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Friday Mosque Of
No.2330,Monday,17 May,2021 www.TOURISMpaper.com Some 20 historical objects have recently been confiscated from three smugglers in The World`s Only Print Tourism Newspaper Kuhdasht, western Lorestan province, a senior police official in charge of protecting cultural heritage said on Friday, CHTN reported. Including a decorative box, statue base, tray, and a few coins, the relics which had been embedded inside a car, were discovered during a routine inspection, Moham- Iranian Police madrezaMoradian announced. The official, however, did not refer to the exact age of the relics. The culprits were Seize Relics from detained and surrendered to the judicial system for further investigation, he noted. Smugglers 4 cooking Some $2m Paid to Support Tourism BozGhormeh Stew BozGhormeh Stew is a traditional recipe Businesses in South Khorasan from Kerman. Kerman is located in the he Iranian government has paid though to tempt archaeologists (rela- southeast of Iran. 1 lb (454g) Stew Beef. some 85 billion rials (over $2 tively accessible Old Esfandiar and Old Inredients: T million at the official exchange Deyhuk are amongst our favorites). ■ 1 Cup Garbanzo Beans rate of 42,000 rials per dollar) in loans Castle lovers will swoon over Birjand’s ■ 6 oz (170g) Whey Kashk to the tourism businesses affected by fortress – which might be slightly over- ■ 1 Onion the coronavirus pandemic in the eastern restored but make a great site for a tradi- ■ 2 Garlic Cloves province of South Khorasan. tional restaurant – and the mountain-top ■ 1/4 Tsp Saffron The loans have been paid to travel agen- fortifications at Qa’en, especially magi- ■ Turmeric cies, tourist complexes, and tour leaders cal at sunset; Forg is one of the most ■ Salt, White Pepper as well as handicrafts units across the picture-perfect castle-citadels in Iran. -
Pleistocene Rodents of the British Isles
PLEISTOCENE RODENTS OF THE BRITISH ISLES BY ANTONY JOHN SUTCLIFFE British Museum (Natural History), London AND KAZIMIERZ KOWALSKI Institute of Systematic and Experimental Zoology, Polish Academy of Sciences, Krakow, Poland Pp. 31-147 ; 31 Text-figures ; 13 Tables BULLETIN OF THE BRITISH MUSEUM (NATURAL HISTORY) GEOLOGY Vol. 27 No. 2 LONDON: 1976 THE BULLETIN OF THE BRITISH MUSEUM (natural history), instituted in 1949, is issued in five series corresponding to the Scientific Departments of the Museum, and an Historical series. Parts will appear at irregular intervals as they become ready. Volumes will contain about three or four hundred pages, and will not necessarily be completed within one calendar year. In 1965 a separate supplementary series of longer papers was instituted, numbered serially for each Department. This paper is Vol. 27, No. 2, of the Geological [Palaeontological) series. The abbreviated titles of periodicals cited follow those of the World List of Scientific Periodicals. World List abbreviation : Bull. Br. Mus. nat. Hist. (Geol. ISSN 0007-1471 Trustees of the British Museum (Natural History), 1976 BRITISH MUSEUM (NATURAL HISTORY) Issued 29 July, 1976 Price £7.40 . PLEISTOCENE RODENTS OF THE BRITISH ISLES By A. J. SUTCLIFFE & K. KOWALSKI CONTENTS Page Synopsis ........ 35 I. Introduction ....... 36 A. History of Studies ..... 37 B. The Geological Background .... 40 II. Localities in the British Isles with fossil rodents 42 A. Deposits OF East Anglia . .... 42 (i) Red Crag 43 (ii) Icenian Crag ....... 43 (iii) Cromer Forest Bed Series ..... 46 (a) Pastonian of East Runton and Happisburgh 47 (b) Beestonian ...... 48 (c) Cromerian, sensu stricto .... 48 (d) Anglian ...... -
Extraction of Sand from the Colo River and Processing of Sand on Portion 37, Lower Colo Road, Colo
