Riparo Arma Di Nasino Series
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Relazione Della Descrizione Fondativa DF.0
DF.0 Relazione della Descrizione Fondativa Dicembre 2016 Comune di Ortovero (SV) DESCRIZIONE FONDATIVA Indice del documento 1. Inquadramento territoriale pag. 1 2. Processi socio-economici in atto e reti di relazione pag. 4 2.1 Le dinamiche demografiche pag. 4 2.2 Gli indicatori di accessibilità pag. 5 2.3 Il sistema economico locale pag. 10 2.4 La S.A.U. e le aziende agricole attive pag. 12 2.5 Il patrimonio abitativo pag. 14 2.6 Gli scenari demografici al 2030 pag. 19 3. I riferimento per il sistema storico-culturale pag. 25 3.1 Il sistema insediativo albenganese pag. 25 3.2 L’evoluzione storica del territorio di Ortovero pag. 27 3.3 Centri storici pag 30 3.4 Le emergenze storico-architettoniche pag. 31 3.5 Il paesaggio agrario storico: i terrazzamenti pag. 37 4. I caratteri fisici e paesistici del territorio pag. 41 4.1 Aspetti geologici, geomorfologici ed idraulici pag 41 4.1 Gli aspetti vegetazionali pag. 41 4.2 L’uso del suolo pag. 47 4.3 La rete ecologica pag. 48 5. Il quadro ambientale e le criticità emerse pag. 55 5.1 Aria pag. 55 5.2 Acqua pag. 57 5.3 Suolo e sottosuolo pag. 65 5.4 Vegetazione e biodiversità pag. 68 5.5 Inquinanti fisici pag. 70 5.6 Rifiuti solidi urbani pag. 72 6. Il sistema insediativo e dei servizi pag. 79 6.1 Ortovero pag. 79 6.2 Pogli pag. 82 6.3 Campi pag. 83 7. Lo stato della pianificazione pag. 85 7.1 Il Piano Territoriale di Coordinamento Paesistico (PTCP) pag. -
A Critical Review of “The Mesolithic” in Relation to Siberian Archaeology ALEXANDER B
ARCTIC VOL. 38, NO. 3 (SEPTEMBER 1985) P. 178-187 A Critical Review of “the Mesolithic” in Relation to Siberian Archaeology ALEXANDER B. DOLITSKY’ ABSTRACT. This paperexplores the potentialof the economic-ecqlogical method basedon the exploitation of fishresources for Mesolithic site iden- tification, as compared to the recently popular yet indecisive technological-typologicalmethod, to predict the existence of “Mesolithic-like” sub- sistence activities in Siberia during the Sartan-Holocene“transition” period. The article is an attempt toestablish, or at least topropose, new criteria that can lead toa higher level of understandingof Mesolithic economies insubarctic and arctic regions. Also, decision-making processes that operate to achieve behavioralgoals based on efficiency of human beingsare suggested. The model, designed with respectto geographical regions identified as interbiotic zones, has the advantage of offering specific alternative hypotheses enabling the definition of both environmental properties and predicted human behavior. Key words: Mesolithic, Siberia, interbiotic zone RÉSUMÉ. L’article &die le potentiel de la méthode économique-écologique fondte sur l’exploitation de poissons en guise de ressources pour l’identification desites mtsolithiques, en comparison avecla mdthode technologique-typologique populaire maisindécise, afin de prddire l’existence d’activitds de subsistencede genre mésolithique en Sibdrie durant la périodede transition Sartan-Holoctne. On tente d’établir ou au moins de pro- poser de nouveaux crittres qui pourraient permettre une meilleure comprdhension des économies mdsolithiques dans les rdgions arctiques et sub- arctiques. De plus, on suggkre des processus de prise de ddcisions qui visent21 établir des buts de comportement fondéssur l’efficacité de I’être hu- main.Conçu par rapport 21 des rdgionsgéographiques nommées zones interbiotiques, le modele a l’avantage d’offrir des choix particuliers d’hypothtses permettant la ddfinition des propridtés environnementales et du comportement humain prévu. -
Hunters and Farmers in the North – the Transformation of Pottery Traditions
