Mattole Restoration Council, Carbon Sequest Lower Mattole River and Estuary Enhancement Project Phase II
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Efforts to Restore the Mattole River and Its Watershed Chad Buran
Efforts to restore the Mattole River and its watershed Chad Buran Introduction Up and down the Pacific Coast of the Northwest United States, the salmon and steelhead populations have been severely impacted by the increased timber harvesting and road construction along the streams that the fish depend on for spawning. The Mattole River is one example of how these activities have descimated the fishery. The efforts to restore the Mattole watershed is one of the first citizen-initiated watershed restoration projects in North America. For more than twenty years, the inhabitants of the watershed have worked to improve the ecological health of streams, fisheries, forests, and soils of the watershed. The Mattole Salmon Group (MSG) was formed by citizens of the watershed in the 1970s in response to the decline in the Mattole salmon fishery. The initial restoration efforts began in 1980, to provide substitute spawning habitat. In the mid-1980s, the Mattole Restoration Council (MRC) was founded to link the various restoration efforts already underway and to coordinate those efforts in the context of the whole basin. These groups have used a variety of restoration techniques to improve the spawning habitat and the health of the Mattole River. The objective of this paper is to describe the restoration approaches that these two Mattole River groups have used and to review the success of these techniques in this location. I will also describe how techniques have been used in different contexts in the watershed and how they have worked in under various conditions of river flow in these locations. Geographic Setting and Historical Context The Mattole River drains a 304-square-mile (787-square-kilometer) watershed in the Coast Ranges of northwestern California. -
King Range National Conservation Area Case Study
University of Colorado Law School Colorado Law Scholarly Commons Getches-Wilkinson Center for Natural Books, Reports, and Studies Resources, Energy, and the Environment 2004 King Range National Conservation Area Case Study Ann Morgan Doug Cannon University of Colorado Boulder. Natural Resources Law Center Follow this and additional works at: https://scholar.law.colorado.edu/books_reports_studies Part of the Natural Resources and Conservation Commons, Natural Resources Law Commons, and the Natural Resources Management and Policy Commons Citation Information Ann Morgan & Doug Cannon, King Range National Conservation Area Case Study (Natural Res. Law Ctr., Univ. of Colo. Sch. of Law 2004). Ann Morgan & Doug Cannon, KING RANGE NATIONAL CONSERVATION AREA CASE STUDY (Natural Res. Law Ctr., Univ. of Colo. Sch. of Law 2004). Reproduced with permission of the Getches-Wilkinson Center for Natural Resources, Energy, and the Environment (formerly the Natural Resources Law Center) at the University of Colorado Law School. KING RANGE NATIONAL CONSERVATION AREA CASE STUDY Ann Morgan and Doug Cannon Natural Resources Law Center January 9, 2004 Table of Contents BACKGROUND................................................................................................................................. 1 PUBLIC LAW 91-476....................................................................................................................... 2 LEGISLATIVE HISTORY ................................................................................................................. -
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future As more and more states are incorporating projections of sea-level rise into coastal planning efforts, the states of California, Oregon, and Washington asked the National Research Council to project sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account the many factors that affect sea-level rise on a local scale. The projections show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections; north of that point, sea-level rise is projected to be less than global projections because seismic strain is pushing the land upward. ny significant sea-level In compliance with a rise will pose enor- 2008 executive order, mous risks to the California state agencies have A been incorporating projec- valuable infrastructure, devel- opment, and wetlands that line tions of sea-level rise into much of the 1,600 mile shore- their coastal planning. This line of California, Oregon, and study provides the first Washington. For example, in comprehensive regional San Francisco Bay, two inter- projections of the changes in national airports, the ports of sea level expected in San Francisco and Oakland, a California, Oregon, and naval air station, freeways, Washington. housing developments, and sports stadiums have been Global Sea-Level Rise built on fill that raised the land Following a few thousand level only a few feet above the years of relative stability, highest tides. The San Francisco International Airport (center) global sea level has been Sea-level change is linked and surrounding areas will begin to flood with as rising since the late 19th or to changes in the Earth’s little as 40 cm (16 inches) of sea-level rise, a early 20th century, when climate. -
