For More Information Please Go To

Total Page:16

File Type:pdf, Size:1020Kb

For More Information Please Go To Te Akatarawa Rd DEEP STREAM AVIEMORE DAM SH83 Kurow to Duntroon LEVEL 1000 23km SECTION 7: 800 AORAKI/MOUNT COOK AORAKI/MOUNT LAKE OHAU LODGE LAKE OHAU 600 BRAEMAR ROAD TWIZEL OMARAMA 400 OTEMATATA KUROW Fitness: Easy • Skill: Easy • Traffic: High • Grade: 3 DUNTROON 200 OAMARU 0 0 20 40 60 80 100 120 140 160 180 200 220 240 260 280 300 Old Slip Rd Awahokomo Rd The next leg of the trail passes HAKATARAMEA the Waitaki River and follows AWAKINO RIVER KUROW 7 SH82 State Highway 83, traversing ancient alluvial plains through Kurow’s wine country. There’s SH83 a short climb near the Maori WAITAKI RIVER rock art site [20km] before a KUROW CREEK gentle downhill gradient on Otiake Road the main highway all the way Grants Rd into Duntroon. Gards Rd OTIAKE RIVER WAITAKI RIVER SH83 Special School Rd Eastern Rd Priest Rd MAORI ROCK ART OTEKAIEKE RIVER DUNTROON 8 MAORI Island Cliff-ROCK ART Duntroon Rd ELEPHANT ROCKS MAORI ROCK ART Island Clliff Duntroon Rd MAEREWHENUA RIVER www.alps2ocean.com Map current as of 29/10/14 N (to Danseys pass) Livingston-Duntroon Rd KEY: Onroad Off-road trail Picnic Area Maori Rock Art Fossil Sites Tokarahi-Ngapara Rd 0 1 2 3 4 5km Conlans Rd Trail route and weather conditions subjectTokarahi-Ngapara to change. Rd Please Scale Paradise Valley Rd check website before daily departure. Peaks Rd Cants Rd Peaks Rd Tunnel RdRAKIS RAILWAY TUNNEL Trail Surfaces: Safety Notes: This section is entirely on State Highway 83. Please take care. Highlights: Cyclists are advised to ride single file and stay left. • Kurow Island • Waitaki River Sealed Road (100%) • Maori Rock Art Sites FOR MORE INFORMATION PLEASE GO TO: www.alps2ocean.com.
Recommended publications
  • Outdoor Recreation Strategy 1 2012 - 2022 Central Otago Outdoor Recreation Sstrategytrategy 2012012222 --- 2022022222
    = `Éåíê~ä=lí~Öç= =lìíÇççê=oÉÅêÉ~íáçå= píê~íÉÖó= = OMNO=J=OMOO= February 2012 This is a community owned strategy developed by the Outdoor Recreation Working Party in consultation with the Central Otago Community Central Otago Outdoor Recreation Strategy 1 2012 - 2022 Central Otago Outdoor Recreation SStrategytrategy 2012012222 --- 2022022222 PAGE EXECUTIVE SUMMARY 4 IMPLEMENTATION 8 INTRODUCTION 15 Goals 15 Why have an Outdoor Recreation Strategy? 15 What Comprises Recreation? 16 What Makes a Good Experience 16 Purpose 16 Management Approaches 16 Planning 17 Importance of Outdoor Recreation 17 Central Otago – Geographically Defined 17 Barriers to Participation in Outdoor Recreation 18 Changing Perceptions of Outdoor Recreation 19 Fragmentation of Leisure Time 19 Conflict of Use 19 Changing Perceptions of Risk 19 Developing Outdoor Skills 20 Outdoor Recreation, Individuals and Communities 20 Environmental Considerations 21 Economic Considerations 21 Key Characteristics of Central Otago 21 Other Strategies 21 Regional Identity (A World of Difference) 22 Other Agencies and Groups Involved 22 Assumptions and Uncertainties 22 OVERARCHING ISSUES Human Waste Disposal 23 Rubbish 23 Dogs 23 Signs, Route Guides and Waymarking (Geographic Information) 24 Access 24 Research 25 Landowners 25 Competing Use 26 Communications 27 SPECIFIC RECREATION ACTIVITIES Notes on Tracks, Trails and Recreational Areas 28 Air Activities 29 Mountain Biking 31 Road Cycling 38 Climbing 40 Four Wheel Driving 43 Gold Panning 47 Hunting – Small Game and Big Game 49 Central
    [Show full text]
  • Farming in North Otago