.. ";0Cl4 ~ /,blf/(' Report to the Honourable Bob Carr Minister for Planning and Environment An Inquiry pursuant to Section 119 of the Environmental Planning and Assessment Act, 1979, into a development application EXTRACTION OF SAND FROM THE COLO RIVER AND PROCESSING OF SAND ON PORTION 37, LOWER COLO ROAD, COLO John Woodward, Chairman COMMISSIONER OF INQUIRY September 1985 f \, F i i S Y D N E Y ,:j it September 1985 ( !'. 1, . TO MINISTER FOR PLANNING AND ENVIRONMENT j \ On 18th January 1985, you directed that an inquiry be ,I. '/ held in accordance with Section 119 of the Environmental Planning and Assessment Act 1979, by a Commission of Inquiry ( with respect to a development application to dredge sand from the Colo River adjacent to portion 37, Lower Colo, in the Shire of Hawkesbury. You commissioned me to conduct ) the inquiry into the proposed development and to report \., my findings and recommendations to you . The public inquiry was held at Sydney commencing on 30th July, 1985. During the course of the inquiry adjournments were granted to allow certain parties further time to prepare their submissions to the inquiry. Field visits were conducted in the presence of the parties to the proposed dredging site on the Colo River, to adjoin ing lands and to nearby properties held by obj ectors to the development and to other vantage points in the area. The public sessions of the inquiry concluded on 14th August 1985. This report is made to you pursuant to the provisions of the Act and sets ")tit my findings and recommendations on the issues raised ,during the course of the inquiry. -
The Falling Netanyahu Takes Down a Cantankerous Political Class
WWW.TEHRANTIMES.COM I N T E R N A T I O N A L D A I L Y 8 Pages Price 50,000 Rials 1.00 EURO 4.00 AED 43rd year No.13954 Saturday MAY 29, 2021 Khordad 8, 1400 Shawwal 17, 1442 Elections is Brighton’s Alireza Steel ingot export Germany recognizes competition to Jahanbakhsh to decide rises 135% in colonial-era massacres in serve people Page 2 on his future Page 3 a month on year Page 4 Namibia as genocide Page 5 Unity is the secret behind the Resistance’s victories: Amir-Abdollahian TEHRAN - Hossein Amir-Abdollahian, the resistance and steadfastness victory could special aide to the speaker of the Iranian be achieved. This victory sent an important Parliament on international affairs, has re- message that the Zionist enemy only under- flected on the secret behind the recent victory stands the language of force and resistance,” of the Palestinian resistance against Israel. he told the Lebanese Al-Ahed News. Amir-Abdollahian said the 2006 victo- The Iranian diplomat added, “This ry of the Lebanese resistance movement victory and other victories achieved by against Israel raised faith in the resistance the resistance, especially the victory of and sent a message that Israel understands July 2006, were achieved in light of the only the language of power. unity of the Lebanese people and the gold- “The flight of the Zionist entity from en equation in Lebanon – the army, the southern Lebanon raised faith in the resist- people, and the resistance. Crabs in ance among the Lebanese, and that through Continued on page 3 Tehran, Moscow confer on joint investment in agricultural sector TEHRAN – Iranian Agriculture Minis- investment in various agricultural fields. -
Hobby's Outreach
HOBBY'S OUTREACH Newsletter ef: BLUE MOUNTAINS HISTORICAL SOCIETY Inc. ISSN 1835-3010 P 0Box17, WENT\VORTH FAILS NSW 2782 Telephone: (02) 4757 3824 Hobby's Reach, 99 Blaxland Road, Wentworth Falls, NSW Email: [email protected] !Volume 20 Number3 August - September 20081 5 APRIL 2008 MEETING Contributed lry Colin Slade Continued from June-July issue The Garden Palace and The International Exhibition Sydney 1879 ,,,,":(a, -i-e-c-e-14~ 'f 111-i:J,'l"fll, !""""""'"" ,.,,1,7(e-~ During the first three days of the Exhibition some eighteen thousand visitors (excluding exhibitors and officials) passed -.... through the gates and an uneasy doubt was felt among the Commissioners as to the popular appeal of the Show. But Saturday 27 September, the first 'Shilling Day', banished all apprehension as 30,000 visitors crowded the Garden Palace and applauded a repeat performance of the Exhibition Cantata and the Hallelujah Chorus. The Sydney tram system owes its origins to the Exhibition. The first tram lines were laid from the nearest railway station at Redfern to Hunter Street to bring visitors in a double-decked carriage driven by a newly built steam tram. After the Exhibition this tram line was doubled all the way and extended to the eastern, southern and western suburbs. Among the many exhibits, only to name but a few from all over the world, included a Turkish Bazaar, Japanese Tea House, 116 samples of tea from different countries, Emerson's Oyster Saloon, a Maori House, Austro-Hungarian Wme and Beer Tasting Hall. A Fijian house, for a time inhabited by dancing natives claiming to have been cannibals, The Australian Dairy (a glass of fresh, cold milk for a penny), 20 kingdoms, republics and colonies were represented. -
