Serendipity Green PDF Download

Author: Rob Levandoski
Publisher: Open Road Media
ISBN: 1504011961
Category : Fiction
Languages : en
Pages : 223

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Book Description
Tuttwyler, Ohio, is the perfect Midwestern town. Beautiful square. Gazebo dripping with gingerbread. Leafy streets lined with big white houses. Even the town’s annual summer festival is perfect. It commemorates the unfortunate clubbing death of the Indian princess Podewedka, by the town’s founding fathers, John and Amos Tuttwyler, back in 1803. The only thing that’s not perfect is Howie Dornick’s house. It’s right on the parade route and it hasn’t been painted in years. But that’s going to change, now that D. William Aitchbone is chairman of the Squaw Days Committee. You can bet on that! But Bill Aitchbone has to tread carefully. Howie, after all, is the illegitimate son of local war hero Artie Brown. Howie finally does paint his house. But not white like all the others. He paints it the most obnoxious shade of green imaginable. Howie’s really in hot water now. Then Hugh Harbinger sees Howie’s green house. Hugh was once New York City’s most famous color designer. Before going off the deep end, he created 300 different shades of black! He’s determined to make a comeback. Determined to make “Serendipity Green” the most popular color ever. Serendipity Green not only lampoons America’s small town festivals, it lowers the boom on big city trendiness as well. It is irreverent and iconoclastic and simply irresistible.

Author:
Publisher: Elsevier
ISBN: 9780080931227
Category : Philosophy
Languages : en
Pages : 952

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Book Description
The domain of nonlinear dynamical systems and its mathematical underpinnings has been developing exponentially for a century, the last 35 years seeing an outpouring of new ideas and applications and a concomitant confluence with ideas of complex systems and their applications from irreversible thermodynamics. A few examples are in meteorology, ecological dynamics, and social and economic dynamics. These new ideas have profound implications for our understanding and practice in domains involving complexity, predictability and determinism, equilibrium, control, planning, individuality, responsibility and so on. Our intention is to draw together in this volume, we believe for the first time, a comprehensive picture of the manifold philosophically interesting impacts of recent developments in understanding nonlinear systems and the unique aspects of their complexity. The book will focus specifically on the philosophical concepts, principles, judgments and problems distinctly raised by work in the domain of complex nonlinear dynamical systems, especially in recent years. -Comprehensive coverage of all main theories in the philosophy of Complex Systems -Clearly written expositions of fundamental ideas and concepts -Definitive discussions by leading researchers in the field -Summaries of leading-edge research in related fields are also included

Author: Peng Du
Publisher: Taylor & Francis
ISBN: 1040030963
Category : Architecture
Languages : en
Pages : 785

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Book Description
This new handbook provides a platform to bring together multidisciplinary researchers focusing on greening high-density agglomerations from three perspectives: climate change, social implications, and people’s health. Written by leading scholars and experts, the chapters aim to summarize the “state-of-the-art” and produce a reference book for policymakers, practitioners, academics, and researchers to study, design, and build high-density cities by integrating green spaces. The topics covered in the book include (but are not limited to) Urban Heat Island, Green Space and Carbon Sequestration, Green Space and Social Equity, Green Space and Public Health, Biophilic Cities, Urban Agriculture, Vertical Farms, Urban Farming Technologies, Nature and Biodiversity, Nature and Health, Biophilic Design, Green Infrastructure, Urban Revitalization, Post-Covid Cities, Smart and Resilient Cities, Tall Buildings, and Sustainable Vertical Cities.

Author: Dave Hughes
Publisher: Stackpole Books
ISBN: 9780811716017
Category : Sports & Recreation
Languages : en
Pages : 490

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Book Description
Provides step-by-step instructions on tying five hundred trout flies and offers information on tying techniques, tools, and materials.