    FARMING IN NORTH OTAGO J. D. CURRIE Ministry of Agriculture and Fisheries, Oarnaru Abstract North Otago is a well-established, efficiently farmed district. Primary production, which grossed an estimated $20 million in the 1973-4 season, will continue to be the major source of regional revenue. The geographic character and the soil resources of the district are described with a comprehensive coverage of historical development, current farming practices and future opportunities for pastoral development. The principal factor limiting agriculture in North Otago is a climate characterized by low, variable rainfall. Pastoral potential is closely tied to investment in oversowing, lucerne and irrigation. Successful farming under difhcult environmental conditions demands above-average ability. The managerial skill of North Otago’s farmers is an outstanding regional resource that augurs well for the future. GEOGRAPHIC DESCRIPTION NORTH OTAGO is a well-defined region. The northern, Canterbury, boundary follows the Waitaki River to its snowfield source in the Southern Alps beyond Lake Ohau. Above Kurow are the hydro dams, below Kurow the river remains as a broad natural boundary, flowing in swift braided channels down a bouldery bed to the sea. The southern boundary that isolates North Otago from its parent province is a mountain wall running north-west from Shag Point to the Lindis Pass and on to the Alps. A fork in the mountains that sweep round from Danseys Pass to Kurow divides North Otago into two districts that are distinct in nature and development. Inland, at Omarama, the sparsely populated run country is similar to Central Otago. Below Kurow is the more closely settled country, The moun- tains and foothills are only suited to extensive grazing, but most of the lower country is made up of rolling loessial downs, good natural grassland, much of it arable.
    [Show full text]
  • FT7 Vanished World
    GEOSCIENCES 09 Annual Conference Oamaru, NZ FIELD TRIP 7 VANISHED WORLD Wednesday 25 November 2009 Leader: Ewan Fordyce Geology Dept, University of Otago BIBLIOGRAPHIC REFERENCE: Fordyce, E. (2009). Vanished World. In: Turnbull, I.M. (ed.). Field Trip Guides, Geosciences 09 Conference, Oamaru, New Zealand. Geological Society of New Zealand Miscellaneous Publication 128B. 13 p. INTRODUCTION The trip has themes of: geological education/ geological sites; regional stratigraphy/ paleontology; and history of geology. It is based around localities from Papakaio to Duntroon-Maerewhenua, North Otago. We will visit a geological visitor centre - Vanished World Centre, Duntroon (www.vanishedworld.co.nz), and significant sites for the Paleogene of southern Canterbury Basin: Cameron's Pit (plant fossils, Cretaceous), Maerewhenua (shallow marine strata, sill, Eocene), and Awamoko-Duntroon (distal marine and unconformities, Oligocene). We will visit 1-2 of the sites specially developed for the public as part of the Vanished World Trail. Text, photos and graphics are by Ewan Fordyce. VANISHED WORLD The Vanished World Trail comprises a self-guided 80 km tour around some 20 geological sites in North Otago, on the coast from Waianakarua (south) to Oamaru (north), and inland to Duntroon in the Waitaki Valley. Sites are on public and private land; access to sites is free, but conditions may be imposed by some landowners. Some sites are close to or on roads, but others require a short walk. The trail is a community initiative developed by locals since 2000, in partnership with the University of Otago, to foster conservation, education and scientific study. The concept of Vanished World arose from local interest in, particularly, research on fossils from the district, but aims to take geology in the broadest sense to the public.
