DOCSLIB.ORG

Ination# 150150 I[T:I#:L9j:,T:I:-:" S-":,Lf

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Ination# 150150 I[T:I#:L9j:,T:I:-: State of Alaska Nomination Form Department of Fish and Game Anadromous Waters Catalog Division of Sport Fish Region SWT COLD BAY A-2 AWC Number of Water Body 283-32-10100-0010 Name of Water body Old Mans Lagoon E usGS Name n Local Name addition I I oelaiqt n Correction n Backup Information ination# 150150 fur 'lsDate Revision Year: ZA/6 rlq Date "-rlzr Date \iIr{ Date OBSERVATION INFORMATION Species Date(s) Observed Rearing Present Anadromous Chum salmon X E D ! u ! |MPoRTANT:Providea||supportingdocumentationthatthiswaterbodyisimportantforth": numberoffishandlifestagesobserved; samplingmethods,samplingouraiionanoarea""rpLo; copieJoffierd-not"r; !t". ntt""n"-pyofamapshov'ing as \i\€rias other inrormation such ffiL"i4f;XtlXi$:5]fl,;if:r"*"Jt$rifihsnedes, as: specific stream reaches observeo as spawnins or rearins Gomments 283'32'10100listed in AK Peninsula M"""g"r""tArea Satmon sy"tilITlillF- nr""ent due to its simirarity to previousry i[T:i#:l9j:,T:i:-:"_s-":,lf-ly,g,:l"l_".:l_".lrrJ1listed AWC water bodies as either a ,'lake,'or,,polygon,; Name of Observer (please print): Signature: Agency: Address: Thiscertifiesthatinmybest.professiona|judgrnerrtandbe|iefthe"oou included in or deleted from the Anadromous foaters Catalog. Date:_ Revision 11/13 Name of Area Biologist (please print): cFp g& E '= i; e g .s3 H X.= e $i i g E s EHoi 5: P: s''B=: E 6 =3 EE .+:. ! s E.o '= E., o gP i E =O EE .E ! F A sJF'rp P F F i ! g€ * I E! ; ': FO O EP g= ;F:u E-E ig 2 +E P Es F *qi ie gE ; F ! € E gg E E E E € 7,1 s E n -e E:(ca B E =*= 'E E or-. E E i E E-E E .o = g E E :;Ee- r! ,;:E iE =E E" EE ; € ; € € .-'fi tr ,9 5 Eg . t e' 3 3 H E ! ? E g =:-eE E E g 5 a tr5.p E ; e O_ tn ie € Et :E vt E rnESE or! Sa A i c= rnp .e+=€ sE T 'E g L €o 2q) E '-- A A R !E F€ .e = Fr .n-^(9 ^go = €F : E € f; c; ^i9E F' si 3F e F e I E =€ r' ry d, X!e;9p :P ;E: I s.€=i gf; E 9scF-9 F 3 gE -(E6-|! Hi H bE E aI c 5u 3 H : gs!#= €€ +e E F q H s t E$ R; 5 F H il(r' ; 96 * E E Pf n f 'E €; qf H i F g BE 3 aJ €F--E $g o, -s iiI. ii :E SP git -'EH= ;"r. iF i r I 'u: IA gHE o (o (lJ: rH "se s€ f E s*E U6 "q Eo E::Ogl il at 3 t E= 'F O $A A; = ssS$ o I E ii uE E i |rUIF\JUt L' i E?; hu xe H+=F ii ii Eg Is$E .c E8(! 0I) 3! - Ossc(uo OPE (1!v(Ebo= c -P- H t€'=(g .E€.=g;E s;.b3 oF T 5E E5i gE !Q .c3: 3i I \ >c 6.E;coo J=5o<E 3 dE 6L.= d.s 5 js I gE .=r L-c O-(ut, .e€ c 5i', E EEE Egq)s b€ 3E e F}E*.s .9 =E€!- q) -P z-oP5 >p qrP3 s: o f Y: ieio cL; = ;E: R 9: F ^IE3 ;- 8grcl4 tr 338 eE &"; a ;3XE'€' oEE XF-ra.l t:r g;ESE EgEs; F O.9 qo gE!3F E g'= g 5 i; ,E E(JrJF)c> E F f,88TfiE iE E ?FsESh=a *!.'til oo p HF9€ s -Es€€9' tr o rE:3E EgEfi;ipu sE E €; E f t ! t ! E=E., 'FtUE€ "t EsE;{ -gtE EFs gF$,mig State of {laska Delartmr.;nt of Fish and Game l,lomination for Waters lmportant lo Anadromous Fish A\f/C Volume SW USGS Quad Cold Bay A-6 Anadromous Water Catalog Nurnber of Waterway stl -fiL - t O7€.