Hunters and farmers in the North – the transformation of pottery traditions and distribution patterns of key artefacts during the Mesolithic and Neolithic transition in southern Scandinavia Lasse Sørensen Abstract There are two distinct ceramic traditions in the Mesolithic (pointed based vessels) and Neolithic (flat based vessels) of southern Scandinavia. Comparisons between the two ceramic traditions document differences in manufacturing techniques, cooking traditions and usage in rituals. The pointed based vessels belong to a hunter-gatherer pottery tradition, which arrived in the Ertebølle culture around 4800 calBC and disappears around 4000 calBC. The flat based vessels are known as Funnel Beakers and belong to the Tragtbæger (TRB) culture, appearing around 4000 calBC together with a new material culture, depositional practices and agrarian subsistence. Pioneering farmers brought these new trends through a leap- frog migration associated with the Michelsberg culture in Central Europe. These arriving farmers interacted with the indigenous population in southern Scandinavia, resulting in a swift transition. Regional boundaries observed in material culture disappeared at the end of the Ertebølle, followed by uniformity during the earliest stages of the Early Neolithic. The same boundaries reappeared again during the later stages of the Early Neolithic, thus supporting the indigenous population’s important role in the neolithisation process. Zusammenfassung Keywords: Southern Scandinavia, Neolithisation, Late Ertebølle Culture, Early -
8. Flint Cobe Axe Found on Fair Isle, Shetland
8. FLINT COBE AXE FOUND ON FAIR ISLE, SHETLAND. The purpose of this note is to put on record the discovery of what seems to b Mesolithiea c flin Fain to corre Isleeax , Shetland discovere Th . mads ywa e in June 1945 while the writer, accompanied by Sub-Lieutenant Appleby, R.N., then in charge of the naval station on the island, was searching for skua chicks. NOTES. 147 The s embeddeflinwa t d with other pebble patca n si f bar ho e ground from which the peat had been eroded. The site was the summit of a knoll on the edge plateae oth f u wher Greae eth t Skua nests aboud yard0 an , 80 t s west-north-west of the naval huts at North Haven. I estimated the height above sea-level as about 300 feet. It is a matter of regret that I did not think of preserving any of the peaty soil in which the flint was embedded on the chance that it might have contained the pollen that would have helped to locate the object in terms of the North European climatic sequence. When this was pointed out to me by Professor Childen touci t n effors mada hge , wa wito tt e h Sub-Lieutenant Applebo t y procure some of the soil, but he was no longer on the island, and no other opportunity has arisen of revisiting the island. objece e ende flina th Th f s Th i sto t cor. measurine 4-y b 5eax cm . cm 2 g1 t notablno flins beee ar ha yt n t shari give t pbu n sharp edgesedgee e Th ar s. -
Respiratory Adaptation to Climate in Modern Humans and Upper Palaeolithic Individuals from Sungir and Mladeč Ekaterina Stansfeld1*, Philipp Mitteroecker1, Sergey Y
www.nature.com/scientificreports OPEN Respiratory adaptation to climate in modern humans and Upper Palaeolithic individuals from Sungir and Mladeč Ekaterina Stansfeld1*, Philipp Mitteroecker1, Sergey Y. Vasilyev2, Sergey Vasilyev3 & Lauren N. Butaric4 As our human ancestors migrated into Eurasia, they faced a considerably harsher climate, but the extent to which human cranial morphology has adapted to this climate is still debated. In particular, it remains unclear when such facial adaptations arose in human populations. Here, we explore climate-associated features of face shape in a worldwide modern human sample using 3D geometric morphometrics and a novel application of reduced rank regression. Based on these data, we assess climate adaptations in two crucial Upper Palaeolithic human fossils, Sungir and Mladeč, associated with a boreal-to-temperate climate. We found several aspects of facial shape, especially the relative dimensions of the external nose, internal nose and maxillary sinuses, that are strongly associated with temperature and humidity, even after accounting for autocorrelation due to geographical proximity of populations. For these features, both fossils revealed adaptations to a dry environment, with Sungir