    [Show full text]
  • Mount Domet Becomes Mount Domett
    Mount Domett The history of a mountain Mount Domett, Little Domett and Kohurau illuminated by moonlight, from Round Hill Road, Five Forks, North Otago. Photograph by Gordon Barney, PixNZ.Com Limited (August 1999, approximately 11:00 p.m.) Mount Domett, in North Otago, is situated at the southeastern end of the St. Marys Range, between Kurow to the northeast and Danseys Pass to the south, and is approximately 55 kilometres northwest of Oamaru. Although not the highest in coastal North Otago or in the range (Kohurau at 2009m/6592′ is the highest in both), Mount Domett at 1942m/6370′ and Little Domett at 1860m/6104′ are certainly the most prominent peaks of the skyline when viewed across the coastal North Otago landscape. Mount Domett and the other peaks of the St. Marys Range are often the objectives of tramping and mountaineering parties and with a variety of routes and terrain in both summer and winter conditions, this mountainous area has been well traversed on numerous occasions since the early twentieth century. On Wednesday, 14 August 2002, Mount Domett had the spelling of its name officially changed from „Domet‟ to „Domett‟, correcting the long-standing spelling error of the name of Alfred Domett, in honour of whom it was named. Alfred Domett was born at Camberwell Grove, Surrey, England on 20 May 1811, the sixth child to Nathaniel Domett and Elizabeth Curling. Lawyer, journalist, administrator and poet, Domett became premier of New Zealand from 6 August 1862 to 30 October 1863. He had already purchased land in the Nelson settlement in May 1842 before sailing out from England on the Sir Charles Forbes, arriving in August 1842.
    [Show full text]
  • The Geology of the Oamaru District, North Otago," and Written by Professor James Park, of Otago University, Dunedin
    IJ bd Ml' '^^. ''i^o. ^ > h- '^3:ai\ 4^ # NEW ZEALAND. Pepavfm«?nt M fc\ of "3Rine&. GEOIjOaiCAL SIJUVBY BRA:N^CH[. (P. G. MORGAN, Director). BULLETIN No. 20 (New Series). ho THE GEOLOGY OF THE OAMARU DISTRICT NORTH OTAGO (EASTERN OTAGO DIVISION). BY JAMES PARK, F.G.S., Dean of the Mining Faculty, Otago University, Dunedin. ISSUED UNDER THE AUTHORITY OF THE HON. W. D. S. MaoDONALD, MINISTER OF MINES. WELLINGTON. BY AUTHORITY : MARCUS P. MARKS, GOVERNMENT PRINTER. 1918. Dlvisiorv , Otogo LccrvADist. , Oarruxru, District, Eastei-rvOta^o vet . accoTTLpany BxMetxrv mZO P.G.MORGAN. DIRECTOR. GEOLOGICAL MAP — :Bvlleti-rb2l°E0. Table Top Hill JSTcJ Oamaru Creek ' . ^ Landon Creek C 8 '8753 p P G MORGAN Section alon g Line EF, Papakaio and Oamaru Survey Districts. - DIRECTOR — ical — Reference to Geolo i^ Colours. A wamoa Sync/ine RECENT AND Branch of Waiareka Creek YOUNGER PLEISTOCENE River gravels, forming river flats and low terraces 800' Oamaru Creek Grant Stream OLDER PLEISTOCENE High level gravels The Sea AWAM AN Blue marine clays and sandy shell beds Section alon g Line CD. Awamoko and Oamaru Survey Districts. HUrCHINSONIAN Greensands and gleuconitic sandstones Deborah (= Hutchinson's Quarry) Limestone Awamoa Syncline OTOTARAN Deborah (^Mineral) Tuffs Waiareka Anticline Ui Z Oamaru Stone _ Kaiarero Creek Kakanui River Cape Wan brow O Waiareka Creek Main South M o WAIAREKAN Waiareka tuffs and minor lava flows. (pillow lavas).-- Awamoa Creek Main Trunk RIy. NG SEIdersl/e blue clays, micaceous sandstones, quartzose^ A PARAN with lignite seam.- The Sea igrits and conglomerates S 11 Section alon g Line AB, Oamaru Survey District.