The Vegetation of the Western Blue Mountains Including the Capertee, Coxs, Jenolan & Gurnang Areas
Department of Environment and Conservation (NSW) The Vegetation of the Western Blue Mountains including the Capertee, Coxs, Jenolan & Gurnang Areas Volume 1: Technical Report Hawkesbury-Nepean CMA CATCHMENT MANAGEMENT AUTHORITY The Vegetation of the Western Blue Mountains (including the Capertee, Cox’s, Jenolan and Gurnang Areas) Volume 1: Technical Report (Final V1.1) Project funded by the Hawkesbury – Nepean Catchment Management Authority Information and Assessment Section Metropolitan Branch Environmental Protection and Regulation Division Department of Environment and Conservation July 2006 ACKNOWLEDGMENTS This project has been completed by the Special thanks to: Information and Assessment Section, Metropolitan Branch. The numerous land owners including State Forests of NSW who allowed access to their Section Head, Information and Assessment properties. Julie Ravallion The Department of Natural Resources, Forests NSW and Hawkesbury – Nepean CMA for Coordinator, Bioregional Data Group comments on early drafts. Daniel Connolly This report should be referenced as follows: Vegetation Project Officer DEC (2006) The Vegetation of the Western Blue Mountains. Unpublished report funded by Greg Steenbeeke the Hawkesbury – Nepean Catchment Management Authority. Department of GIS, Data Management and Database Environment and Conservation, Hurstville. Coordination Peter Ewin Photos Kylie Madden Vegetation community profile photographs by Greg Steenbeeke Greg Steenbeeke unless otherwise noted. Feature cover photo by Greg Steenbeeke. All Logistics -
Two Centuries of Botanical Exploration Along the Botanists Way, Northern Blue Mountains, N.S.W: a Regional Botanical History That Refl Ects National Trends
Two Centuries of Botanical Exploration along the Botanists Way, Northern Blue Mountains, N.S.W: a Regional Botanical History that Refl ects National Trends DOUG BENSON Honorary Research Associate, National Herbarium of New South Wales, Royal Botanic Gardens and Domain Trust, Sydney NSW 2000, AUSTRALIA. [email protected] Published on 10 April 2019 at https://openjournals.library.sydney.edu.au/index.php/LIN/index Benson, D. (2019). Two centuries of botanical exploration along the Botanists Way, northern Blue Mountains,N.S.W: a regional botanical history that refl ects national trends. Proceedings of the Linnean Society of New South Wales 141, 1-24. The Botanists Way is a promotional concept developed by the Blue Mountains Botanic Garden at Mt Tomah for interpretation displays associated with the adjacent Greater Blue Mountains World Heritage Area (GBMWHA). It is based on 19th century botanical exploration of areas between Kurrajong and Bell, northwest of Sydney, generally associated with Bells Line of Road, and focussed particularly on the botanists George Caley and Allan Cunningham and their connections with Mt Tomah. Based on a broader assessment of the area’s botanical history, the concept is here expanded to cover the route from Richmond to Lithgow (about 80 km) including both Bells Line of Road and Chifl ey Road, and extending north to the Newnes Plateau. The historical attraction of botanists and collectors to the area is explored chronologically from 1804 up to the present, and themes suitable for visitor education are recognised. Though the Botanists Way is focused on a relatively limited geographic area, the general sequence of scientifi c activities described - initial exploratory collecting; 19th century Gentlemen Naturalists (and lady illustrators); learned societies and publications; 20th century publicly-supported research institutions and the beginnings of ecology, and since the 1960s, professional conservation research and management - were also happening nationally elsewhere. -
Pleistocene - History of Earth's Climate