^ -- colo Nam€ of Waterway Ott€r Point Croek USGS name Local name Otter Point Creek 311"4007 Aooition Yes Oeletion Conoction Backup Information Revision Year: 2-@t Both * Code: E -U rr-fr?br Drafted Date OBSERVATION INFORMATION Species Date(s) Observed 3pauminq Rearing Miqration Anadromous :cckeve salmon 7t9t00 7t31t00 8t1t0'l iockcve !ockeve iocKeve MPORTANT: Provide all supporting documentation that this water body is important for the spawningJearing or migration of anadromous including: number of fish and life stages observed; sampling methods, sampling duration and area sampled; copies of field notes; etc. Attach a copy of a map showing location of mouth and observed upper €xtent of each species, as well as other information such as: specific stream reaches observed as spawning or rearing habitrat; locations, types, and heights of any barriers; etc. Comments: mouth coordnates are lagoon mouth coordinates. There was also observations in the 1960's Srream moutlti 55103'06.1:eL 15.001798N. Lat. And 163'47, 19.2" or 163.788669 W tons. Upper Salmon Limit: as approximat€d on attach€d mao Name of Observer (please print) Date: Signature: '1?'ot Address: 211 Mission Rd Kodiak. AK 99615 is certifies that in my best professional the above information is this waterbody should be included in deleted from the Catalog of Waters lmportant for Spawning. Rearing or Migration of Anadromous Fishes per AS 16.05.870. Signature of Area Biologist Rovi6ron 7/93 Prepared by: Joe Dinnocenzo 1 3-Dec-01 ,J,Y:* : li r' :; \; ,'l-.i., .:. g t; l':;': lr:tril?.41'& Itis j;:^A !-:uix i i fi s .-* \ .N\ $\Ji i \-J .( N N =r. b, a. e e .;* t I s ).t: hl N lr'- - 6 ,! trl {- E u,tr9 rr.E5 3 E Fo 6 Ll, fii a FE E E ttz cE { E e. a td r. 9 trl 4t { E vlx z { r{ { g;: HfY) \uLA #l izttr-rlt \J .l! tr I I I a J4u () l..tr- Xqrr.l F 5df;=f, 3 osi ,o (J'| Hili I4D E t- dg 1!r co ji (n I h l,r.l Ol Lr- !n o =i rlo g f;r F. o () h Ei mC) {$l L-r() 5i * OF' {-l c\ -B i '^; ffil l-V=il*, f) 6gH c) |JJ L'L o.(r = b (o odrt o Ln r-1-FdE cE (j} ro * 2 E E*i.._\*-k\n t. I I :9 6 q t) 1 q fi8 g\ q -i a ft. "'..\ q q trl T\ d tq Ai q )a$ r! I \J? 3 N) G !t '.tJ i. -*fu- ; J t. { : s{) ."b $ .t0 {-.* t ,"" st Iv) fr) q$ iz/o $-+ q ht 1i {', .'. i Iaatt x (.?n\J/ 'Reuit t?BL' ion State of Alaska q Department of Fish and Game Publ ic Review Nomination for l.laters f'{-'to Important to Anadromous Species s4t0 t0?00' Addi tion -sJ _Deletion rl., tl/ , -t,, l, Name of llaterbody (if known): (1,,r* 'Af.(r L (t.o.r:i.r L ocati on: Anadromous Waters Catalog Volume and Number (t.,.. i1T _ USGS I :63,360 Quadrangle or l:250,000 (if l:63,360 not avai I able) \{n , ,,, r [- Date(s) Observed Stage(s) (Spawning, neaiing l'ligration) comments: Please provide any clarifying information. Also, please inu include a ?13,"'fnjn;":;tr;j:,,1:[:]1, itiod";u;il:"'i[ii iun b;"; [.iy or u,e_,ip_ *'g:"111:1,/-l-{rr { ,r s. ,r,/ r,:> u*T Name of Observer (p'lease t. - ) print) _- I t_i_{ _{^a"I Date: Si gnature: 4u&/_ A- - 'eCJ*Jlsa-,rI Address: Auk-egf-ettstrh6aet_- _ ry , fic*, 1,,9'1-. k,-J rIrF tz hf/E gc t(o bo E oL P (5 L OJ .= OJ 33' --c6P (uJL(D EE VPPd @(o -Qg fi€ irc a9#(! 3! 3=9> EE ho {:.Q(oo E{,\P c)! iFo c'# !-c gQ E€ ->-=-? .9;=(o cL .= ,> ti -t- E o€i q.r P(!c ooX H =':o, .= Ol L.P rn LF Fl q'ooE XN EE ivt eRo io .= --l! 6: .