Waterfall Challenge MODERATE • 3 POINTS Dirt Road
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Sulphur Creek Sulphur Creek Has Cut a Deep Canyon That Passes Through the Oldest Rocks Exposed at Capitol Reef
Capitol Reef National Park National Park Service U.S. Department of the Interior Sulphur Creek Sulphur Creek has cut a deep canyon that passes through the oldest rocks exposed at Capitol Reef. It is a perennial stream with a flow that varies significantly in response to upstream water usage, snowmelt, and heavy rain. There are about two miles of scenic narrows and three small waterfalls. Bypassing the falls requires the ability to scramble down 12-foot (3.6 m) ledges. The route usually requires some walking in shallow water, but it is not uncommon for there to be much deeper water that might even require swimming. This route may be difficult for children if deep water is present. Ask at the visitor center for the latest condition report. Dangerous flash floods are an occasional hazard on this route—do not hike the Sulphur Creek route if there is a chance of rain. The 5.8-mile (9.3 km) one-way hike through Sulphur Creek Canyon involves leaving a shuttle vehicle at each end. If you don’t have two vehicles, a 3.3-mile (5.3 km) hike along Highway 24 is required to return your starting point. Vehicle shuttles are not provided or facilitated by the park. Though legal, hitchhiking is not recommended. This route is not an official, maintained trail. Route conditions, including obstacles in canyons, change frequently due to weather, flash floods, rockfall, and other hazards. Routefinding, navigation, and map-reading skills are critical. Do not rely solely on unofficial route markers (rock cairns, etc.); they are not maintained by the National Park Service (NPS), may not indicate Sulphur Creek the route in this description, or may be absent. -
Surviving a Flash Flood in a Slot Canyon
Surviving a Flash Flood in a Slot Canyon Narrow canyons can turn into sheer-walled death traps during heavy rain. Emerging from them safely depends on smart planning, constant awareness, and, when those don't work, a healthy dose of luck. By: Joe Spring for Outside Magazine On July 24, 2010, a flash flood swept 39-year-old Joe Cain and two friends through Utah's Spry Canyon and over a 40-foot cliff. He lived to talk about it—barely. Here's his story, as told to JOE SPRING. IT WAS MY FIRST TIME canyoneering. I was camping in Zion National Park with two friends, Jason Fico and Dave Frankhouser. We planned to do two canyons. The three of us had been doing outdoor stuff for a long time and we had all been rock climbing. I’d been climbing since the mid-90s. I’d been in slot canyons before, scrambling around and hiking up the narrows, and we were all very proficient about setting up rappels on anchors. The first day, July 24, we decided to do Spry Canyon. Jason had been through that canyon before. It’s a three-hour hike from the trailhead to the top where we dumped in. There were sections that you kind of scrambled through, sections you hiked through, and then a drop off with some anchors where you have to rappel. We anticipated we would be done in four hours. This was late July, 2010, monsoon season in Utah. We knew that if it rained this time of year it would probably start in mid-to-late afternoon. -
Minneopa State Park Is That Ground Wheat and Other Grains from 1864 to STATE PARK a FULL SET of STATE PARK RULES and the Third Oldest State Park in Minnesota
© 2020, Minnesota Department of Natural Resources ABOUT THE PARK SO EVERYONE CAN MINNEOPA ENJOY THE PARK... Established in 1905, Minneopa State Park is that ground wheat and other grains from 1864 to STATE PARK A FULL SET OF STATE PARK RULES AND the third oldest state park in Minnesota. It is best 1890. REGULATIONS IS AVAILABLE ONLINE. known for the double waterfall that 54497 GADWALL RD. PARK OPEN MANKATO, MN 56001 thunders during high water. The upper falls 8 a.m.–10 p.m. daily. BLUE EARTH COUNTY • 507-386-3910 [email protected] drops 7 to 10 feet and the lower falls tumbles another 40. This feature is the result of water CAMPGROUND QUIET HOURS cutting into layers of sandstone over time. 10 p.m.