Pleistocene - History of Earth's climate http://www.dandebat.dk/eng-klima5.htm History of Earth's Climate 5. - Cenozoic II - Pleistocene Home DH-Debate 4. Tertiary Introduction - The Pleistocene Ice Ages - The climate in the ice-free part of the World - During Last Glacial Maximum, the World became cold and 6. End of Pleistocene dusty - Temperature and CO2 - Milankovic Astronomical Climate Theory - Interglacials and other warm Periods - The Super volcano Toba - Links og literature Introduction Pleistocene is the period in Earth's history that we commonly refer to as the Ice Age. Through much of this period, the Earth's northern and southern regions were covered by kilometer thick glaciers. It is important to recognize that the Pleistocene was a series of real ice ages, separated by relatively short interglacial periods. The Pleistocene started 2.6 million years ago and lasted until the termination of the Weichsel glaciation about 11,711 years ago. Timeline of Earth's geological periods. Time progresses from right to left. The glowing inferno just after Earth was formed is named Hadean. In Archean water condensed and an atmosphere of nitrogen and methane was formed together with the first rocks that we know about. In Proterozoic cyano bacteria produced oxygen, which oxidized iron and methane, in the end of the period life emerged on the seabed. Phanerozoic represents the era in which there have been visible tangible life. It is divided in Paleozoic, Mesozoic and Cenozoic. Paleozoic was the period of early life. Mesozoic was the time of the dinosaurs, and Cenozoic is the era of mammals, which latter further is divided into Tertiary and Quaternary. -
13. Late Pliocene-Pleistocene Glaciation
13. LATE PLIOCENE - PLEISTOCENE GLACIATION W. A. Berggren, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts The discussion in this chapter is broken down into two increase in the former exceeding that of the latter; or parts: the first deals with glaciation in the North Atlantic as (v) less detritals, clay and carbonate deposited per unit time revealed in the data obtained on Leg 12; in the second part (that is, decreased sedimentation rate) with the decrease in an attempt is made to provide a chronologic framework of the latter exceeding the former. In view of the demon- Late Pliocene-Pleistocene glaciation and to correlate gla- strable increase in sedimentation rate above the preglacial/ cial/interglacial sequences as recorded in land and deep-sea glacial boundary at Sites 111, 112 and 116 due to increased sediments. amounts of detrital minerals and the fact that glacial periods in high latitudes are characterized by a carbonate GLACIATION IN THE NORTH ATLANTIC minimum (Mclntyre et al., in press) it can be seen that the One of the most significant aspects of Leg 12 was the correct explanation for the increase in natural gamma activ- various results which were obtained regarding glaciation in ity in the glacial part of the section is rather complex. Thin the North Atlantic. Glacial sediments were encountered at bands of carbonate were found at various levels intercalated all sites in the North Atlantic with the exception of Site with detrital-rich clays which indicates interglacial intervals, 117 (for the purpose of this discussion the North Atlantic so that the correct explanation probably lies with (iii) encompasses Sites 111 through 117; Sites 118 and 119 are above. -
Dsdp42pt2 Index.Pdf
INDEX Absorption chromatography, bitumoids, 683 Azov, Sea of, Caspibraackish ostracodes from, 1039 Acritarchs, 993 Background and objectives, Site 379, 30 Aegean Sea, present-day salinity values, 643 Site 380, 120 Afig Formation, 1208 Site 381, 294 Age determinations based on pollen, 515 Bacteria, sulfate-reducing, 767 radiocarbon values, 627 Bacterial activity, carbon dioxide reduction, 673 varves, 483 controlled by methane production, 649 Algerian continental margin, 1181 Bacterial densities in Black Sea sediments, 769 Algerian shelf, tectonic activity, 1181 Bacterial sulfate reduction, depositional environment of, 625 Alkaline metal content, Black Sea sediments, 597 Balearic Basin, 1100 Alkanes, 697 Barite, 423 Alloisoleucine-isoleucine ratios, dependence on deposi- Bathymetry, Black Sea, 360, 1043 tional environment, 700 Belaya River, 413 Alpha cold period, 30, 41, 