=93 ei v>=*) Err* b='=:G. ! or*i= o^i; -YI ;{ I E E sS€u- iEpe eE i5 €b @ L E= O C()FiC ; o xnroRE c!e F H a- A -\ rr. 'F fE€ e- o-=e-.Fr,9P t+a€ [.s XH; S= E lt=u E i:rg€ i€g; E +€=E rE- coN € E 8*-. €Ery 'E;f; EggsoE'6:: < O g.Xc.'{-Hs ij(, .e gt '1 Eti'l{ di I gA E-i; .g -; ;e E',.9t1 6E ccL(o troo=6 tr...O- a EE FE;E'= 3c €,r |rVTFUI i f H ESFE 9 8,T r=H Lagoon - Wikipedia, the free encyclopedia Page 1 of7 Lagoon From Wikipedi4 the fiee encyclopedia A lagoon is a shallow body ofwater separated from a larger body ofwater by barrier islands or reefs. Lagoons are commonly divided into coastal lagoons and atoil lagoons. They have also been identified as occurring on mixed-iand and graver coastlines. There is an overlap between bodies ofwater classified u, .ouJd lagoons and bodies of water classified as estuaries. Lagoons are common coastal f-eatures around the world. Contents r I Definition r 2 Etymology Balos coastal lagoon r 3 Atoll lagoons ofnorthwestern Crete. The shallow lagoon is separated from the Mediterranean r 4 Coastal lagoons sea by nanow shoals connecting to a small, rocky r 5 River-mouth lagoons on mixed sand and gravel beaches mountaln.
Load more

Recommended publications
  • Alexander the Great's Tombolos at Tyre and Alexandria, Eastern Mediterranean ⁎ N
    Available online at www.sciencedirect.com Geomorphology 100 (2008) 377–400 www.elsevier.com/locate/geomorph Alexander the Great's tombolos at Tyre and Alexandria, eastern Mediterranean ⁎ N. Marriner a, , J.P. Goiran b, C. Morhange a a CNRS CEREGE UMR 6635, Université Aix-Marseille, Europôle de l'Arbois, BP 80, 13545 Aix-en-Provence cedex 04, France b CNRS MOM Archéorient UMR 5133, 5/7 rue Raulin, 69365 Lyon cedex 07, France Received 25 July 2007; received in revised form 10 January 2008; accepted 11 January 2008 Available online 2 February 2008 Abstract Tyre and Alexandria's coastlines are today characterised by wave-dominated tombolos, peculiar sand isthmuses that link former islands to the adjacent continent. Paradoxically, despite a long history of inquiry into spit and barrier formation, understanding of the dynamics and sedimentary history of tombolos over the Holocene timescale is poor. At Tyre and Alexandria we demonstrate that these rare coastal features are the heritage of a long history of natural morphodynamic forcing and human impacts. In 332 BC, following a protracted seven-month siege of the city, Alexander the Great's engineers cleverly exploited a shallow sublittoral sand bank to seize the island fortress; Tyre's causeway served as a prototype for Alexandria's Heptastadium built a few months later. We report stratigraphic and geomorphological data from the two sand spits, proposing a chronostratigraphic model of tombolo evolution. © 2008 Elsevier B.V. All rights reserved. Keywords: Tombolo; Spit; Tyre; Alexandria; Mediterranean; Holocene 1. Introduction Courtaud, 2000; Browder and McNinch, 2006); (2) establishing a typology of shoreline salients and tombolos (Zenkovich, 1967; The term tombolo is used to define a spit of sand or shingle Sanderson and Eliot, 1996); and (3) modelling the geometrical linking an island to the adjacent coast.