–8 a.m. Take the Mill Road to look for the bison, VISITOR TIPS VEHICLE PERMITS reintroduced in 2015. These animals will Required; purchase at park office or self-pay station. • Respect trail closures. naturally manage the prairie ecosystem, • Minneopa has two sections. just as they did over a hundred fifty years ago. PETS WELCOME The office and waterfall are off Near this area, you may view another Keep on 6-foot leash; leave no trace; only service animals allowed in park buildings. County Highway 69. Camping, reminder of the park’s rich history: Seppmann Don’t miss the double waterfall stone windmill, and bison are Mill. Enjoy a walk to the sandstone windmill FIREWOOD off Highway 68. Use only from approved vendors. • Minneopa Creek is not TRAIL HIGHLIGHTS recommended for swimming. -
Bed Load Transport and Boundary Roughness Changes As Competing
Originally published as: Roth, D. L., Finnegan, N. J., Brodsky, E. E., Rickenmann, D., Turowski, J., Badoux, A., Gimbert, F. (2017): Bed load transport and boundary roughness changes as competing causes of hysteresis in the relationship between river discharge and seismic amplitude recorded near a steep mountain stream. ‐ Journal of Geophysical Research, 122, 5, pp. 1182—1200. DOI: http://doi.org/10.1002/2016JF004062 PUBLICATIONS Journal of Geophysical Research: Earth Surface RESEARCH ARTICLE Bed load transport and boundary roughness changes 10.1002/2016JF004062 as competing causes of hysteresis in the relationship Key Points: between river discharge and seismic amplitude • Hysteresis in seismic signals near rivers may not always indicate recorded near a steep mountain stream hysteresis in bed load sediment transport rates, as previously assumed Danica L. Roth1 , Noah J. Finnegan1 , Emily E. Brodsky1 , Dieter Rickenmann2 , • The seismic signal generated by water 3 2 4 turbulence, rather than sediment Jens M. Turowski , Alexandre Badoux , and Florent Gimbert transport, can dominate seismic 1 2 observations near rivers Department of Earth and Planetary Sciences, University of California, Santa Cruz, California, USA, WSL Swiss Federal 3 • Shifting of grains on the river bed may Institute for Forest, Snow and Landscape Research, Birmensdorf, Switzerland, GFZ German Research Centre for change the seismic response to fluid Geosciences, Potsdam, Germany, 4University of Grenoble Alpes, CNRS, IRD, IGE, Grenoble, France flow between rising and falling water levels (hysteresis) Abstract Hysteresis in the relationship between bed load transport and river stage is a well-documented phenomenon with multiple known causes. Consequently, numerous studies have interpreted hysteresis in fl Correspondence to: the relationship between seismic ground motion near rivers and some measure of ow strength (i.e., D. -
Piseco Lake's Least Wanted
Spiny Water Flea Invasive zooplankton found in Piseco Lake, Lake Pleasant, and Sacandaga Lake. Does not harm humans or pets. Gobbles up native zooplankton. Competes with native fish for food. Clumps on fishing line, prevents fish from being landed. No control methods exist. EWM Eurasian Watermilfoil Variable Leaf Milfoil Aquatic invasive plants. EWM is found in Lake Algonquin, Fifth, Sixth and Seventh Lakes. VLM is found in Eldon Lake, Forked Lake, Fourth, Fifth, Sixth and Seventh Lakes, Lake Durant, Long Lake, Raquette Lake, and Rock Pond. Inhibit boating and fishing, and devalue shoreline property. Expensive to control. VLM Check and remove visible plants, animals, and mud from your boat, trailer, and equipment. Dispose of in the trash or on dry land. Drain water from bilge, motor, livewells, bait buckets, ballast tanks, kayaks, and canoes. Clean your watercraft and gear with hot (greater than 140oF) water or spray with high pressure water. Dry at least 5 days. 518-548-3991 · www.hcswcd.com Facebook · YouTube Map of Adirondack Lakes with aquatic invaders. From the Adirondack Park Invasive Plant Program P.O. Box 65 Keene Valley, New York 12943 (518) 576-2082 http://adkinvasives.com/ List of Adirondack Waters with Aquatic Invaders. From the Adirondack Park Invasive Plant Program P.O. Box 65 Keene Valley, New York 12943 (518) 576-2082 http://adkinvasives.com/ Over. List of Adirondack Waters with Aquatic Invaders. From the Adirondack Park Invasive Plant Program P.O. Box 65 Keene Valley, New York 12943 (518) 576-2082 http://adkinvasives.com/ . -