being strongly associated with cold temperatures and Mladeč with warm-to-hot temperatures. These results suggest relatively quick adaptative rates of facial morphology in Upper Palaeolithic Europe. Te presence and the nature of climate adaptation in modern humans is a highly debated question, and not much is known about the speed with which these adaptations emerge. Previous studies demonstrated that the facial morphology of recent modern human groups has likely been infuenced by adaptation to cold and dry climates1–9. Although the age and rate of such adaptations have not been assessed, several lines of evidence indicate that early modern humans faced variable and sometimes harsh environments of the Marine Isotope Stage 3 (MIS3) as they settled in Europe 40,000 years BC 10. -
Cover SD Tagungen4 Gronen
Sonderdruck aus / Offprint from Die Neolithisierung Mitteleuropas The Spread of the Neolithic to Central Europe Die Tagung wurde gefördert durch: RGZM – TAGUNGEN Band 4 ISBN 978-3-88467-159-7 ISNN 1862-4812 © 2010 Verlag des Römisch-Germanischen Zentralmuseums Mainz € 78,– Bestellungen / orders: shop.rgzm.de [email protected] Satz: Andrea Fleckenstein, Frankfurt; Claudia Nickel (RGZM) Gesamtredaktion: Stefanie Wefers (RGZM) Endredaktion: Stefanie Wefers, Claudia Nickel (RGZM) Umschlagbild: Michael Ober (RGZM) Bibliografische Information der Deutschen Nationalbibliothek Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.d-nb.de abrufbar. Das Werk ist urheberrechtlich geschützt. Die dadurch begründe- ten Rechte, insbesondere die der Übersetzung, des Nachdrucks, der Entnahme von Abbildungen, der Funk- und Fernsehsendung, der Wiedergabe auf fotomechanischem (Fotokopie, Mikrokopie) oder ähnlichem Wege und der Speicherung in Datenverarbei- tungsanlagen, Ton- und Bildträgern bleiben, auch bei nur aus- zugsweiser Verwertung, vorbehalten. Die Vergütungsansprüche des §54, Abs. 2, UrhG. werden durch die Verwertungsgesell- schaft Wort wahrgenommen. Herstellung: Druck- und Verlagsservice Volz, Budenheim Printed in Germany Römisch-Germanisches Zentralmuseum Forschungsinstitut für Vor- und Frühgeschichte Detlef Gronenborn · Jörg Petrasch (Hrsg.) DIE NEOLITHISIERUNG MITTELEUROPAS Internationale Tagung, Mainz 24. bis 26. Juni 2005 THE SPREAD -
Pleistocene - the Ice Ages
Pleistocene - the Ice Ages Sleeping Bear Dunes National Lakeshore Pleistocene - the Ice Ages • Stage is now set to understand the nature of flora and vegetation of North America and Great Lakes • Pliocene (end of Tertiary) - most genera had already originated (in palynofloras) • Flora was in place • Vegetation units (biomes) already derived Pleistocene - the Ice Ages • In the Pleistocene, earth experienced intensification towards climatic cooling • Culminated with a series of glacial- interglacial cycles • North American flora and vegetation profoundly influenced by these “ice-age” events Pleistocene - the Ice Ages What happened in the Pleistocene? 18K ya • Holocene (Recent) - the present interglacial started ~10,000 ya • Wisconsin - the last glacial (Würm in Europe) occurred between 115,000 ya - 10,000 ya • Height of Wisconsin glacial activity (most intense) was 18,000 ya - most intense towards the end of the glacial period Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal plains become extensive • continental islands disappeared and land bridges exposed 100 m line Beringia Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal plains become extensive • continental islands disappeared and land bridges exposed Malaysia to Asia & New Guinea and New Caledonia to Australia Present Level 100 m Level Pleistocene - the Ice Ages What happened in the Pleistocene? • up to 100 meter drop in sea level worldwide • coastal -
Ae Circondario Savona