    [Show full text]
  • The Wrybill <I>Anarhynchus Frontalis</I>: a Brief Review of Status, Threats and Work in Progress
    The Wrybill Anarhynchus frontalis: a brief review of status, threats and work in progress ADRIAN C. RIEGEN '1 & JOHN E. DOWDING 2 •231 ForestHill Road, Waiatarua, Auckland 8, NewZealand, e-maih riegen @xtra.co. nz; 2p.o. BOX36-274, Merivale, Christchurch 8030, New Zealand, e-maih [email protected]. nz Riegen,A.C. & Dowding, J.E. 2003. The Wrybill Anarhynchusfrontalis:a brief review of status,threats and work in progress.Wader Study Group Bull. 100: 20-24. The Wrybill is a threatenedplover endemic to New Zealandand unique in havinga bill curvedto the right.It is specializedfor breedingon bareshingle in thebraided riverbeds of Canterburyand Otago in the SouthIsland. After breeding,almost the entirepopulation migrates north and wintersin the harboursaround Auckland. The speciesis classifiedas Vulnerable. Based on countsof winteringflocks, the population currently appears to number4,500-5,000 individuals.However, countingproblems mean that trendsare difficult to determine. The mainthreats to theWrybill arebelieved to be predationon thebreeding grounds, degradation of breeding habitat,and floodingof nests.In a recentstudy in the MackenzieBasin, predation by introducedmammals (mainly stoats,cats and possibly ferrets) had a substantialimpact on Wrybill survivaland productivity. Prey- switchingby predatorsfollowing the introductionof rabbithaemorrhagic disease in 1997 probablyincreased predationrates on breedingwaders. A recentstudy of stoatsin the TasmanRiver showedthat 11% of stoat densexamined contained Wrybill remains.Breeding habitat is beinglost in somerivers and degraded in oth- ers,mainly by waterabstraction and flow manipulation,invasion of weeds,and human recreational use. Flood- ing causessome loss of nestsbut is alsobeneficial, keeping nesting areas weed-free. The breedingrange of the speciesappears to be contractingand fragmenting, with the bulk of the popula- tion now breedingin three large catchments.
    [Show full text]
  • Basemap Using the NZ Digital River Network
    Building a Hydrologic Base Map Prepared by David R. Maidment Waterways Centre for Freshwater Research University of Canterbury 14 March 2018 Goals of the Exercise This exercise shows how to develop a hydrologic base map for a catchment showing the catchment boundary and the rivers and streams within it. This is done in two ways – for the Rakaia river in Canterbury using the NZ Digital River Network, and for the Puriri river catchment in Papua-New Guinea using ArcGIS Online ready to use Hydro Services. Computer and Data Requirements To carry out this exercise, you need to have a computer, which runs ArcGIS Desktop version 10.5. This exercise will also work with version 10.4.1 if you do not have access to Version 10.5. You will need a login and password for the University of Canterbury Organizational Account for ArcGIS Online. Part One: Basemap using the NZ Digital River Network Check out information about the New Zealand Digital River Network, or REC (River Environment Classification) at https://www.niwa.co.nz/freshwater-and-estuaries/management- tools/river-environment-classification-0 You can download a copy of the dataset for all of New Zealand at: https://www.niwa.co.nz/static/web/nzRec2_v4.gdb.zip This is a 487 MB file, so you need a good Wifi connection or wired internet connection to do this. When you uncompress this file, it looks like this The nzRec2_V4.gdb is a 2.2 GB geodatabase covering all of New Zealand. If you have the full REC database and you open ArcMap and look at the REC Geodatabase, below is what you see.