Offshore Pacific Highlights in Summer-Fall 2005: Just Another Year
IOffshoreSummer-Fall Pacific 2005.Hig.hlights JustAnother in Year PETERPYLE ß INSTITUTEFOR BIRD POPULATIONS ß RO. BOX 1346 ß POINTREYES STATION, CALIFORNIA 94956 ß (EMAIL:[email protected]) IncreasingOur Knowledge ofOcean wasthat seabird productivity had been average morea questionof badtiming than of whole- Events,One Year at a Time towell above average in theperiod 1999-2004. sale disaster. By earlyfall, the wordhad spread:2005 was For a burgeonedpopulation of younger Seabirdpopulation sizes and productivity an unusualyear for seab•rdsoff the Pacific coast seabirds,this was a firstreal test of theirforag- provideexcellent barometers of the stateof of NorthAmerica. But was it that unusual? ing abilities,and it is neithersurprising nor ourmarine ecosystems, helping us keep a fin- Manyyears ago, David Ainley concluded that unhealthy(at thepopulation level) that a die- geron negativeanthropogenic effects such as therewas no suchthing as a "normal"year in off shouldhave ensued. Furthermore, offshore climatechange, oil contamination,and over- the California Current, and it would fishing.But we mustbe patientto follow that theremay not be "un- ß '=•,--L• CSCAPE2005 understandsuch large-scale process- usual"years either. Rather, seabird es. For these reasons,the National dynamicsin the PacificOcean are • "•C'13 r/•ie Co3sr NMS Oceanicand Atmospheric Adminis- Washin,on bestexplained interms of overlap- tration(NOAA) is increasingsup- pingclimatological and oceaniccy- Le• d•es portfor a widevariety of long-term cles,which influencecomplex ma- -
Trees Decided Issue
Peninsula Diary Mayo Hayes O’Donnell manuscripts, pictures and other items, much of which pertains to the early history of Monterey. February 16, 1950 The Monterey History and Art Association is a member Trees Decided Issue of the state historical society and many Peninsula Under a heading “Tall Trees May Have Swung Early residents are also contributing members of this Capital to Monterey” Lee Shippey writes in the Los worthwhile group. Mr. Aubrey Drury is the president Angeles Times abut a Christmas Card sent to him by and Joseph R. Knowland is a vice president. Among the Thomas W. Norris of Carmel. The card was a reprint of a patron members are Mrs. Henry Potter Russell and Miss letter from Sebastian Vizcaino, written in Monterey on Margaret Jacks, both of whom are also interested in the December 28, 1602. It tells that Vizcaino had been History ad Art Association and the Foundation in ordered by the Count de Monte-Rey to explore the Monterey. Allen Griffin and Mrs. Harry W. Toulmin and harbors of the “the South Sea” from Acapulco to Cape Mrs. John Payson Adams are numbered among the Mendocino, having been sent out with supplies for sustaining membership list. eleven months. The Colonial House and Garden Symposium will take He had left Acapulco on May 5 of that year and the place in Colonial Williamsburg, Virginia, in February and difficulties had been so great that some of the men had March, under the sponsorship of House and Garden and died and the provisions and munitions were too low to Colonial Williamsburg. -
Elements of Recovery
ELEMENTS OF RECOVERY An Inventory of Upslope Sources of Sedimentation in the Mattole River Watershed with Rehabilitation Prescriptions and Additional Information for Erosion Control Prioritization Prepared for the California Department of Fish and Game by the Mattole Restoration Council P.O. Box 160 Petrolia, CA 95558 December 1989 ELEMENTS OF RECOVERY Erosion is as common an aspect of life in the Coast Range as Pacific sunsets. As the mountains rise up out of the soft ocean bottom, a tenuous and fluid equilibrium is established -- most of each year's uplift is washed or shaken back into the sea. An inch of soil which took a hundred years to build can wash away in a single storm unless held in place by grasses, shrubs, and trees. The streams and rivers are conduits for all this material on its way downhill. Yet under conditions of equilibrium, no more sediment enters the stream than can be easily stored or quickly transported through the system. The Mattole in prehis- toric times was able to move thousands of yards of sediment each year and still be called "clear water," the meaning of the word Mattole in the native tongue. To give an idea of how much ma- terial is moving through the fluvial system, one geologist has estimated that Kings Peak would be 40,000 feet high were it not for this "background" erosion. It doesn't take much to create a disturbance in such a deli- cately balanced system. The erosive power of water increases in proportion to the square of its volume. A midslope road poorly placed, or built on the cheap, or lazily maintained, or aban- doned, can divert large volumes of water from one drainage to another, or onto a slope unarmored by large rock or tree roots. -
Documents from the 1602-1603 Sebastiã¡N Vizcaã No Expedition
