DOCSLIB.ORG

TT Commons Font Family Type Specimen

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
TT Commons Font Family Type Specimen TT Commons Font Family Type Specimen TT Commons Design TypeType Release Date Feb 26, 2018 Publisher TypeType Styles 18 styles File Formats otf, ttf, woff, eot, svg www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 2 About TT Commons TT Commons is a universal sans serif with Initially, we did not plan to release this font The typeface intentionally does not have a minimal contrast of strokes, a closed aper- for sale, but given the number of incoming distinctive decorative details. On the contrary, ture and geometric shapes of characters. The requests, we changed our decision. At the it wins hearts with his laconism, simplicity and design of the typeface was developed for the same time, we have significantly improved the sharpness of forms, which set the seasoned widest possible range of tasks with which any typeface: we increased the number of faces corporate style for years to come. quality corporate font is required to cope. to 18, added small capitals for the Latin and The name TT Commons comes from the word The history of TT Commons originates from Cyrillic alphabets, expanded the character 'common' (widely accepted, typical, frequent) the new TypeType logo, which appeared case to 771 glyphs, introduced 18 OpenType —this typeface can be used for any everyday in late 2016 as part of the rebranding project. features, and included trial hinting (ClearType tasks related to typography. And small Ideas embedded in the logo formed the basis and DirectWrite) performed at our studio by capitals, stylistic alternates, ligatures, arrows, of two fully developed faces (regular and me- our team. Low contrast strokes and averaged different types of figures and other features dium), which in early 2017 became the official drawing of letters makes TT Commons excel- (ordn, frac, case, c2sc, smcp, sinf, sups, numr, corporate typeface of the TypeType Foundry. lent for large arrays of text. On the other hand, dnom, tnum, onum, lnum, pnum, liga, dlig, calt, individually developed design of each glyph salt, ss01) add significant functionality. If you makes it possible to use it successfully as are in doubt about which font to choose, pick a display font. TT Commons, it will definitely work. 123 TT Commons Medium 180 pt AaBb www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 3 About TT Commons TT Commons is available in 9 weights (Thin, ExtraLight, Light, Regular, Meduim, DemiBold, Bold, ExtraBold, and Black) and 9 true match- ing italics. Weights Italics TT Commons Thin TT Commons Thin Italic TT Commons ExtraLight TT Commons ExtraLight Italic TT Commons Light TT Commons Light Italic TT Commons Regular TT Commons Regular Italic TT Commons Medium TT Commons Medium Italic TT Commons DemiBold TT Commons DemiBold Italic TT Commons Bold TT Commons Bold Italic TT Commons ExtraBold TT Commons ExtraBold Italic TT Commons Black TT Commons Black Italic www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 4 Examples While the north of the peninsula was Soon afer, the Pomors were followed already settled in the 7th–5th millen- by the tribute collectors from the nium BCE, the rest of its territory Novgorod Republic, and the penin- remained uninhabited until the 3rd sula gradually became a part of the millennium BCE. Novgorodian lands. TT Commons Thin 16 pt TT Commons Thin Italic 16 pt By the end of the 19th century, the Nevertheless, the economy rebound- indigenous Sami population had ed somewhat in the first decade of been mostly forced north by the the 2000s and the peninsula remains Russians as well as by newly arriving the most industrially developed