    [Show full text]
  • Station to Station Station to Station
    Harper Road, Lake Coleridge R.D.2 Darfield, Canterbury PH: 03 318 5818 FAX: 03 318 5819 FREEPHONE: 0800 XCOUNTRY (0800 926 868) GLENTHORNE GLENTHORNE STATION STATION EMAIL: [email protected] WEBSITE: www.glenthorne.co.nz STATION TO STATION GLENTHORNE STATION STATION TO STATION SELF DRIVE 4WD ADVENTURES CHRISTCHURCH SELF DRIVE 4WD ADVENTURES THE ULTIMATE HIGH COUNTRY EXPERIENCE LAKE COLERIDGE NEW ZEALAND 5 days and 6 nights Tracks can be varied to suit experience levels TOUR START OXFORD AMBERLEY and part trips are available. GLENTHORNE STATION 1 Accommodation is provided along with LAKE COLERIDGE dinner and breakfast. KAIAPOI Plenty of time for walking, fishing, mountain biking, DARFIELD MT HUTT 77 CHRISTCHURCH swimming and photography. METHVEN Daily route book supplied on arrival. Season runs from January to March. 1 LINCOLN Tracks are weather dependant however there are RAKAIA alternative routes, if a section is not available. Traverse the high country from “Station to Station” ASHBURTON CONTACT US FOR A FREE INFORMATION PACK through some of the South Islands remotest areas 0800 XCOUNTRY [0800 926 868] in your own 4WD. PH: 03 318 5818 Starting north of the Rakaia River at FAX: 03 318 5819 Glenthorne Station on the shores of Lake Coleridge, the trail winds its way via formed station tracks EMAIL: [email protected] interlinked by back country roads and finishing in WEBSITE: www.glenthorne.co.nz Otago’s lake district. Harper Road, Lake Coleridge R.D.2 Darfield, Canterbury PH: 03 318 5818 FAX: 03 318 5819 GLENTHORNE FREEPHONE: 0800 XCOUNTRY (0800 926 868) STATION EMAIL: [email protected] LAKE COLERIDGE NEW ZEALAND WEBSITE: www.glenthorne.co.nz GLENTHORNE STATION STATION TO STATION SELF DRIVE 4WD ADVENTURES Starting north of the Rakaia at Lake Coleridge the trail winds Your Station to Station adventure begins at Glenthorne Station, THE ULTIMATE HIGH COUNTRY EXPERIENCE its way via formed station tracks and back country roads.
    [Show full text]
  • Modeling Regional Coastal Evolution in the Bight Of
    MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA Ondoa Gregoire Abessolo, Magnus Larson, Rafael Almar, Bruno Castelle, Edward Anthony, Johan Reyns To cite this version: Ondoa Gregoire Abessolo, Magnus Larson, Rafael Almar, Bruno Castelle, Edward Anthony, et al.. MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA. Coastal Sediments’19, May 2019, Tampa, United States. 10.1142/9789811204487_0178. hal-02394959 HAL Id: hal-02394959 https://hal.archives-ouvertes.fr/hal-02394959 Submitted on 11 Dec 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA ONDOA GREGOIRE ABESSOLO1,2, MAGNUS LARSON3, RAFAEL ALMAR1, BRUNO CASTELLE4, EDWARD J. ANTHONY5, J. REYNS6,7 1. LEGOS, OMP, UMR 5566 (CNRS/CNES/IRD/Université de Toulouse), 14 Avenue Edouard Belin, 31400, Toulouse, France. [email protected], [email protected]. 2. Ecosystems and Fisheries Resources Laboratory, University of Douala, BP 2701, Douala, Cameroun. 3. Department of Water Resources Engineering, Lund University, Box 118, S-221 00, Lund, Sweden. [email protected]. 4. EPOC, OASU, UMR 5805 (CNRS - Université de Bordeaux), Allée Geoffroy Saint- Hilaire – CS 50023 – 33615, Pessac Cedex, France.