Author: Mary Bergin
Publisher: Rowman & Littlefield
ISBN: 1493065955
Category : Travel
Languages : en
Pages : 201

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Book Description
You know the adage. Good things come in small packages. Here’s proof: dozens of delicious little destinations that delight travelers who crave fun, safe, surprising, and under-the-radar escapes from big-city bustle and congestion. Time to downshift and discover the natural beauty, unique spirit, and enduring character of unusual burgs of Wisconsin. An eclectic mix of communities makes the cut for this selective guide to rural treasures, many of which are lesser known because of limited or no advertising. Visit for an hour, day, overnight or longer. All these special places have a population of no more than 5,000 people, and many have less than 1,000.

Author: Gary David Blount
Publisher: [email protected]
ISBN:
Category : Biography & Autobiography
Languages : en
Pages : 80

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Book Description
Cliff Lake is a pristine, turquoise colored water, medium altitude trout fishery. Cliff Lake contains three-trout species: Rainbow Trout, Cutthroat Trout and Brook Trout. Cliff Lake sits in an old Earth Quake Fault created many years ago. The Earth Quake in 1959 that created Quake Lake on the Madison River 6-miles from Cliff Lake caused some damage at Cliff Lake. Cliff Lake sustained some damage from this Earth Quake, large boulders from the cliffs surrounding the lake dislodged, falling into the lake and onto a tent in the campground killing one-person. This Earth Quake Fault contains six-lakes, from northerly to southerly: Wade Lake, Cliff Lake, Otter Lake, Goose Lake, Hidden Lake and Elk Lake. Cliff Lake is a nesting area for Bald Eagles, Golden Eagles, Osprey, Sand Hill Crain, Great Blue Herons and Loons. Cliff Lake has three inlets: Lost Mine Canyon Creek, Antelope Creek and Horn Creek. There is no surface water leaving Cliff Lake to the north towards Wade Lake. The water flows underground through the Earth Quake Fault into Wade Lake. Cliff Lake at times has decent hatches of Pale Morning Dun (Ephemerella inermis and Ephemerella infrequens) and Speckled Dun (Callibaetis nigritis) in Lost Mine Canyon Creek, Horn Arm and Antelope Prong Arm. The lake is full of Mottled Sculpin (Cottus bairdi), Slimy Sculpin (Cottus cognatus) and Cray Fish; the jig fishermen can produce some nice trout from this lake. Cliff Lake has three-campgrounds: Cliff Point, Hill Top and a primitive campground. Cliff Lake is 30-miles From West Yellowstone, Montana.

Author: Gary David Blount
Publisher: [email protected]
ISBN:
Category : Biography & Autobiography
Languages : en
Pages : 58

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Normal 0 The Gibbon River originates from two-lakes, Grebe Lake and Wolf Lake just south of Observation Peak in Yellowstone National Park. The Gibbon River is a small meandering stream flowing through a Lodge Pole Forest from Norris Junction upstream to its headwaters and is primarily a Brook Trout and Grayling fishery. This area is known to be inhabited by numerous Grizzly Bears and Moose so beware in fishing this area. Below Norris Junction to Gibbon Falls the Gibbon River is lined with Thermals and Geysers and has increased in size due to the additional water from Solfatara Creek, Geysers and Thermals. This section meanders through Elk Meadows, then through a windy narrow canyon and is primarily a Brown Trout fishery with a few Grayling and Brook Trout mixed in. Below Norris Junction is the beautiful Norris Geyser Basin and everyone should visit this area. The section of the Gibbon River below Gibbon Falls to its confluence with the Firehole River, which creates the Madison River, is primarily a spawning and rearing area for Brown Trout, Rainbow Trout and Mountain Whitefish migrating up from Hebgen Lake in the spring and fall. Overall the Gibbon River has every type of trout water a fishermen could want. The entire drainage is full of wildlife: Grizzly Bears, Black Bears, Elk, Moose, Bison, Deer, Coyotes and Wolves.