and Izhma Komi and Kominized Nenets. urbanized region in northern Russia. TT Commons ExtraLight 16 pt TT Commons ExtraLight Italic 16 pt The peninsula is covered by taiga It is located in the far northwest in the south and tundra in the north, of Russia, almost completely inside where permafrost limits the growth the Arctic Circle and is washed by of the trees resulting in landscape the Barents Sea in the north and the dominated by shrubs and grasses. White Sea in the east and southeast. TT Commons Light 16 pt TT Commons Light Italic 16 pt www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 5 Examples Because the last ice age removed Deposits of construction materials the top sediment layer of the soil, such as granite, quartzite are also the Kola Peninsula is on the surface abundant. Diatomaceous earth extremely rich in various ores and deposits are common near lakes minerals. and are used to produce insulation. TT Commons Regular 16 pt TT Commons Italic 16 pt Monsoon winds are common Record highs exceed +30 °C (86 °F) in most areas, with south winds almost on all the territory of the prevailing in winter months and peninsula. First frosts occur as early with somewhat more pronounced as August and may last through easterly winds in summer. May and even June. TTT Commons Medium 16 pt TT Commons Medium Italic 16 pt The peninsula is covered by taiga In northern coastal areas, stony in the south and tundra in the and shrub lichens are common. north. In the tundra, cold and The taiga in the southern areas windy conditions and permafrost is composed mostly of pine trees limit the growth of the trees. and firs. TT Commons DemiBold 16 pt TT Commons DemiBold Italic 16 pt www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 6 Examples Reindeer herds visit the grass- American minks, which were lands in summer. Other animals released near the Olenitsa River include red and Arctic foxes, wol- in 1935–1936, are now common verines, moose, otters, and lynx throughout the peninsula and in the southern areas. are commercially hunted. TT Commons Bold 16 pt TT Commons Bold Italic 16 pt Twenty-nine species of fresh The average temperature in July water fish are recognized on the is about +11 °C (52 °F). Record territory of peninsula, including lows reach −50 °C (−58 °F) in the trout, stickleback, northern central parts and −35 to −40 °C pike, and European perch. (−31 to −40 °F) on the coasts. TT Commons ExtraBold 16 pt TT Commons ExtraBold Italic 16 pt The rivers are an important Strong storm winds blow for habitat for the Atlantic salmon, 80–120 days a year. The waters which return from Greenland of the Murman Coast remain and the Faroe Islands to spawn warm enough to remain ice- in fresh water. free even in winter. TT Commons Black 16 pt TT Commons Black Italic 16 pt www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 7 Supported languages TT Commons supports more than 72 langua- ges including Western, Central, Northern European languages and most of cyrillic. Albanian Filipino Macedonian Spanish Basque Finnish Moldavian Swahili Belarusian French Norwegian Swedish Bosnian Gaelic Polish Turkish Breton German Portuguese Turkmen (Latin) Corsican Hungarian Romanian Ukrainian Croatian Icelandic Russian Zulu Czech Indonesian Sámi (Lule, and others Danish Irish Southern) English Italian Serbian Estonian Latvian Slovak Faroese Lithuanian Slovenian www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 8 По Кольскому полу- острову протекает много рек: Поной (самая длинная река), Варзуга, Кола, Териберка, Йоканга, Воронья, Умба и др. TT Commons Light 60 pt Russian www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 9 Languages Wybrzeża są słabo urozmaicone. Norge hadde råderett over Kola