    [Show full text]
  • Island Wakes in the Southern California Bight R
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, C11012, doi:10.1029/2004JC002675, 2005 Island wakes in the Southern California Bight R. M. A. Caldeira,1,2 P. Marchesiello,3 N. P. Nezlin,4 P. M. DiGiacomo,5 and J. C. McWilliams3 Received 19 August 2004; revised 21 February 2005; accepted 14 June 2005; published 18 November 2005. [1] Wind- and current-induced island wakes were investigated using a multiplatform approach of in situ, remote sensing, and numerical model simulations for the Southern California Bight (SCB). Island wind wakes are a result of sheltering from the wind, with weak wind mixing, strong heat storage, and consequent high sea surface temperature (SST). Wind wakes around Santa Catalina Island are most persistent during spring and summer months. Current wakes, caused by the disruption of the poleward traveling California Countercurrent, induce eddies to form off the north end of Catalina Island, and these move poleward every 9–12 days. Current wake eddies induce strong mixing, with low SST and high-density sea surface signatures, whereas wind wakes induce high sea surface temperature signatures associated with the formation of a well-defined shallow thermocline. Current wake eddies vary from 1 to 30 km in diameter. From numerical solutions we predicted the frequency of occurrence of current-induced wakes off Santa Catalina Island. Wind wakes were also observed off all the other islands of the SCB as seen from the analysis of synthetic aperture radar data. Time series analysis of the island mass effect phenomenon has shown a concurrence of low SST and high sea surface chlorophyll for Santa Catalina, San Nicholas, and San Clemente islands that might be related to the seasonality of the California Current and California Countercurrent.
    [Show full text]
  • Science for Solutions
    Science for Solutions NOAA COASTAL OCEAN PROGRAM Decision Analysis Series No. 15 Characterization of Hypoxia Topic 1 Report for the Integrated Assessment on Hypoxia in the Gulf of Mexico Nancy N. Rabalais, R. Eugene Turner, Dubravko Justic´, Quay Dortch, and William J. Wiseman, Jr. May 1999 U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Ocean Service Coastal Ocean Program GULF OF MEXICO HYPOXIA ASSESSMENT This report is the first in a series of six reports developed as the scientific basis for an integrated assessment of the causes and consequences of hypoxia in the Gulf of Mexico, as requested by the White House Office of Science and Technology Policy and as required by Section 604a of P.L. 105-383. For more information on the assessment and the assessment process, please contact the National Centers for Coastal Ocean Science at (301) 713-3060. DECISION ANALYSIS SERIES The Decision Analysis Series has been established by NOAA's Coastal Ocean Program (COP) to present documents for coastal decision mak- ers which contain analytical treatments of major issues or topics. The is- sues, topics, and principal investigators have been selected through an extensive peer review process. To learn more about the COP or the De- cision Analysis Series, please write to: NOAA National Centers for Coastal Ocean Science Coastal Ocean Program 1315 East-West Highway, Room 9700 Silver Spring, Maryland 20910 phone: 301-713-3338 fax: 301-713-4044 web: http://www.cop.noaa.gov e-mail: [email protected] Cover image: Extent of bottom water with dissolved oxygen less than 2 mg/l for July 1996 (based on data of Rabalais, Turner, and Wiseman).
    [Show full text]
  • Introduction Getting There Places to Fish Methods Regulations
    3 .Cam River 10. Okana River (Little River) The Cam supports reasonable populations of brown trout in The Okana River contains populations of brown trout and can the one to four pound size range. Access is available at the provide good fishing, especially in spring. Public access is available Tuahiwi end of Bramleys Road, from Youngs Road which leads off to the lower reaches of the Okana through the gate on the right Introduction Lineside Road between Kaiapoi and Rangiora and from the Lower hand side of the road opposite the Little River Hotel. Christchurch City and its surrounds are blessed with a wealth of Camside Road bridge on the north-western side of Kaiapoi. places to fish for trout and salmon. While these may not always have the same catch rates as high country waters, they offer a 11. Lake Forsyth quick and convenient break from the stress of city life. These 4. Styx River Lake Forsyth fishes best in spring, especially if the lake has recently waters are also popular with visitors to Christchurch who do not Another small stream which fishes best in spring and autumn, been opened to the sea. One of the best places is where the Akaroa have the time to fish further afield. especially at dusk. The best access sites are off Spencerville Road, Highway first comes close to the lake just after the Birdlings Flat Lower Styx Road and Kainga Road. turn-off. Getting There 5. Kaiapoi River 12. Kaituna River All of the places described in this brochure lie within a forty The Kaiapoi River experiences good runs of salmon and is one of The area just above the confluence with Lake Ellesmere offers the five minute drive of Christchurch City.