Author: Gary David Blount
Publisher: [email protected]
ISBN:
Category : Biography & Autobiography
Languages : en
Pages : 82

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Normal 0 The Yellowstone Drainage supports the largest inland population of native Yellowstone Cutthroat Trout on Earth. The Yellowstone Cutthroat Trout is considered a shared resource in Yellowstone Lake: Grizzly Bears, Black Bears, Bald Eagles Golden Eagles, Pelicans, Osprey, Great Blue Herons, Kingfishers, Gulls, Grebes, Terns, Loons, Mergansers, Mink, Otters, Wolves and Coyotes prey upon Yellowstone Cutthroat Trout. In the Yellowstone drainage 200,000-pounds of Yellowstone Cutthroat Trout are eaten each year by these animals and birds. Yellowstone Lake is the largest fresh water lake in the United States above 7,000-feet, it’s altitude is 7,733-feet above sea level. The Yellowstone Lake encompasses 136 square miles, it is 20-miles long, 14-miles wide and has 110-miles of shoreline. Yellowstone Lake is 320-feet deep at its deepest point. The average depth is 139-feet. Yellowstone Cutthroat Trout generally inhabit the upper 60-feet because their food source rarely occurs below that depth. The average surface temperature in August is 60 degrees Fahrenheit; the bottom the temperature never rises above 42 degrees Fahrenheit. The serenity of Yellowstone Lake can suddenly change with afternoon thunderstorms and their accompanying winds. These winds can routinely produce 3-foot waves or larger within minutes on Yellowstone Lake. With water temperatures averaging 41 degrees Fahrenheit you can develop hypothermia quickly if your vessel capsizes. Fishing season in Yellowstone Lake opens June 15th each year, usually! There are 124-tributaries the Yellowstone Cutthroat Trout use for spawning including the largest tributary, the Yellowstone River. These spawning tributaries open July 15th each year, however some remain closed all year. The use of all lead fishing tackle is band; fisherman must use Non-Toxic alternative products. The West Thumb geyser basin area has intense heat in the lake sediments, which indicate a shallow thermal system underlying this more recent caldera. If the lake level should fall just a few feet, an immense steam (hydrothermal) explosion could occur here. Mary Bay and Indian Pond now show evidence of these craters.

Author: Gary David Blount
Publisher: [email protected]
ISBN:
Category : Biography & Autobiography
Languages : en
Pages : 244