N.B. IL CALENDARIO E’ STATO REDATTO IN BASE ALLE COMUNICAZIONI RICEVUTE DA PARTE DEGLI UFFICI NEL PERIODO 01/05/2016 AL 15/07/2016 TRIBUNALE DI SAVONA 17100 Savona - C.so XX Settembre - Tel. 019/83.161 - Fax Segreteria Presidenza 019/821371 civile 8316417 - penale 8316316 [email protected] COMPETENZE TERRITORIALI: Alassio, Albenga, Albisola Superiore, Albissola Marina, Altare, Andora, Arnasco, Balestrino, Bardineto, Bergeggi, Boissano, Borghetto, Santo Spirito, Borgio Verezzi, Bormida, Cairo Montenotte, Calice Ligure, Calizzano, Carcare, Casanova Lerrone, Castelbianco, Castelvecchio di Rocca Barbena, Celle Ligure, Cengio, Ceriale, Cisano sul Neva, Cosseria, Dego, Erli, Finale Ligure, Garlenda, Giustenice, Giusvalla, Laigueglia, Loano, Magliolo, Mallare, Massimino, Millesimo, Mioglia, Murialdo, Nasino, Noli, Onzo, Orco Feglino, Ortovero, Osiglia, Pallare, Piana Crixia, Pietra Ligure, Plodio, Pontinvrea, Quiliano, Rialto, Roccavignale, Sassello, Savona, Spotorno, Stella, Stellanello, Testico, Toirano, Tovo San Giacomo, Urbe, Vado Ligure, Varazze, Vendone, Vezzi Portio, Villanova d'Albenga, Zuccarello. PRESIDENTE (1) SOAVE dr. Giovanni PRESIDENTI DI SEZIONE (2) 1. FIUMANO’ dr.ssa Caterina 2. CANAPARO dr.ssa Lorena GIUDICI (19) 1. ZERILLI dr. Giovanni 2. GIORGI dr.ssa Fiorenza 3. MELONI dr. Francesco 4. PRINCIOTTA dr. Alberto 5. FOIS dr. Enrico 6. ACQUARONE dr.Luigi 7. CANEPA dr. Marco 8. TABACCHI dr.ssa Cristina 9. DE DOMINICIS dr.ssa Laura 10. PISATURO dr. Filippo 11. ATZENI dr. Davide 12. MORELLO dr.ssa Maria Laura 13. GIANNONE dr. Francesco 14. PELOSI dr. Fabrizio 15. POGGIO dr. Stefano 16. CINGANO dr.ssa Valentina 17. MELE dr.ssa Daniela 2 N.N. 0 GIUDICE SEZIONE LAVORO (1) COCCOLI dr.ssa Alessandra. GIUDICI ONORARI DI TRIBUNALE (12) 1. -
New Studies of the Upper Paleolithic Site Byki-7 on the Seim River
New studies of the Upper Paleolithic site Byki-7 on the Seim River Group of the Upper Paleolithic sites of Byki are situated on the left bank of Seim River (Desna river basin) 470 km SSW from Moscow and 50 km to the East from Kursk (Grigorieva & Filippov 1978; Chubur 2001; Akhmetgaleeva 2015). The main typological feature of Peny, Byki 1, 2, 3 and 7 (layers Ia & I) sites’ flint assemblages is the presence of geometric microliths, mainly triangles with oblique truncation of one edge and a straight truncated base. Complexes belong to the Late Upper Paleolithic with rich archaeological and faunal context. The close similarity of the sites’ points assemblage let us say about their archaeological unity. The lower cultural layers suspected as the remains of winter time settlements. We did not find yet any really archaeologically comparable materials for the Byki site’s data outside this micro region. Fig. 1. Spatial distribution of different cultural layers and dwellings on the Byki-7 site. 1 - boundaries of the cultural layer Ia; 2 - boundaries of the cultural layer I: 1, 2 –numbering of Layer I dwellings; 3 - boundaries of the cultural layer II; 4 - areas of maximum saturation of the cultural layer Ia; 5 - boundaries of permafrost deformations of II generation; 6 - boundaries of permafrost deformations of I generation; 7 - the location of cultural layer Ib. The analysis of Byki fauna materials has definitely showed the presence of a boreal sub-complex of so-called Late Last Glacial mammoth faunal complex (Akhmetgaleeva & Burova 2008). Basic hunting animals for human inhabitants of Byki sites were hare, arctic fox, reindeer and horse (Equus ferus). -
A Reexamination of Late-Pleistocene Boreal Forest Reconstructions for the Southern High Plains
QUATERNARY RESEARCH 28,238-244 (1987) A Reexamination of Late-Pleistocene Boreal Forest Reconstructions for the Southern High Plains VANCE T. HOLLIDAY Department of Geography, Science Hall, University of Wisconsin, Madison, Wisconsin 53706 Received March 9, 1987 Previous paleoecological research on the Southern High Plains resulted in development of a late Quatemary chronology of “pollen-analytical episodes” and the proposal that boreal forest existed in the region in the late Pleistocene. These interpretations are now considered untenable because (1) a number of the radiocarbon ages are questionable, (2) there are serious problems of differential pollen preservation and reproducibility of the pollen data, (3) there is an absence of supporting geological or paleontological data, and (4) the soils of the area contain none of the distinctive pedologicd characteristics produced by a boreal forest. Available data suggest that the region was primarily an open grassland or grassland with some nonconiferous trees through most of the Qua- ternary. 