Jest zbudowany z granitów, gnej- frem til 1265. Dette endret seg på sów i łupków krystalicznych, w jego 1200−tallet da russiske pomorer zachodniej części znajduje się oppdaget velstanden av vilt og fisk masyw Chibin (Judyczwumczorr på halvøya. Ikke lenge etter fulgte 1200 m n.p.m.), w części południo- tributtinnsamlere fra Republikken wej nizina przykryta osadami polo- Novgorod, og halvøya ble gradvis dowcowymi. Przez półwysep prze- en del av Novgorod. Ingen perma- pływają liczne zasobne w energię nente bosetninger, derimot, ble rzeki: Ponoj, Warzuga, Umba etablert av novgoroderne før i Jokanga. 1400−tallet. Polish Norwegian Poloostrov má rozlohu přibližně Kuolan niemimaata asuttaa venä- 100 000 km². Severní břeh je läisten lisäksi saamelaisten alku- vysoký a srázný, zatímco jižní břeh peräiskansa. Kantalahden ympä- je nízký a mírný. V západní části ristössä asuneet karjalaiset ovat poloostrova se rozkládají dvě toisen maailmansodan jälkeen pohoří Chibiny a Lovozerské tun- käytännössä sulautuneet venäläi- dry (nadmořská výška do 1 120 m) siin. Kuolaan muutti 1800−luvulla a ve střední části se podél osy myös suomalaisia, jotka kuitenkin poloostrova táhne vysočina Kejvy pakkosiirrettiin kesällä 1942 muual- (do 397 m), tvořící hlavní místní le Neuvostoliittoon toisen maail- rozvodí. mansodan aikana. Czech Finnish www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 10 mösť ñěcėssăry lāņgűåģęs şùppôrt TT Commons Medium 110 pt www.typetype.org TypeType Foundry, St. Petersburg, 2018 TT Commons Font Family Type Specimen 11 Glyphs Basic Character Set Uppercase ABCDEFGHIJKLMNOPQRSTUVWXYZ Lowercase abcdefghijklmnopqrstuvwxyz Figures 0123456789 Cyrillic Uppercase АБВГДЕЁЖЗИЙКЛМНОПРСТУФХЦ ЧШЩЪЫЬЭЮЯЄҐЂЋЉЊЏЃЌЎЈІЇЅ Cyrillic Lowercase абвгдеёжзийклмнопрстуфхц чшщъыьэюяєґђћљњџѓќўјіїѕ Punctuation & Symbols !¡?¿«»‹›.,:;‘’‚“”„…’”|¦-–—_\/()[]{}·•* #§©®¶№™@&†‡°^ Accented Uppercase ÀÁĂÂÄĀÅÃĄÆĆČĈÇĎĐÈÉĚËĖÊĒĘĞĢ ĶĹĽĻŁÌÍÎÏİĪĮŃŇŅÑÒÓÔÖŐŌÕŒØÞŔŘŖ
Load more

Recommended publications
  • Lifespan and Growth of Astarte Borealis (Bivalvia) from Kandalaksha Gulf, White Sea, Russia
    Lifespan and growth of Astarte borealis (Bivalvia) from Kandalaksha Gulf, White Sea, Russia David K. Moss, Donna Surge & Vadim Khaitov Polar Biology ISSN 0722-4060 Polar Biol DOI 10.1007/s00300-018-2290-9 1 23 Your article is protected by copyright and all rights are held exclusively by Springer- Verlag GmbH Germany, part of Springer Nature. This e-offprint is for personal use only and shall not be self-archived in electronic repositories. If you wish to self-archive your article, please use the accepted manuscript version for posting on your own website. You may further deposit the accepted manuscript version in any repository, provided it is only made publicly available 12 months after official publication or later and provided acknowledgement is given to the original source of publication and a link is inserted to the published article on Springer's website. The link must be accompanied by the following text: "The final publication is available at link.springer.com”. 1 23 Author's personal copy Polar Biology https://doi.org/10.1007/s00300-018-2290-9 ORIGINAL PAPER Lifespan and growth of Astarte borealis (Bivalvia) from Kandalaksha Gulf, White Sea, Russia David K. Moss1 · Donna Surge1 · Vadim Khaitov2,3 Received: 2 October 2017 / Revised: 13 February 2018 / Accepted: 21 February 2018 © Springer-Verlag GmbH Germany, part of Springer Nature 2018 Abstract Marine bivalves are well known for their impressive lifespans. Like trees, bivalves grow by accretion and record age and size throughout ontogeny in their shell. Bivalves, however, can form growth increments at several diferent periodicities depending on their local environment.