    [Show full text]
  • Scanned Using Fujitsu 6670 Scanner and Scandall Pro Ver 1.7
    1487 1970/223 THE FRESHWATER FISHERIES REGULATIONS (SOUTH CANTERBURY AND WAITAKI VALLEY) MODIFICATION NOTICE 1970 PURSUANT to the Fisheries Act 1908 and the Freshwater Fisheries Regulations 1951, and, in relation to clause 4 (e) hereof, on the written application of the South Canterbury Acclimatisation Society and the Waitaki Valley Acclimatisation Society, the Minister of Marine hereby gives the following notice. NOTICE 1. Title-This notice may be cited as the Freshwater Fisheries Regulations (South Canterbury and Waitaki Valley) Modification Notice 1970. 2. Commencement-This notice shall come into force on the day after the date of its notification in the Gazette. 3. Application-This notice shall be in force only within the South Canterbury and Wa~taki Valley Acclimatisation Districts (including Lakes Aviemore and Benmore where it shall apply except as modified by the Fisheries Experimental Waters (Lakes Aviemore and Benmore) Regulations 1969*). 4. Modification of regulations-The Freshwater Fisheries Regulations 1951 t are hereby modified as follows: Limit Bag (a) No person shall on anyone day take or kill- (i) In the South Canterbury Acclimatisation District, more than 15 acclimatised fish (being trout or salmon), of which not more than 4 may be salmon and not more than 12 may be trout, of which trout not more than 4 may be taken from Lakes Alexandrina and McGregor, including their tributaries, and not more than 8 may be taken from any other lake or lakes, including their tributaries, or from rivers and their tributaries, west of Burke's Pass: (ii) In the Waitaki Valley Acclimatisation District, more than 10 acclimatised fish (being trout or salmon), of which not more than 4 may be salmon and not more than 8 may be trout: *S.R.
    [Show full text]
  • Waitaki/Canterbury Basin
    GEOSCIENCES 09 Annual Conference Oamaru, NZ FIELD TRIP 11 WAITAKI/CANTERBURY BASIN Sunday 22 November to Monday 23 November Leader: Ewan Fordyce Geology Dept, University of Otago BIBLIOGRAPHIC REFERENCE: Fordyce, E. (2009). Waitaki/Canterbury Basin. In: Turnbull, I.M. (ed.). Field Trip Guides, Geosciences 09 Conference, Oamaru, New Zealand. Geological Society of New Zealand Miscellaneous Publication 128B. 23 p. Introduction , Trip 11: Waitaki/Canterbury Basin Day 1 : short stop at Vanished World Centre [see also mid-conference trip #7]; Wharekuri Creek (Oligocene near-basin margin = a shoreline nearby in "drowned" NZ); Corbies Creek/Backyards (basement - Kaihikuan fossiliferous Triassic marine); Hakataramea Valley (Paleogene nonmarine to marine, including richly fossiliferous Oligocene, and Quaternary block faulting); Waihao Valley (if time permits - Eocene large forams and other warm-water fossils and/or Oligocene unconformities). Night in Waimate. Day 2 : Otaio Gorge (Paleogene-early Miocene nonmarine-marine sequence); Squires Farm (Oligocene unconformity); Makikihi (Plio-Pleistocene shallow marine to nonmarine fossiliferous strata); Elephant Hill Stream (Early Miocene; start of Neogene basin infill). Which localities are visited will depend on weather, time taken at early stops, and farm/quarry activities which normally don’t prevent access - but may occasionally. The guide draws on some material from earlier guides (Fordyce & Maxwell 2003, and others cited). Graphics, photos, and field observations, are by Ewan Fordyce unless indicated.
    [Show full text]
  • The Year 2012: Slightly Cooler Than Average for Most Areas
    National Climate Summary: 2012 Issued: 10 January 2013 The year 2012: Slightly cooler than average for most areas Rainfall A relatively dry year for western areas of both Islands. Above normal rainfall for Gisborne, parts of Central Otago, and between Oamaru and Timaru. Temperatures Below average temperatures over the northeast South Island, also Wellington, Wairarapa, parts of the Manawatu, and between Tararua District and the Waikato. Near or slightly below average temperatures elsewhere. Sunshine Sunnier than normal for western areas from Te Kuiti to the Kapiti Coast, as well as the West Coast of the South Island. Below normal sunshine for Wellington, Wairarapa, Blenheim, Northland and Central Otago. Near normal sunshine elsewhere. Soil moisture At the end of the year significant soil moisture deficits were present in eastern areas of both Islands, as well as Auckland, Manawatu, Wellington, Nelson, Otago, and central Southland. Click on the following links to jump to the information you require: Overview Prevailing climate patterns The year in review Rainfall anomaly maps Temperature anomaly maps The numbers Annual rainfall Annual temperature Annual sunshine 2012 climate in the six main centres Significant extremes Overview The year 2012 was rather dry and sunny in western areas of both Islands, but annual rainfall in eastern areas of both Islands was generally near normal or above normal. Many regions experienced a somewhat cool year. Annual mean sea level pressures were slightly lower than usual across New Zealand in 2012, but the circulation anomaly for the year was rather weak. More easterly circulation than normal affected the country for the first five months of the year, as well as in August.