Anatomy of the Nile Following the Twists and Turns of the World's Longest River
VideoMedia Spotlight Anatomy of the Nile Following the twists and turns of the world's longest river For the complete video with media resources, visit: http://education.nationalgeographic.org/media/anatomy-nile/ Funder The Nile River has provided fertile land, transportation, food, and freshwater to Egypt for more than 5,000 years. Today, 95% of Egypt’s population continues to live along its banks. Where does the Nile begin? Where does it end? Watch this video, from Nat Geo WILD’s “Destination Wild” series, to find out. For an even deeper look at the Nile, use our vocabulary list and explore our “geo-tour” of the Nile to understand the geography of the river and answer the questions in the Questions tab. Questions Where is the source, or headwaters, of the Nile River? The streams of Rwanda’s Nyungwe Forest are probably the most remote sources of the Nile. The snow-capped peaks of the Rwenzori Mountains are another one of the remote sources of the Nile. The Rwenzori Mountains, sometimes nicknamed the “Mountains of the Moon,” straddle the border between the Democratic Republic of the Congo and Uganda. Many geographers also consider Lake Victoria, the largest lake in Africa, to be a source of the Nile. The most significant outflow from Lake Victoria, winding northward through Uganda, is called the “Victoria Nile.” Can you find a waterfall on the Nile River? As it twists more than 6,500 kilometers (4,200 miles) through Africa, the Nile has dozens of small and large waterfalls. The most significant waterfall on the Nile is probably Murchison Falls, Uganda. -
Freshwater Fishing: a Driver for Ecotourism
New York FRESHWATER April 2019 FISHINGDigest Fishing: A Sport For Everyone NY Fishing 101 page 10 A Female's Guide to Fishing page 30 A summary of 2019–2020 regulations and useful information for New York anglers www.dec.ny.gov Message from the Governor Freshwater Fishing: A Driver for Ecotourism New York State is committed to increasing and supporting a wide array of ecotourism initiatives, including freshwater fishing. Our approach is simple—we are strengthening our commitment to protect New York State’s vast natural resources while seeking compelling ways for people to enjoy the great outdoors in a socially and environmentally responsible manner. The result is sustainable economic activity based on a sincere appreciation of our state’s natural resources and the values they provide. We invite New Yorkers and visitors alike to enjoy our high-quality water resources. New York is blessed with fisheries resources across the state. Every day, we manage and protect these fisheries with an eye to the future. To date, New York has made substantial investments in our fishing access sites to ensure that boaters and anglers have safe and well-maintained parking areas, access points, and boat launch sites. In addition, we are currently investing an additional $3.2 million in waterway access in 2019, including: • New or renovated boat launch sites on Cayuga, Oneida, and Otisco lakes • Upgrades to existing launch sites on Cranberry Lake, Delaware River, Lake Placid, Lake Champlain, Lake Ontario, Chautauqua Lake and Fourth Lake. New York continues to improve and modernize our fish hatcheries. As Governor, I have committed $17 million to hatchery improvements. -
Waterbody Classifications, Streams Based on Waterbody Classifications