    [Show full text]
  • Thermochronology and Exhumation History of The
    Thermochronology and Exhumation History of the Northeastern Fennoscandian Shield Since 1.9 Ga: Evidence From 40 Ar/ 39 Ar and Apatite Fission Track Data From the Kola Peninsula Item Type Article Authors Veselovskiy, Roman V.; Thomson, Stuart N.; Arzamastsev, Andrey A.; Botsyun, Svetlana; Travin, Aleksey V.; Yudin, Denis S.; Samsonov, Alexander V.; Stepanova, Alexandra V. Citation Veselovskiy, R. V., Thomson, S. N., Arzamastsev, A. A., Botsyun, S., Travin, A. V., Yudin, D. S., et al. (2019). Thermochronology and exhumation history of the northeastern Fennoscandian Shield since 1.9 Ga:evidence from 40Ar/39Ar and apatite fission track data from the Kola Peninsula. Tectonics, 38, 2317–2337.https:// doi.org/10.1029/2018TC005250 DOI 10.1029/2018tc005250 Publisher AMER GEOPHYSICAL UNION Journal TECTONICS Rights Copyright © 2019. American Geophysical Union. All Rights Reserved. Download date 01/10/2021 04:51:21 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/634481 RESEARCH ARTICLE Thermochronology and Exhumation History of the 10.1029/2018TC005250 Northeastern Fennoscandian Shield Since 1.9 Ga: Key Points: 40 39 • Since 1.9 Ga, the NE Fennoscandia Evidence From Ar/ Ar and Apatite Fission was characterized by a slow exhumation (1‐2 m/Myr) Track Data From the Kola Peninsula • Total denudation of the NE Roman V. Veselovskiy1,2 , Stuart N. Thomson3 , Andrey A. Arzamastsev4,5 , Fennoscandia since 1.9 Ga did not 6 7,8 7,8 9 exceed ~3‐5km Svetlana Botsyun , Aleksey V. Travin , Denis S. Yudin , Alexander V. Samsonov , • The Kola part of Fennoscandia and Alexandra V.
    [Show full text]
  • Seiches in the Semiclosed Seas of the Continental Shelf
    International Journal of Oceanography & Aquaculture MEDWIN PUBLISHERS ISSN: 2577-4050 Committed to Create Value for Researchers Seiches in the Semiclosed Seas of the Continental Shelf Inzhebeikin Yu I* Research Article Russian Academy of Sciences, Russia Volume 4 Issue 3 Received Date: September 18, 2020 *Corresponding author: Published Date: October 23, 2020 Center, Rostov-on-Don, Russia, Email: [email protected] Inzhebeikin Yu I, Russian Academy of Sciences, Southern Scientific DOI: 10.23880/ijoac-16000199 Abstract Seiche movements in two small areas of semi-closed seas on the Continental Shelf (the White Sea and the Sea of Azov) with very different morphometric characteristics are considered in this paper. In addition, tidal movements are highly developed in the White sea, while in the Azov sea tides are virtually absent. We’ve used morphometric characteristics of the seas, including the ones recently obtained by the Azov Sea, as well as methods of numerical hydrodynamic simulation based on the theory of shallow water, and spectral analysis of the observation data of the sea level fluctuations. Keywords: Continental Shelf; Semi-Closed Seas; White Sea; Sea Of Azov; Seiche; Numerical Hydrodynamic Simulation; Spectral Analysis; Flood Introduction located in the Northern and South-Western boundaries of the European part of Russia respectively (Figure 1). In August 2006, on the Dolzhanskaya spit of the Azov sea, the water level rose sharply, people and cars washed away in the sea, the spit broke in several places. At the same time there was no storm warning. In June 2010 on the Yeisk spit of the same sea of Azov at full calm across the sea suddenly appeared powerful current washed away children, wandering on the spit knee-deep in water.