    [Show full text]
  • New York Bight
    NEW YORK BIGHT RESTORATION PLAN REPORT TO CONGRESS NEW YORK BIGHT RESTORATION PLAN FINAL REPORT MARCH 1993 A PRODUCT ,.·F THE NEW YORK-NEW JERSa:'. 1j;U>\RY PROGR/,.� MANAGEMENT cu;·:�·.:RENCE TABLE OF CONTENTS EXECUTIVE SUMMARY S-1 Use Impairments and Precipitating Pollutant Factors S-1 Floatable Debris S-2 Pathogen Contamination S-2 Toxic Contamination S-3 Nutrient and Organic Enrichment S-4 Habitat Loss and Degradation S-5 Program Administration S-5 INTRODUCTION 1 General 1 Congressional Mandate 1 Prior Reports and Activities 2 Preliminary Problem Assessment 3 RESTORATION PLAN MODULES 4 Floatable Debris 5 Introduction 5 Short-term Floatables Action Plan 5 Comprehensive Floatables Plan 6 Independent Activities and Public Education 7 MARPOL Annex V 7 Recycling and Waste Reduction 8 Program Constraints 8 Program Follow-Up 9 Pathogen Contamination 9 Introduction 9 Beach/Shellfish Bed Closure Action Plan 9 Ocean Dumping Ban Act 10 Combined Sewer Overflow (CSO) Abatement Program 10 Alternative Pathogenic Indicator Study 10 Program Constraints 11 Program Follow-Up 11 3. Toxic Contamination 11 Introduction 11 Problem Characterization 12 Total Maximum Daily Load/Wasteload Allocation (TMDL/WLA) 13 Antidegradation 14 TABLE OF CONTENTS (cont.) Toxic Contamination (cont.) Dredged Material Management 14 Ecosystem Indicators 16 Other Existing Programs and Authorities 16 Program Constraints and Follow-Up 17 Nutrient and Organic Enrichment 17 Introduction 17 Problem Characterization 17 Eutrophication Modeling 18 Ecosystem Indicators 18 Program Constraints and Follow-Up 19 5. Habitat Loss and Degradation 19 Introduction 19 Habitat Inventory 19 Regulatory Programs 20 Non-Regulatory Approach 20 Geographic Targeting 20 Program Constraints 20 Program Follow-Up 21 A Comprehensive Focus 21 Program Administration 22 LIST OF FIGURES Figure 1 - The New York Bight 2 Figure 2 - The New York-New Jersey Harbor 3 Figure 3 - Management Conference Membership and Structure 5 ATTACHMENTS 1.
    [Show full text]
  • Survival of Chinook Salmon, Oncorhynchus Tshawytscha, from A
    812 Abstract.-To characterize the im­ Survival of chinook salmon, pact ofspring floods on the survival of juvenile chinook salmon in the un­ Oncorhynchus tshawytscha, from a stable, braided rivers on the east coast ofNew Zealand's South Island, I exam­ spawning tributary of the Rakaia Rivet. ined correlations between spring and summer flows in the mainstem of the New Zealand, in relation to spring and Rakaia River and fry-to-adult survival for chinook salmon spawningin a head­ summer mainstem flows water tributary. Flow parameters that were investigated included mean flow, maximum flow, and the ratio of mean Martin J. Unwin to median flow (an index of flow vari­ National Institute of Water and Atmospheric Research (NIWA) ability), calculated during peak down­ PO Box 8602, Christchurch, New Zealand river migration ofocean-type juveniles (August to January). Survival was E-mail address:[email protected] uncorrelated with mean or maximum flow but was positively correlated with the ratio of mean to median flow dur­ ing spring (October and November). The correlation suggests that pulses of suits can be derived (Kope and Bots­ freshwater entering the ocean during To understand the population dy­ floods may butTer the transition offin­ namics of anadromous Pacific ford, 1990). gerlings from fresh to saline waters and salmonids <Oncorhynchus spp.), it Despite the importance of in­ thus partly compensate for the lack of is important to isolate and charac­ stream habitats for rearingjuvenile an estuary on the Rakaia River. A posi­ terize the influence of varying en­ chinook salmon <0. tshawytscha), tive correlation between spring flow variability and the proportion ofocean­ vironmental factors on annual pro­ the relation betweenflow and brood type chinook in relation to stream-type duction.