Waterbody Classifications, Streams Based on Waterbody Classifications Waterbody Type Segment ID Waterbody Index Number (WIN) Streams 0202-0047 Pa-63-30 Streams 0202-0048 Pa-63-33 Streams 0801-0419 Ont 19- 94- 1-P922- Streams 0201-0034 Pa-53-21 Streams 0801-0422 Ont 19- 98 Streams 0801-0423 Ont 19- 99 Streams 0801-0424 Ont 19-103 Streams 0801-0429 Ont 19-104- 3 Streams 0801-0442 Ont 19-105 thru 112 Streams 0801-0445 Ont 19-114 Streams 0801-0447 Ont 19-119 Streams 0801-0452 Ont 19-P1007- Streams 1001-0017 C- 86 Streams 1001-0018 C- 5 thru 13 Streams 1001-0019 C- 14 Streams 1001-0022 C- 57 thru 95 (selected) Streams 1001-0023 C- 73 Streams 1001-0024 C- 80 Streams 1001-0025 C- 86-3 Streams 1001-0026 C- 86-5 Page 1 of 464 09/28/2021 Waterbody Classifications, Streams Based on Waterbody Classifications Name Description Clear Creek and tribs entire stream and tribs Mud Creek and tribs entire stream and tribs Tribs to Long Lake total length of all tribs to lake Little Valley Creek, Upper, and tribs stream and tribs, above Elkdale Kents Creek and tribs entire stream and tribs Crystal Creek, Upper, and tribs stream and tribs, above Forestport Alder Creek and tribs entire stream and tribs Bear Creek and tribs entire stream and tribs Minor Tribs to Kayuta Lake total length of select tribs to the lake Little Black Creek, Upper, and tribs stream and tribs, above Wheelertown Twin Lakes Stream and tribs entire stream and tribs Tribs to North Lake total length of all tribs to lake Mill Brook and minor tribs entire stream and selected tribs Riley Brook -
Potential for Debris Flow and Debris Flood Along the Wasatch Front Between Salt Lake City and Willard, Utah, and Measures for Their Mitigation
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Potential for debris flow and debris flood along the Wasatch Front between Salt Lake City and Willard, Utah, and measures for their mitigation by Gerald F. Wieczorek, Stephen Ellen, Elliott W. Lips, and Susan H. Cannon U.S. Geological Survey Menlo Park, California and Dan N. Short Los Angeles County Flood Control District Los Angeles, California with assistance from personnel of the U.S. Forest Service Open-File Report 83-635 1983 This report is preliminary and has not been edited or reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature, Contents Introduction Purpose, scope, and level of confidence Historical setting Conditions and events of this spring The processes of debris flow and debris flood Potential for debris flow and debris flood Method used for evaluation Short-term potential Ground-water levels Partly-detached landslides Evaluation of travel distance Contributions from channels Contributions from landslides Recurrent long-term potential Methods recommended for more accurate evaluation Mitigation measures for debris flows and debris floods Approach Existing measures Methods used for evaluation Hydrologic data available Debris production anticipated Slopes of deposition General mitigation methods Debris basins Transport of debris along channels Recommendations for further studies Canyon-by-canyon evaluation of relative potential for debris flows and debris floods to reach canyon mouths, and mitigation measures Acknowledgments and responsibility References cited Illustrations Plate 1 - Map showing relative potential for both debris flows and debris floods to reach canyon mouths; scale 1:100,000, 2 sheets Figure 1 - Map showing variation in level of confidence in evaluation of potential for debris flows and debris floods; scale 1:500,000. -
Piseco Lake Public Campgrounds Unit Management Plan
Division of Operations Bureau of Recreation __________________________________________ Piseco Lake Public Campgrounds Unit Management Plan Final Plan Town of Arietta, Hamilton County, New York _____________________________________________ October 2017 New York State Department of Environmental Conservation Division of Operations, 3rd Floor 625 Broadway, Albany, NY12233 Governor ANDREW M. CUOMO Commissioner BASIL SEGGOS OFFICE OF THE COMMISSIONER New York State Department of Environmental Conserviltion 625 Broadway, 14th Floor, Albany, New York 12233-1010 P: (518) 402-8545 I F: (518) 402-8541 MEMORANDUM TO: The Record FROM: Basil Seggos SUBJECT: Piseco Lake Campground The Piseco Lake Campground Unit Management Plan has been completed. The Adirondack Park Agency has found the UMP to be in conformance with the Adirondack Park State Land Master Plan. The UMP is consistent with Environmental Conservation Law, and Department Rules, Regulations and Policies and is