    [Show full text]
  • UNESCO/IOC/HELCOM Baltic Floating University Mid-Cruise Workshop Training Through Practice and Research...; 4Th; the Baltic Floa
    Intergovernmental Oceanographic Commission technical series 53 The Baltic Floating University: Training Through Research in the Baltic, Barents and White Seas - 1997 Compiled by: N. Plink, A.V. Nekrasov, G.G. Gogoberidze Ye. Yu. Kliukov, S.V. Lukyanov and M.B. Shilin Edited by: Ray C. Griffiths UNESCO 1998 sc-9ahwa9 The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariats of UNESCO and IOC concerning the legal status of any country or territory, or its authorities, or concerning the delimitation of the frontiers of any country or territory. For bibliographic purposes, this document should be cited as follows: The Baltic Floating University: Training through Research In the Baltic, Barents and White Seas - 1997. IOC Technical Series No. 53, UNESCO 1998 (English) Printed in 1998 by the United Nations Educational, Scientific and Cultural Organization 7, place de Fontenoy, 75352 Paris 07 SP Printed in UNESCO’s Workshops 0 UNESCO 1998 Printed in France IOC Technical Series No. 53 Page iii TABLE OF CONTENTS Page ABSTRACT ACKNOWLEDGEMENTS INTRODUCTION 1 MAIN RESULTS OF THE BFU CRUISES IN THE BALTIC SEA AND THE GULF OF FINLAND 4 INVESTIGATIONS IN THE WESTERNPART OF THE MUHU STRAIT 22 Introduction 22 Main objectives 22 Description of the cruise 22 Results 24 Hydrography and meteorology 24 HydrobiologV and sea-bed characteristics 26 M4INRESEARCH RESULTS OF THE BFU-NORTH PROGRAMME 30 Results for Kandalaksha Gulf, in the White Sea 30 Results
    [Show full text]
  • The History of the Finnish Botanical Exploration of Russian Lapland in 1861 and 1863
    Memoranda Soc. Fauna Flora Fennica 94: 1–35. 2018 ISSN 0373-6873 (print) Helsinki 4 June 2018 ISSN 1796-9816 (online) The history of the Finnish botanical exploration of Russian Lapland in 1861 and 1863 Alexander N. Sennikov* & Mikhail N. Kozhin Sennikov, A. N., Botanical Museum, Finnish Museum of Natural History, P.O. Box 7, 00014 University of Helsinki, Finland; & Herbarium, Komarov Botanical Institute of Russian Academy of Sciences, Prof. Popov str. 2, 197376 St Petersburg, Russia. E-mail: alexander.sennikov@ helsinki.fi (*Author for correspondence) Kozhin, M. N., Department of geobotany, Biological faculty, Lomonosov Moscow State University, 119234, Leninskye Gory 1–12, GSP–1, Moscow, Russia; & Avrorin Polar-Alpine Botanical Garden and Institute of Kola Scientific Centre of Russian Academy of Sciences, 184250, Kirovsk, Murmansk Region, Russia. E-mail: [email protected] The early Finnish expeditions to the Kola Peninsula were organised by the Societas pro Fauna et Flora Fennica. The first expedition, in 1861, was made by two separate teams. Petter Adolf Karsten and Nils Isak Fellman headed to the western part, and Gustaf Selin studied the southwest- ern coast and then also proceeded to the western part; Karl Emil Inberg, an entomologist, collected insects separately along the track from Kandalaksha to Kola. The second expedition, in 1863, with participation of Fellman, Mårten Magnus Wilhelm Brenner and Nils Johan Laurin, studied the coasts of the White and Barents Seas around the whole Peninsula. The historical background of these expeditions and their circumstances are described in detail and discussed. Literature sources and herbarium specimens are traced in order to produce precise maps and gazetteers of the expe- ditions.
    [Show full text]
  • Molecular Phylogeny and Phylogeography of Potentilla Multifida L
    plants Article Molecular Phylogeny and Phylogeography of Potentilla multifida L. agg. (Rosaceae) in Northern Eurasia with Special Focus on Two Rare and Critically Endangered Endemic Species, P. volgarica and P. eversmanniana Ivan A. Schanzer 1,* , Alina V. Fedorova 1, Olga V. Shelepova 1 and Guzyaliya F. Suleymanova 2,3 1 Tsitsin Main Botanical Garden of Russian Academy of Sciences, Botanicheskaya Str., 4, 127276 Moscow, Russia; [email protected] (A.V.F.); [email protected] (O.V.S.) 2 Khvalynsky National Park, Oktyabrskaya Str., 2B, 412787 Khvalynsk, Russia; [email protected] 3 Saratov State University, Astrakhanskaya Str., 83, 410012 Saratov, Russia * Correspondence: [email protected]; Tel.: +7-915-362-1911 Received: 5 November 2020; Accepted: 17 December 2020; Published: 18 December 2020 Abstract: The results of a molecular genetic study of Potentilla multifida agg. using two plastid markers (ndhC-trnV and psbA-trnH) and a nuclear ITS marker suggested that this group comprises a number of relatively young and incompletely differentiated species widely distributed in Northern Eurasia. The sequences were analyzed using tree-based (maximum likelihood) and network-based (statistical parsimony network) approaches. The plastid data suggested incomplete lineage sorting, characteristic of the group as a whole. The nuclear ITS results demonstrated quite a different pattern, with mostly conspecific accessions shaping monophyletic clades. The majority of the Potentilla sect. Multifidae species studied possess few, usually closely related plastid haplotypes, or are even monomorphic. In contrast, P. volgarica, a narrow endemic from the Volga River valley, presents plastid haplotypes belonging to two distantly related groups. Such a pattern of genetic diversity in P.