147, 299, 997 Benthic foraminifers from sediments of western shelf, Black Alpha glacial stage, 133, 513, 516 Sea, 783 Aluminosilicates, Hole 379A, 531 Benthic foraminifers, as salinity indicators, 493 Amino acid abundances, effect of depth on, 699 Hole 380, 146 Effects of reducing and oxidizing environment on, 699 Site 381, 298 Hole 379A, 699, 704, 727 Benthic ostracodes from Lake Erie, 1039 Hole 380A, 699 Benthic ostracodes from Great Lakes, 1039 Site 381, 699, 727 Benzene, 673 temporal variations in, 699 Bering Sea sediments, 744 Amino acids, 725, 1176 Bet Guvrin formation, 1197 Amino acids in Black Sea sediment samples, 698 description of, 1201 Amorphous silica, geochemistry -
Mountain-Derived Versus Shelf-Based Glaciations on the Western Taymyr Peninsula, Siberia Christian Hjort1 & Svend Funder2
Mountain-derived versus shelf-based glaciations on the western Taymyr Peninsula, Siberia Christian Hjort1 & Svend Funder2 1 Quaternary Sciences, Lund University, GeoCenter II, Sölvegatan 12, SE-223 62 Lund, Sweden 2 Natural History Museum, University of Copenhagen, Øster Voldgade 5-7, DK-1350 Copenhagen K, Denmark Keywords Abstract Siberian geology; glacial inception; glacial history. The early Russian researchers working in central Siberia seem to have preferred scenarios in which glaciations, in accordance with the classical gla- Correspondence ciological concept, originated in the mountains. However, during the last 30 C. Hjort, Quaternary Sciences, Lund years or so the interest in the glacial history of the region has concentrated on University, GeoCenter II, Sölvegatan 12, ice sheets spreading from the Kara Sea shelf. There, they could have originated SE-223 62 Lund, Sweden. E-mail: from ice caps formed on areas that, for eustatic reasons, became dry land [email protected] during global glacial maximum periods, or from grounded ice shelves. Such ice doi:10.1111/j.1751-8369.2008.00068.x sheets have been shown to repeatedly inundate much of the Taymyr Peninsula from the north-west. However, work on westernmost Taymyr has now also documented glaciations coming from inland. On at least two occasions, with the latest one dated to the Saale glaciation (marine isotope stage 6 [MIS 6]), warm-based, bedrock-sculpturing glaciers originating in the Byrranga Moun- tains, and in the hills west of the range, expanded westwards, and at least once did such glaciers, after moving 50–60 km or more over the present land areas, cross today’s Kara Sea coastline. -
D. Palaeozoological Research
Eiszeitalter u. Gegenwart Band 23/24 Seite 333-339 Öhringen/Württ., 15. Oktober 1973 D. Palaeozoological Research by HORST REMY, Bonn translated by U. BUREK, S. CHRULEV and R. THOMAS, Tübingen 1. Molluscs Comprehensive studies of Pleistocene land- and freshwater molluscs have so far been largely restricted to the faunas of interglacial and Würmian glacial deposits, and to the history of postglacial faunas. ANT has reconstructed the postglacial history of changes in landsnail distributions in NW-Germany and Westphalia (ANT 1963a, 1967). The present day fauna consists of a preexisting fauna ("Urfauna") together with postglacial immi grants. The elements of the "Urfauna" are eurythermal species, which were already living in NW-Germany during Würm Glaciation. These species comprise about 24 °/o of the present day fauna. In the South German periglacial region this portion is rather higher. Microclimatic conditions must have been more favourable in this region, presumably because the influence of the alpine ice mass was not as strong as that of the continental ice sheet to the north. There were many ecological niches whose local climates were more favourable for the survival of such species. Along the south coast of England, SW of the land connection with the continent, several migrant species survived (Atlanto-Britannic Fauna). In the forested region west of the Urals, the species wich today constitute the Siberio-Asiatic Fauna survived, while the immigrant species of the Mediterranean Fauna survived on the E-coast of Spain, on the W-coast of Italy and SE-Europe. It is not yet certain where some of the immigrant species lived during the glaciation; possibly these forms survived the ice age in S-Germany and the adjoining regions.