    [Show full text]
  • October 1988
    THE LONG BATTLE FOR EQUAL PAY-TRUMPS OR TRUCE? TENTH YEAR OF PUBLICATION OCTOBER 1988 Playwright Renee Talks for the first tii The Mervyn Thomi VIOTHERHOOi wo W om en’s Stories WAHIA PUBLI < Growing Future or M aori Artists t Writers LIBRARY AUCKLAND OLLEGE OF El REBEL OR REACTIONARY? t u r n % The Gluepot Hotel in Ponsonby will host two seasons of comedy cabaret Dare Swan during the Festival. Tickets $16 inc. Booking and GST. O C3 Tue 25th to Sat 29th October. 8pm nightly, Matinee 2pm Sat. The Auckland Comedy Festival will showcase a season by Sydney dance company Dare Swan at the Maidment Theatre in the last week of October. Dare Swan (pictured below) was founded in 1982 and comprises New Zealanders Chris Jannides and Kilda Northcott, founding members of Limbs Dance Cabaret — Week One. Company, Peta Rutter, formerly of Slick Stage, as Oct 26-29. Gluepot. well as Australian’s Kaye Freeman and Anastasi Siotasis. Red Mole join local Comedy- store star Chris Hegan, Sydney mime Ira Seidenstein, and the father of the Christchurch Fringe, River, for a three hour cabaret show, running Wednesday to Saturday in the first week of the Festival. Aucklanders will remember Red Mole from their work in the late seventies, and their appearance at the Sweetwaters Festival in 1980. The core of the group (pictured above), now based in Wellington after a decade of work in America and Europe, will return to Auckland for the Comedy Festival with newly created B O O K ^ a ^ S cabaret material. MmmoKmm Mmmmmm ■ m m H p e r iv n I 1 L f J U 1 T VJL i Presented by Expression Multi-media and the Aotea Centre in association with No Ordinary beer.
    [Show full text]
  • The Malay Archipelago
    BOOKS & ARTS COMMENT The Malay Archipelago: the land of the orang-utan, and the bird of paradise; a IN RETROSPECT narrative of travel, with studies of man and nature ALFRED RUSSEL WALLACE The Malay Macmillan/Harper Brothers: first published 1869. lfred Russel Wallace was arguably the greatest field biologist of the nine- Archipelago teenth century. He played a leading Apart in the founding of both evolutionary theory and biogeography (see page 162). David Quammen re-enters the ‘Milky Way of He was also, at times, a fine writer. The best land masses’ evoked by Alfred Russel Wallace’s of his literary side is on show in his 1869 classic, The Malay Archipelago, a wondrous masterpiece of biogeography. book of travel and adventure that wears its deeper significance lightly. The Malay Archipelago is the vast chain of islands stretching eastward from Sumatra for more than 6,000 kilometres. Most of it now falls within the sovereignties of Malaysia and Indonesia. In Wallace’s time, it was a world apart, a great Milky Way of land masses and seas and straits, little explored by Europeans, sparsely populated by peoples of diverse cul- tures, and harbouring countless species of unknown plant and animal in dense tropical forests. Some parts, such as the Aru group “Wallace paid of islands, just off the his expenses coast of New Guinea, by selling ERNST MAYR LIB., MUS. COMPARATIVE ZOOLOGY, HARVARD UNIV. HARVARD ZOOLOGY, LIB., MUS. COMPARATIVE MAYR ERNST were almost legend- specimens. So ary for their remote- he collected ness and biological series, not just riches. Wallace’s jour- samples.” neys throughout this region, sometimes by mail packet ship, some- times in a trading vessel or a small outrigger canoe, were driven by a purpose: to collect animal specimens that might help to answer a scientific question.
    [Show full text]