    [Show full text]
  • Updated Data on the Current Seismicity of the White Sea and the Karelian Region During the Period 2005–2016
    Arctic Environmental Research 19(1): 11–19 UDC 550.34.06 DOI 10.3897/issn2541-8416.2019.19.1.11 Research Article Updated data on the current seismicity of the White Sea and the Karelian region during the period 2005–2016 YaV Konechnaya1,2, AN Morozov1,3, NV Vaganova2, IA Zueva4 1 Geophysical Survey of Russian Academy of Sciences (Arkhangelsk, Russian Federation) 2 N. Laverov Federal Center for Integrated Arctic Research of Russian Academy of Sciences (Arkhangelsk, Russian Federation) 3 N. Laverov Federal Center for Integrated Arctic Research of Russian Academy of Sciences (Obninsk, Russian Federation) 4 Institute of Geology Karelian Research Center of Russian Academy of Sciences (Petrozavodsk, Russian Federation) Corresponding author: Yana Konechnaya ([email protected]) Academic editor: Aleksandr I. Malov ♦ Received 7 February 2019 ♦ Accepted 15 February 2019 ♦ Published 8 March 2019 Citation: Konechnaya YaV, Morozov AN, Vaganova NV, Zueva IA (2019) Updated data on the current seismicity of the White Sea and the Karelian region during the period 2005–2016. Arctic Environmental Research 19(1): 11–19. https://doi.org/10.3897/issn2541- 8416.2019.19.1.11 Abstract This article is the result of previous studies to clarify the seismicity of the White sea, supplemented by similar studies on the continental part of the Republic of Karelia. The relocated catalog of earthquakes was created for the period from 2005 to 2016 for White Sea and the Karelian region. With the help of proven methods, the parameters of the epicenters of identified earthquakes were relocated and a map of current seismicity was obtained. The parameters of the epicenters were specified using BARENTS travel-time model, a single meth- odological approach (using Generalized beamforming) and all currently available source data and bulletins of Russian and foreign seismic stations.
    [Show full text]
  • C:\Documents and Settings\Alan Smithee\My Documents\MOTM
    L`x1/0/Lhmdq`knesgdLnmsg9Rs`tqnkhsd For this month’s mineral, we are pleased to feature dark, reddish-brown, twinned staurolite crystals in a white schist matrix from northern Russia’s Kola Peninsula. Our write-up explains the high-grade, metamorphic origin and the rich lore of twinned staurolite crystals, while providing insight into one of Russia’s most mineralogically fascinating regions. OVERVIEW PHYSICAL PROPERTIES Chemistry: (Fe,Mg,Zn)3-4(Al,Fe)18(Si,Al)8O48H2-4 Basic Iron Magnesium Zinc Oxyaluminosilicate (Iron Magnesium Zinc Aluminum Oxysilicate Hydroxide), often containing titanium, chromium, manganese, and lithium. Class: Silicates Subclass: Nesosilicates Group: Staurolite Crystal System: Monoclinic Crystal Habits: Single or twinned crystals: single crystals are prismatic with six- sided, pseudohexagonal cross sections; twinned crystals common as Figure 1. Staurolite with nearly 90° twinned crystals, penetration intergrowths of two individual crystals at angles of nearly 60 plus untwinned single crystal. degrees or nearly 90 degrees. Color: Yellowish-brown, reddish-brown, and brownish-black; rarely bluish; weathers to gray. Luster: Vitreous to dull Transparency: Usually translucent to opaque; rarely transparent. Streak: White to grayish-white Refractive Index: 1.736-1.762 Cleavage: Distinct in one direction Fracture: Uneven to subconchoidal, brittle Hardness: 7.0-7.5 Specific Gravity: 3.7-3.8 Luminescence: None Distinctive Features and Tests: Best field marks are color; occurrence in metamorphic environments; and frequent, distinctive “crossed” twinning. Dana Classification Number: 52.2.3.1.1 NAME Pronounced STORE-uh-lite, the name stems from the late Greek word stauros, “cross,” and lithos, “stone,” literally “stone cross.” Interestingly, the Greek word stauros as used in the classical Greek of epic poems like the Iliad and the Odyssey, meant “upright stake” or “pale.” When stauros came to mean “cross” is debated be scholars.