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Normal 0 The headwaters of the Bitterroot River originate from two-major Head Waters. The East Fork of the Bitterroot River originates from the Sapphire Mountains and Anaconda Pintler Wilderness Areas. The West Fork of the Bitterroot River originates from the Bitterroot Mountains and the Selway – Bitterroot Wilderness Areas. The West Fork of the Bitterroot River was dammed in the early 1900’s creating Painted Rocks Reservoir. Below Painted Rocks Reservoir lies the tail-water fishery section of the West Fork of the Bitterroot River, which flows downstream to its confluence with the East Fork of the Bitterroot River north of the town of Conner, Montana. The East Fork of the Bitterroot River is still a free flowing stream. The Wild Fires of “2000” burned much of the timberland in the headwaters of both drainages. During spring run-off and summer thunderstorms the East Fork of the Bitterroot River turns turbid from the ash that is washed into the river from the tributaries flowing into the river. The West Fork of the Bitterroot River however remains clear, Painted Rocks Reservoir allows the headwater run-off to settle out within the reservoir before entering the West Fork of the Bitterroot River below the dam. The East Fork of the Bitterroot River confluence with the West Fork of the Bitterroot River forms the mainsteam of the Bitterroot River, which flows northerly to its confluence with the Clarkfork River outside the city of Missoula, Montana. The Bitterroot River trout fishery has experienced depravation from mankind since the early 1900’s when Marcus Daly “The Copper King” and others commissioned the building of an extensive network of irrigation canals throughout the Bitterroot Valley. The largest canal is the Big Ditch, which runs northerly over seventy-five miles in length traversing the eastside of the Bitterroot River Valley. They built large diversion dams across the Bitterroot River and diverted most of the tributaries in the Bitterroot Valley. These diversion dams dewater the Bitterroot River severely during the summer months. Most of the Bitterroot Tributaries become dry during critical spawning periods for Rainbow Trout, Westslope Cutthroat Trout, Brown Trout and Bull Trout. With these depravation problems on the Bitterroot River there are still some sections of the Bitterroot River that offer good fishing for Rainbow Trout, Brown Trout and Westslope Cutthroat Trout and to a lesser degree Bull Trout. The Bitterroot River at time offers some excellent dry fly fishing. In March and April there are Stone Flies: Skwala Stone Flies (Skwala parallela) and Winter Stone Flies (Capina sp.), May Flies: Midges (Diptera / Chironomous), Early Blue-Winged Olive (Baetis tricaudatus), Dark Gray Quill (Ameletus connectus) and Caddies Flies: Grannom (Brachycentrus occidentalis) and Green Sedge (Ryacophila sp.). In May, June, July and August there are Stone Flies: Salmon Fly (Pteronarcys californica), Western Big Golden Stone Fly (Calineuria californica), Western Medium Golden Brown Stone Fly (Isoperla sp.), Little Yellow Stone Fly (Alloperla pallidula) and Little Olive Stone Fly (Alloperla delicata); May Flies: Midges (Diptera / Chironomous), Late Blue-Winged Olive (Baetis parvus), Little Western Blue-Winged Olive (Ephemerella margarita), Western Green Drake (Drunella grandis), Pale Morning Dun (Ephemerella inermis and Ephemerella infrequens), Small Western Green Drake (Ephemerella flavilinea), Western Leadwing (Isonychia sicca) and Dark Gray Quill (Ameletus connectus); Caddis Flies: Grannom (Brachycentrus occidentalis), Green Sedge (Ryacophila sp.), Great Gray Spotted Sedge (Arctopsyche grandis), Little Tan Short Horn Sedge (Glossosoma sp.), Ring Horn Microcaddis (Leucotrichia pictipes), Spotted Sedge (Hydropsyche sp.), Little Sister Sedge (Cheumatopsyche campyla) and Little Plain Brown Sedge (Lepidostoma pluviale). In September and October there are May Flies: Late Blue-Winged Olive (Baetis parvus), Little Western Blue-Winged Olive (Ephemerella margarita), Tiny Western Olive (Pseudocloeon edmundsi), Pale Morning Dun (Ephemerella inermis and Ephemerella infrequens), Gray Drake (Siphlonurus occidentalis), White Winged Black (Tricorythodes minutus), Caddis: Giant Orange Sedge (Dicosmoecus sp.) and Midges (Diptera / Chironomous).

Author: Gary David Blount
Publisher: [email protected]
ISBN:
Category : Biography & Autobiography
Languages : en
Pages : 102