hereby approved and adopted. Basil Seggos Commissioner New York State Department of Environmental Conservation 11)/,, I ' 1--- Dcpartmentof r--"~ St-AEWYORKHl)f I c._, ':"'•o•••Nrn- Environmental ~ Conservation PISECO LAKE PUBLIC CAMPGROUNDS SITE SPECIFIC - VOLUME II UNIT MANAGEMENT PLAN NOTE: Volume I is a generic plan and contains overview, environmental setting, goals, policy, management, and impact assessment criteria which pertain universally and in common to all Adirondack and Catskill public campgrounds and special day-use classified intensive-use areas. Volume II is a site- specific document containing inventories of physical, biological, and human-made features, together with specific management actions for the individual site. Volume III contains support data in the form of an appendix to Volumes I and II. The New York State Department of Environmental Conservation (DEC) prepares unit management plans (UMP) to cover the next five-year management period. -
Formation of Waterfalls |Sample Answer
Formation of Waterfalls | Sample answer 2017 Q3.B Examine the impact of the processes of erosion on the formation of one fluvial landform A fluvial landform of erosion is a waterfall. A waterfall is a vertical drip in the youthful stage of a river over which a river falls, usually where a band of soft rock e.g limestone lies downstream from a band of hard rock e.g granite. The process of hydraulic action is very active in forming a waterfall. This is the sheer force of the moving water against the land. It begins as rapids on the river floor which erodes the river’s banks and bed to give rise to the vertical descent of the river’s course. As the river erodes vertically it erodes the soft rock much quicker than the harder rock which leads to differential erosion. The water in the youthful stage is very fast flowing due to the steeper gradient which then allows the water to carry rocks. This makes the process of abrasion active, as the moving rocks scrape and smoothe the river channel. The leads to the increase in the depth of the rapids and the erosive power of hydraulic action. As differential erosion continues, a small waterfall may be formed and seen within the river. The falling water then erodes a deep hole called a plunge pool at the base of the river, as the water is fast flowing and erosive because it is not hindered by friction. The river’s load is word down itself within the plunge pool due to the process of attrition, as the river’s load hits of each other, the riverbed and the back wall. -
Warmwater Fishing New York's Adirondack Lakes
Warmwater Fishing New York’s Adirondack Lakes New York State is full of good waters to catch a variety of warmwater fish species. Here is just a sampling of some of the lakes located in New York’s Adirondack Park. Size rentals boat boat cabin rentalscabin Waterbody (acres) County bass largemouth smallmouth bass pike northern musky musky/tiger pickerel walleye yellow perch bullhead crappie sunfish bass rock white perch trout/salmon ice fishing bait/tackle nearby boat rampspublic boat ramps private boatcartop access marinas campsites Blake Reservoir 710 St. Lawrence * * * * * * * * * Blue Mountain Lake 1,260 Hamilton * * * * * * * * * * * Brant Lake 1,300 Warren * * * * * * * * * * * * * Carry Falls Reservoir 6,458 St. Lawrence * * * * * * * * * * Chazy Lake 1,606 Clinton * * * * * * * * * Cranberry Lake 6,987 St. Lawrence * * * * * * * * * * * Eagle Lake 422 Essex * * * * * * * * * * * * * Eighth Lake 314 Hamilton * * * * * * * * * * Forked Lake 1,250 Hamilton * * * * * * * * * * Fourth Lake 2,137 Herkimer * * * * * * * * * * * * * * Great Sacandaga Lake 22,500 Fulton/ * * * * * * * * * * * * * * * * * * * * Saratoga Higley Flow 698 St. Lawrence * * * * * * * * * * * * Indian Lake 4,364 Hamilton * * * * * * * * * * * * * * * * Lake George 28,000 multiple * * * * * * * * * * * * * * * * * * * Lake Placid 2,803 Essex * * * * * * * * * * * * * Lake Pleasant 1,400 Hamilton * * * * * * * * * * * * * * * * * * Lincoln Pond 500 Essex * * * * * * * * * * Long Lake 4,090 Hamilton * * * * * * * * * * * * * * * * Loon Lake 600 Warren * * * * * * *