    [Show full text]
  • KAROL PIASECKI Szczecin the WHITE SEA POMORYE and ITS
    Studia Maritima, vol. XXII (2009) ISSN 0137-3587 KAROL PIASECKI Szczecin THE WHITE SEA POMORYE AND ITS INHABITANTS 1. The White Sea Pomorye owes its name to a group of Slavic settlers1 living mainly on the so-called Pomor Coast, i.e. a fragment of the White Sea coast be- tween the River Kem and Onega (Fig. 1). The present name of the White Sea became widespread at the beginning of the 17th century. Before that, the Slavic inhabitants of its coasts used a name Студеное Море, which means the Cold Sea, whereas on western maps, since the times of the reissue in 1568 of Claudius Ptole- my’s Geography, it appeared as Sinus Grandvicus (Granvicus, Grandvich). The name was taken from Norwegian sailors, for whom initially it probably meant the Western end of the Murmansk Coast.2 1 The term Pomors appeared for the first time in written sources in 1526, when: Поморцы с моря Океана из Кондолакской гyбы лросили вмесmе с лоплянамва yсmройства церкви. It functions quite commonly in the 16th century, both as a name of the inhabitants of the Pomor Coast, as well in the function of a proper name – I. Ul’janov: Strana Pomorja, 1984. From the second half of the 17th century, mainly because of Vasiliy Tatishchev, the author of the monumental Russian History, Pomorye was understood in three meanings: as 1) a territory of the White Sea coast from the Onega to the Kem, 2) the territory of the whole White Sea Coast, 3) the territory of the whole Russian North, including the provinces of Archangelsk, Vologda and Olonets.
    [Show full text]
  • Arzamastsev, Arzamastseva, 1993)
    Proceedings of the MSTU, Vol. 15, No. 2, 2012 pp.277-299 UDC 550.42 Alkaline volcanism in the Kola Peninsula, Russia: Paleozoic Khibiny, Lovozero and Kontozero calderas A.A. Arzamastsev, M.N. Petrovsky Geological Institute, KSC RAS, Apatity Abstract. This paper presents the results of studying the Paleozoic volcanic series of the Kola Province, wide- spread in the areas of the Lovozero and Khibina massifs, the Kontozero caldera, and the Ivanovka volcano- plutonic complex. A distinctive feature of the volcanics is the presence of moderately alkaline basanites along with silica-undersaturated alkaline rock associations. All of the rocks are significantly enriched in incompatible elements: the contents of Rb, Ba, Sr, Nb, Zr and Y in the volcanics of the Lovozero and Kontozero formations. The Sm-Nd and Rb-Sr data suggest that the volcanics of the study area were derived from two different mantle sources: (1) superdepleted mantle material resulted from the multistage crustal growth over Archaean and Proterozoic time in the Kola-White Sea rift-collision zone and (2) a source that had properties of moderately enriched EMI-type mantle. It has been shown that the emplacement of the volcanics preceded the main pulse of alkaline magmatism in the region and can be referred to as the initial phase of the Paleozoic tectono-magmatic reactivation. According to geochronological data, the alkaline volcanic rocks were emplaced at least 20-30 m.y. before the intrusion of the alkaline plutonic rocks. Аннотация. Представлены результаты изучения палеозойских вулканических серий Кольской провинции, распространенных в районах Ловозера, Хибин, Контозера и Ивановского вулкано- плутонического комплекса.