Documents from the 1602-1603 Sebastián Vizcaíno Expedition up the California Coast The story of Sebastián Vizcaíno’s 1602-03 voyage formally begins on September 27th, 1599, with the issuance of a Royal Order from the Spanish Court of Phillip III authorizing an expedition from Acapulco with the specific purpose of exploring and mapping the California coast. More than three decades before, in 1565, trade had first been established between Acapulco and the Orient, and once or twice every year several of the famed Manila galleons would make crossings of the Pacific. From Mexico, these enormous ships would take very little-- mostly silver, which was greatly coveted by the Chinese. On the return trip, however, they would be filled to capacity with spices, porcelain, ivory, lacquer ware, and Chinese silks to be sold in European markets. Once the galleons arrived in Acapulco, their cargo was transported overland to the Mexican port of Veracruz, and from there would be placed on the Spanish fleet bound for Spain. The trip from Acapulco to the Philippines was a relatively easy one and took only three months, from March to late May or early June. The return trip and its ideal route, however, were much more problematic. In 1565, it had been discovered by accident that by sailing from Manila far to the north before heading east, ships could pick up trade winds that would push them eastward towards the west coast of North America. This maneuver would take the galleons to what is today Cape Mendocino off the coast of Northern California, and from there the ships would simply follow the California coast south-southwest all the way to Acapulco, arriving three or four weeks later. -
United States Department of the Interior King Range National
United States Department of the Interior BUREAU OF LAND MANAGEMENT King Range Project Office P.O. Box 189, 768 Shelter Cove Road Whitethorn, CA 95589 www.ca.blm.gov/kingrange King Range National Conservation Area: Roads & Trails Report February 1, 2021 Water sources: All sources of water throughout the King Range National Conservation Area require treatment and/or proper filtration. All coastal watersheds are flowing as well as high country springs, Miller Spring and Maple Spring below the summit of King Peak. Bear Hollow Spring status is currently unknown. When navigating roadways within the King Range National Conservation Area ensure appropriate vehicle safety equipment is present in automobile (including properly inflated spare tire, jack and wrench). Cellphone reception is limited throughout the King Range, an SOS emergency responder device is recommended. “Pack it in, Pack it out.” All visitors are asked to follow Leave No Trace (LNT) guidelines when recreating in the King Range Wilderness. Human waste is to be disposed of in the sand near the tide line by digging an eight-inch-deep cathole and burying it, do not bury waste in or around campsites and creeks. Toilet paper can be buried with waste or packed out. BURNING TRASH IS PROHIBITED. ALL TRASH MUST BE PACKED OUT. As of December 1st, 2020, fire prevention orders have been rescinded however visitors are asked to follow LNT guidelines when having a campfire in the wilderness area. Dig a pit on the beach, never leave fires unattended, ensure the fire is properly extinguished when finished, and remove fire pit before departing. -
1. Introduction
Ancestor Creek Habitat Improvement Project EA # DOI-BLM-CA-N030-2021-0008 U.S. Department of the Interior Bureau of Land Management (BLM) Arcata Field Office Arcata, CA Prepared By: _____________________________________ ___/___/___ Zane Ruddy, Fish Biologist Reviewed By: ______________________________________ ___/___/___ Dan Wooden, Assistant Field Manager 1. Introduction Background and Setting Ancestor Creek is a one square mile tributary to the upper Mattole River in northern Mendocino County (Figure 1). The BLM manages one 40-acre parcel in the watershed, and the remainder of the watershed is managed by the California State Parks and private landowners. The watershed is primarily second growth conifer and hardwood-dominated forest. Ancestor Creek has been identified as a priority tributary for habitat restoration for Endangered Species Act threatened coho salmon (Oncorhyncus kisutch), Chinook salmon (O. tshawytscha), and steelhead (O. mykiss) in the Mattole River (MRRP 2011, NMFS 2014, NMFS 2016) and recent spawner and juvenile surveys have identified it as one of the only streams where coho salmon persist in the watershed (MRRP 2011). Landscape disturbance in the Mattole River watershed, primarily logging and road building during the 1950s – 1980s, and wood removal during the early-mid 1980s, vastly decreased salmonid rearing habitat by disconnecting floodplains from the main channel and increasing channel incision. Juveniles rely on slower velocity habitats for shelter during the winter months, deep pools for protection from predators and increasing temperatures during the summer, and off-channel habitats that support macroinvertebrates. The lack of channel complexity in Ancestor Creek has created a “bowling alley” effect (Figure 2) in which water travels through the channel at high velocity causing incision and bank undercuts therefore reducing habitat and depositing fine sediment into the system. -