    [Show full text]
  • Headwater Trout Fisheries Ln New Zealand
    Headwater trout fisheries ln New Zealand D.J. Jellyman E" Graynoth New Zealand Freshwater Research Report No. 12 rssN 1171-9E42 New Zealmtd, Freshwater Research Report No. 12 Headwater trout fïsheries in New Zealand by D.J. Jellyman E. Graynoth NI\ryA Freshwater Christchurch January 1994 NEW ZEALAND FRBSHWATER RESEARCH REPORTS This report is one of a series issued by NItilA Freshwater, a division of the National Institute of Water and Atmospheric Research Ltd. A current list of publications in the series with their prices is available from NIWA Freshwater. Organisations may apply to be put on the mailing list to receive all reports as they are published. An invoice will be sent for each new publication. For all enquiries and orders, contact: The Publications Officer NIWA Freshwater PO Box 8602 Riccarton, Christchurch New Zealand ISBN 0-47848326-2 Edited by: C.K. Holmes Preparation of this report was funded by the New Zealand Fish and Game Councils NIWA (the National Institute of Water and Atmospheric Research Ltd) specialises in meeting information needs for the sustainable development of water and atmospheric resources. It was established on I July 1992. NIWA Freshwater consists of the former Freshwater Fisheries Centre, MAF Fisheries, Christchurch, and parts of the former Marine and Freshwater Division, Department of Scientific and Industrial Research (Hydrology Centre, Christchurch and Taupo Research hboratory). Ttte New Zealand Freshwater Research Report series continues the New Zealand Freshwater Fßheries Report series (formerly the New Zealand. Ministry of Agriculture and Fisheries, Fisheries Environmental Repon series), and Publications of the Hydrology Centre, Chrßtchurch. CONTENTS Page SUMMARY 1.
    [Show full text]
  • Geology of the Waitaki Area
    GEOLOGY OF THE WAITAKI AREA P. J . FORSYTH ( COMPILER) BffiLlOGRAPIllC REFERENCE Forsyth , I'J.(compiler) 2001: Geology of the Waitaki area. Institute of Geological & Nuclear Sciences 1:250 000 geological map 19. I sheet + 64p. l..ower Hutt, New Zealand. lnstitute ofGeologicaJ & Nuclear Sciences Limited. Development and maintenanceof ARCIINFO GIS database by D.W. Heron and M.S. Ratlenbury GIS operations by D.W. Heron, B. Smith-Lyttle, B. Morri son and D.Thomas Contributions to offshore geology by A. Duxtield, R.H. Herzer &B.o. Field Edited by D.W. Heron and MJ. Isaac Prepared for publication by P.L. Murray Printed by Graphic Press & Packaging Ltd, Levin ISBN 0-478-09739-5 © Copyri ght Institute of GeologicaI& Nuclear Sciences Limited 200 I FRONT COVER The Waitaki River valley, looking upstream from near Kurow. The modern flood plain has a vegetation cover of scrub and willow, but areas above flood level are intensively farmed. Kurow (middle distance) lies below Kurow Hill and the lower slopes of the 51 Marys Range. Hydroelectric storage lakes are impounded behind the Waitaki and Aviemore dams. The ranges in view are formed of Rakaia terrane sandstone. mudstone and semischist. Photo CN42818-20: D.L. Homer GEOLOGY OF THE WAITAKI AREA Scale 1:250 000 P. J. FORSYTH (COMPILER) Institute of Geological & Nuclear Sciences 1:250 000 geological map 19 Institute of Geological & Nuclear Sciences Limited Lower Hutt, New Zealand 2001 CONTENTS ABSTRACT iv TECTO IC HISTORY 40 Keywords.................................................................. v Paleozoic to Mesozoic 40 Late Cretaceous to Midd le Miocene 40 INTRODUCTION . Late Miocene and Pliocene 40 Quaternary tectonics.