    [Show full text]
  • Kola Peninsula S2 Map Eng
    LEGEND The international Barents Protected Area Network Federal protected areas Vaydagubsky lighthouse Nemetsky cape BARENTS SEA (BPAN) project brings together nature conservation authorities, scientific institutes and nature Regional protected areas Kandalaksha nature reserve conservation NGOs in Finland, Sweden, Norway and Northwest Russia. It is an initiative of the nature Planned federal protected areas conservation group of the Barents Euro-Arctic Council. At the moment it is a key nature conservation project in Planned regional protected areas the Barents Region – one of the largest remaining areas 72 1 of untouched natural ecosystems on Earth. Local nature monuments Check-point «Borisoglebsky» Motovsky Gulf The guiding principle of the BPAN project is “Nature has no borders”. Its main aim is to create a Pechenga representative network of protected areas in the Nature monuments NORWAY Pikshchuyev lighthouse Е-105 Barents Region in order to preserve vulnerable Botanical (forest) northern nature irrespective of state or administrative Zapolyarny borders. The basis for such transboundary cooperation NIKEL Botanical (species protection) 50 17 Kildin lies in the concept of Econet. It combines protected Western areas of different status, which guarantees the Geological 60 Кildinsky lighthouse 61 sustainability of protected areas and the functioning of itovka Pasvik T 18 Teribersky lighthouse ecosystems, better than isolated protected areas. nature reserve Pechenga Hydrological Kandalaksha Zapadnaya11 Litsa Sayda-Guba nature reserve Natural
    [Show full text]
  • C:\Documents and Settings\Alan Smithee\My Documents\MOTM
    @oqhk1/01Lhmdq`knesgdLnmsg9@rsqnogxkkhsd The month we are shining the spotlight on astrophyllite, a rare, complex silicate from one of the world’s most remarkable mineralogical provinces—the Kola Peninsula of northern Russia. Read on to learn about astrophyllite’s unusual colors, luster, and attractive starburst patterns, as well as the preparation that goes into our write-ups. OVERVIEW PHYSICAL PROPERTIES Chemistry: (K,Na)3(Fe,Mn)7Ti2Si8O24(O,OH)7 Basic Potassium Sodium Iron Manganese Titanium Oxysilicate, often containing small amounts of fluorine, calcium, magnesium, aluminum, niobium, and zirconium. Class: Silicates Subclass: Single-chain Inosilicates Group: Astrophyllite Crystal System: Triclinic Crystal Habits: Usually as small, thin, tabular or bladed crystals grouped in radiating, starburst-shaped aggregates; also disseminated, lamellar, and massive. Color: Usually golden-yellow, bronze-yellow, yellowish-brown, or amber; less frequently brown, greenish- brown, or reddish-brown. Colors can be patchy or zoned. Crystals are often pleochroic, exhibiting shifts in color with changes in viewing angle. Luster: Sub-metallic, pearly on cleavage surfaces Transparency: Usually translucent to opaque; thin crystals may be transparent. Streak: Golden to yellowish-brown Cleavage: Perfect in one direction Fracture: Uneven; brittle. Hardness: 3.0-3.5 Specific Gravity: 3.3-3.4 Luminescence: None Refractive Index: 1.680-1.700 Distinctive Features and Tests: Best field marks are yellow-to-brownish colors, color zoning, and pleochroism; perfect cleavage in one direction; brittleness; radiating, starburst-shaped crystal aggregates; sub-metallic luster; and occurrence in syenite and nepheline-syenite fissures and pegmatites. Can be confused with augite, which is harder and forms shorter prisms; and schorl, which is harder and forms hexagonal crystals.
    [Show full text]