North Pacific Ocean
314 ¢ U.S. Coast Pilot 7, Chapter 8 19 SEP 2021 125° 124° OREGON 42° 123° Point St. George Crescent City 18603 KLAMATH RIVER Trinidad Head 18600 41° 18605 HUMBOLDT BAY Eureka 18622 18623 CALIFORNIA Cape Mendocino Punta Gorda Point Delgada 40° Cape Vizcaino 18626 Point Cabrillo NOYO RIVER 18628 39° 18620 18640 Point Arena NORTH PA CIFIC OCEAN Bodega Head 18643 TOMALES BAY 38° Point Reyes Bolinas Point San Francisco Chart Coverage in Coast Pilot 7—Chapter 8 NOAA’s Online Interactive Chart Catalog has complete chart coverage http://www.charts.noaa.gov/InteractiveCatalog/nrnc.shtml 19 SEP 2021 U.S. Coast Pilot 7, Chapter 8 ¢ 315 San Francisco Bay to Point St. George, California (1) the season, and precipitation of 0.1 inch (2.54 mm) or ENC - US2WC06M more can be expected on about 10 to 11 days per month Chart - 18010 south of Cape Mendocino and on up to 20 days to the north. Snow falls occasionally along this north coast. (9) Winds in spring are more variable than in winter, as (2) This chapter describes Bodega Bay, Tomales Bay, Noyo River and Anchorage, Shelter Cove, Humboldt the subtropical high builds and the Aleutian Low shrinks. Bay and numerous other small coves and bays. The only The change takes place gradually from north to south. deep-draft harbor is Humboldt Bay, which has the largest Northwest through north winds become more common city along this section of the coast, Eureka. The other while south winds are not quite so prevalent. With the important places, all for small craft, are Bodega Harbor, decrease in storm activity, rain falls on only about 6 Noyo River, Shelter Cove and Crescent City Harbor. -
How to Survive Earthquakes and Tsunamis in Northern California
HOW TO SURVIVE EARTHQUAKES AND TSUNAMIS IN NORTHERN CALIFORNIA Part of the Putting Down Roots in Earthquake Country Series Includes new information on the 2011 Japan Tsunami in California 1 Copyright 2011, Humboldt Earthquake Education Center at Humboldt State University. Reproduction by permission only. You Can Prepare for the What do I do? Disclaimer This document is intended to promote earthquake and tsunami readiness. It is based on the best currently available scientific, engineering, and Next Quake or Tsunami During an Earthquak E You Shoul D: sociological research; following its suggestions, however, does not guarantee the safety of an individual or of a SOME PEOplE THINK it is not worth preparing for an earthquake or a tsunami If you are indoors, drop and take cover under a sturdy structure. The writers, contributors, and sponsors of this because whether you survive or not is up to chance. NOT SO! Most Northern table or other furniture. to it and stay put until the handbook assume no liability for death, injuries, property Hold on TION damage, or other effect of an earthquake or tsunami. California buildings will survive even a large earthquake, and so will you, shaking stops. TION C Prepared by the Humboldt Earthquake Education Center especially if you follow the simple guidelines in this handbook and start C and the Redwood Coast Tsunami Work Group (RCTWG), Stay clear of items that can fall and injure you, such as u preparing today. If you know how to recognize the warning signs of a tsunami aftEr an Earthquak E You Shoul D: u in cooperation with the California Earthquake Authority and understand what to do, you will survive that too—but you need to know windows, fireplaces and heavy furniture. -
USA CA Capemendocino Inser
EERI SPECIAL EARTHQUAKE REPORT -JUNE 1992 (0 (Photographs provided by Tom Varner (EERI 1989) and Laura Varner, Dames & Moore.) Overview. During April 25-26, three earthquakes of magnitude 6 or greater occurred in a 24-hour span in the Petrolia area of Humboldt County, California. The first, and largest, was magnitude 7.0 near Petrolia, and was the strongest earthquake in California since Loma Prieta in 1989. The second (magnitude 6.0) and third (magnitude 6.5) events were off the coast of Cape Mendocino. There was building damage to older wood frame buildings in Ferndale, Rio Dell, Fortuna, and Scotia . Damage to a Victorian house in Ferndale ~eismologyc instrument atand Cape Geology. Mendocino An tion or local ground failure. Three obtained. Of particular interest (2.5 miles epicentral distance) faults meet near Mendocino; the was the 2g or greater peak accel- recorded a peak acceleration of 2g San Andreas Fault is to the south, eration recorded at Cape Mendo- lasting 0.1 to 0.2 seconds during the Cascadia subduction zone is to cino, discussed earlier, and a the magnitude 7.0 shock. This is the north, and the Mendocino Fault 0.69g record obtained in Petrolia. the highest acceleration ever re- is to the west. There is a broad Acceleration levels of 1.25g were corded in California, but it may be zone of deformation between the recorded at an abutment of the attributable to instrument malfunc- faults, and the resulting structure Painter Street Overcrossing, while is quite complex. If the main the ground acceleration was shock was on the Cascadia sub- 0.55g.