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Normal 0 The Rattlesnake Creek fishery is unique due to its closure to fishing 45-years ago. Since that time, Rattlesnake Creek has been protected because it supplied Missoula, Montana with municipal water. In 1983, a 25-kilometer section of Rattlesnake Creek above the confluence of Beeskove Creek was opened to catch and release fishing; approximately 12-km immediately below this section remains closed. This study was designed to document the dynamics of an unfished trout population and their response to catch and release angling. The results will provide a point of reference for comparing trout populations in pristine systems with those in heavily impacted and managed streams. Until we understand the structure of undisturbed fisheries and their habitats, our present protection and enhancement efforts will lack both a rational context and effective direction. Objectives for the 1986 study were: 1. Document trout population abundance, size, and species composition, in two unfished sections and two fished sections of Rattlesnake Creek. 2. Evaluate the effects of catch and release fishing on the trout population in Rattlesnake Creek. 3. Document and compare changes in angler catch and pressure on Rattlesnake Creek upstream from Beeskove Creek. 4. Identify early spring and late fall movement patterns of Rattlesnake Creek trout populations. 5. Describe winter habitat used by Westslope Cutthroat Trout. Objectives This one year study was designed to collect baseline data necessary to evaluate the effects of catch and release fishing above Beeskove Creek and the population dynamics of an unfished population of Westslope Cutthroat Trout below Beeskove Creek in western Montana. The objectives for the first year were: 1. Determine wild trout species composition, distribution, size, abundance, and age in four sections of Rattlesnake Creek. 2. Document angler catch and pressure on Rattlesnake Creek upstream of Beeskove Creek. 3. Four sections of Rattlesnake Creek were studied from March, 1985 through February, 1987 to document species composition, distribution, size, and abundance of trout. The effects of catch and release fishing seasonal and diel habitat use were also evaluated. 4. Westslope Cutthroat Trout, Bull Trout, and Brook Trout were present in Rattlesnake Creek. Size and abundance of Westslope Cutthroat Trout and Bull Trout were large compared to other small, relatively infertile streams in western Montana. Catch and release angling (300 anglers per year) had no measurable effect on size and abundance of trout in Rattlesnake Creek. Twenty-one percent of all Westslope Cutthroat Trout tagged were recaptured and 68% of the Westslope Cutthroat Trout over 400-millimeters were caught and released. These and other data collected on Rattlesnake Creek indicate the extreme vulnerability of Westslope Cutthroat Trout to angling. 5. Diel and seasonal changes in Westslope Cutthroat Trout behavior and habitat use were documented. Westslope Cutthroat Trout behavior during late spring days was related to spawning. Feeding was the dominant activity during summer days and cover seeking dominated during winter days. Diel shifts were most noticeable from winter days to winter nights. Twice as many trout were seen at night under harsh winter conditions. Winter night counts correlated well with the summer day counts. Study Area The upper Rattlesnake Creek drainage is located in west central Montana, 8.3-kilometers (5.6-miles.) north of Missoula. The drainage encompasses approximately 21,053 ha (81.3-miles²), and is within the Lolo National Forest. Rattlesnake Creek originates on the flanks of McLeod and Triangle peaks, flowing south-southwest to its confluence with the Clark Fork of the Columbia River at Missoula. The creek descends 1,613-meters (5,291.0-ft) in 37.0-kilometers and has a mean gradient of 4.3%, with a gradient of 1.75% in the study sections (USFS-Lolo, 1976). There are nine perennial tributaries to Rattlesnake Creek. Wrangle, Lake, and High Falls creeks originate from glacial lakes while Porcupine, East Fork of Rattlesnake, Beeskove, Pilcher, Fraser and Spring Creeks originate from springs. More than 40 lakes are located in the upper drainage. The geologic parent material in the area includes argillite, quartzite, and limestone of the Precambrian Belt series as well as Cambrian shales and limestones (Nelson & Dobell 1961). The watershed is characterized by relatively high peak discharge per unit area (Van der Poel 1979). The general topography of the drainage is steep and mountainous. Vegetation varies from a spruce-fir forest in the upper drainage to an open pine-larch forest below Franklin Bridge. Cottonwood trees and shrubs are found in the lower riparian zone and occasionally the valley bottom opens up to small grassy meadows. Rattlesnake Creek is a 3rd order stream with a rubble-gravel bottom and an average annual discharge of 45 to 50-cubic feet per second. The Rattlesnake Creek drainage is managed primarily as a watershed and secondarily as a recreational area (USFS Management Plan 1984). Although Rattlesnake Creek is not currently used as a municipal water supply, plans of building a filtration plant and again using the water municipally are being discussed. A water company dam located 4.0-kilometers upstream from the mouth of Rattlesnake Creek would be the most probable site for a filtration plant. The 12.2-meters high dam prevents all upstream fish migration from the Clark Fork River.