sumter - Unit 134 7 Sumter County Adriana Way Sumter - Unit 711 (Adriana Villas) 7 Sumter County Adrienne Way Sumter - Unit 176 9 Sumter County Adrienne Way Sumter - Unit 949 (Megan -
A Geomorphic Classification System
A Geomorphic Classification System U.S.D.A. Forest Service Geomorphology Working Group Haskins, Donald M.1, Correll, Cynthia S.2, Foster, Richard A.3, Chatoian, John M.4, Fincher, James M.5, Strenger, Steven 6, Keys, James E. Jr.7, Maxwell, James R.8 and King, Thomas 9 February 1998 Version 1.4 1 Forest Geologist, Shasta-Trinity National Forests, Pacific Southwest Region, Redding, CA; 2 Soil Scientist, Range Staff, Washington Office, Prineville, OR; 3 Area Soil Scientist, Chatham Area, Tongass National Forest, Alaska Region, Sitka, AK; 4 Regional Geologist, Pacific Southwest Region, San Francisco, CA; 5 Integrated Resource Inventory Program Manager, Alaska Region, Juneau, AK; 6 Supervisory Soil Scientist, Southwest Region, Albuquerque, NM; 7 Interagency Liaison for Washington Office ECOMAP Group, Southern Region, Atlanta, GA; 8 Water Program Leader, Rocky Mountain Region, Golden, CO; and 9 Geology Program Manager, Washington Office, Washington, DC. A Geomorphic Classification System 1 Table of Contents Abstract .......................................................................................................................................... 5 I. INTRODUCTION................................................................................................................. 6 History of Classification Efforts in the Forest Service ............................................................... 6 History of Development .............................................................................................................. 7 Goals