    [Show full text]
  • National Directory Master
    National Directory and Delivery Guide Page 3 May 2015 National Directory and Delivery Window Guide PLACE DESCRIPTION DESTINATION ETA SAT DEL ABBOTSFORD Suburb Of Dunedin DUD EM V ABBOTSHILL Suburb Of Dunedin DUD EM . ABBY CAVES Suburb Of Whangarei WRE EM . ABUT HEAD 118 Kms From Greymouth GYM (NZC) ONFWD TO AGENT . ACACIA BAY 6 Kms From Taupo TPO LM . ACHRAY 108 Kms From Christchurch CHC ONFWD TO AGENT . ADAIR 8 Kms From Timaru TIU ONFWD TO AGENT . ADAMS FLAT 79 Kms From Dunedin DUD ONFWD TO AGENT . ADDINGTON Suburb Of Christchurch CHC EM V ADDISONS 11 Kms From Westport WSP (NZC) ONFWD TO AGENT . ADELE ISLAND Tasman Bay NSN ONFWD TO AGENT . ADMIRAL HILL 35 Kms From Masterton MAS ONFWD TO AGENT . ADMIRALTY BAY 64 Kms From Nelson NSN ONFWD TO AGENT . AHAURA 35 Kms From Greymouth GYM (NZC) ONFWD TO AGENT . AHIARUHE 40 Kms From Masterton MAS ONFWD TO AGENT . AHIKIWI 80 Kms From Whangarei WRE (NZC) ONFWD TO AGENT . AHIKOUKA 25 Kms From Masterton MAS ONFWD TO AGENT . AHIMIA 43 Kms From Thames THS ONFWD TO AGENT . AHIPARA 14 Kms From Kaitaia KAT (NZC) ONFWD TO AGENT . AHIRAU 40 Kms From Gisborne GIS (NZC) ONFWD TO AGENT . AHIROA 105 Kms From Thames THS ONFWD TO AGENT . AHITI 27 Kms From Gisborne GIS (NZC) ONFWD TO AGENT . AHITITI 27 Kms From Gisborne GIS (NZC) ONFWD TO AGENT . AHITITI 68 Kms From New Plymouth NPL ONFWD TO AGENT . AHOROA 38 Kms From Hawera NPL ONFWD TO AGENT . AHUITI 65 Kms From Wanganui WAG ONFWD TO AGENT . AHURANGI 74 Kms From Wanganui WAG ONFWD TO AGENT .
    [Show full text]
  • Kiwisaldula Waiho and K. Hurunui, Two New Species of Saldidae (Hemiptera: Heteroptera) from the South Island of New Zealand, with Redescriptions of K
    Zootaxa 4341 (1): 041–055 ISSN 1175-5326 (print edition) http://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2017 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4341.1.3 http://zoobank.org/urn:lsid:zoobank.org:pub:2DA6B97F-06AF-4ECF-ADBB-23F9A9E7292D Kiwisaldula waiho and K. hurunui, two new species of Saldidae (Hemiptera: Heteroptera) from the South Island of New Zealand, with redescriptions of K. butleri (White) and K. laelaps (White) MARIE-CLAUDE LARIVIÈRE & ANDRÉ LAROCHELLE New Zealand Arthropod Collection, Landcare Research, Private Bag 92170, Auckland 1142, New Zealand. E-mail: [email protected]; [email protected] Abstract Kiwisaldula waiho new species and K. hurunui new species, are described from the South Island of New Zealand. Kiwisaldula butleri (White, 1878) and K. laelaps (White, 1878), two taxonomically little-known taxa, are redescribed. Morphological descriptions are provided together with illustrations emphasising the most important diagnostic features of external morphology and male genitalia. Information is given on synonymy, type specimens, material examined, geo- graphic distribution and biology. Key words: shore bugs, revision, systematics, biodiversity Introduction This is the third in a series of papers aiming to revise the taxonomy of New Zealand Saldidae (Hemiptera: Heteroptera) and to provide comprehensive information on their geographic distribution and biology. Larivière & Larochelle (2015) erected the genus Zemacrosaldula which occurs on both main islands of New Zealand and contains four species. Subsequently, these workers (Larivière & Larochelle 2016) studied the North Island and nearby offshore islands saldids, and the type series of two South Island species. This resulted in the establishment of two new genera (Aoteasalda, one species; Kiwisaldula, six species) and completed the generic re- assignment of all New Zealand shore bug species previously assigned to the genus Saldula Van Duzee, 1914 (sensu lato).
    [Show full text]