0 1987 University of Washington. INTRODUCTION leoecological data were collected and most of the interpretations made. This paper is a In the late 1950s and early 1960s consid- critical reexamination of the chronology of erable research was conducted into the late the proposed pollen-analytical episodes Quaternary, principally late Pleistocene, and the interpretations of boreal forest for paleoecology of the Southern High Plains the region, made in light of recent advances of northwestern Texas and eastern New in palynology and radiocarbon dating and Mexico (Wendorf, 1961a; Wendorf and better understanding of the late Quaternary Hester, 1975a). One of the most significant geology, soils, and paleontology of the discoveries made, b,ased on considerable Southern High Plains and following on pollen data, was the high content of pine some points raised by Holliday er al. -
L'entroterra Tra Borgio Verezzi E Andora
L’ALTRA RIVIERA l’entroterra tra Borgio Verezzi e Andora L’ALTRA RIVIERA L’entroterra tra Borgio Verezzi e Andora “Là nella stretta fascia di un monte più alto dell’orizzon- te vedrò sotto il mio mare, il mio corpo sarà sale, sarà il bianco di una vela e il giallo di una ginestra”. Passeg- giando per i viottoli acciottolati dei borghi che abbrac- ciano le valli tra Andora e Borgio Verezzi, sbirciando fra le loro case in pietra chiara affacciate sul mare, tornano alla mente le parole di quella magnifica canzone di Joan Manuel Serrat e Gino Paoli che è “Mediterraneo”. Giù in basso le vele bianche immerse nel blu del mare, sulla collina il giallo delle ginestre e la fragranza della lecceta, sui vecchi muri i fiori delicatamente azzurri della cam- panula a foglie uguali (l’endemica Campanula isophylla tanto celebre fra i botanici), i faggi secolari sui crinali dei monti … poi vigne, uliveti, panorami … in sintesi, l’altra Riviera. 1 L’oRo VERdE dELLE nosTRE valli 2 3 AssApoRARE IL gusTo dEL soLE 4 5 I coLoRI dELLA natuRA 6 7 Il Festival Teatrale piazzette, qualche antico tempo in cui il 22 luglio, VEREZZI di Borgio Verezzi lavatoio, la chiesa di San giorno di Santa Maria L’evento culturale di Martino con l’antico Maddalena, le famiglie Un borgo amato dai poeti maggior richiamo per campanile romanico… e di Verezzi cucinavano Verezzi è il Festival persino un mulino detto le lumache; questa “...Meglio che dalla strada, Verezzi si passeggia dai tetti; Teatrale che si tiene ogni “fenicio” per la tecnica tradizione continua che non sono tetti, ma terrazzini cotti e ingobbiti dal sole: estate nella suggestiva costruttiva. -
European Red List of Habitats
European Red List of Habitats Part 2. Terrestrial and freshwater habitats Environment More information on the European Union is available on the internet (http://europa.eu). Luxembourg: Publications Office of the European Union, 2016 ISBN 978-92-79-61588-7 doi: 10.2779/091372 © European Union, 2016 Reproduction is authorised provided the source is acknowledged. The photos are copyrighted and cannot be used without prior approval from the photographers. Printed in England Printed on recycled paper that has been awarded the EU eco-label for graphic paper (http://ec.europa.eu/environment/ecolabel/) Cover: Active volcano, Iceland. © Wim Ozinga. Insets: Freshwater lake, Finland. © Heikki Toivonen. Larix forest, Mercantour, France. © Benoît Renaux. Soft coastal cliff, Latvia. © John Janssen. Machair grassland, Ireland. © Joop Schaminée. Calcareous quaking mire, Finland. © Teemu Tahvanainen. Spring mire, Dolomites, Italy. © Michal Hájek. European Red List of Habitats Part 2. Terrestrial and freshwater habitats Authors J.A.M. Janssen, J.S. Rodwell, M. García Criado, S. Gubbay, T. Haynes, A. Nieto, N. Sanders, F. Landucci, J. Loidi, A. Ssymank, T. Tahvanainen, M. Valderrabano, A. Acosta, M. Aronsson, G. Arts, F. Attorre, E. Bergmeier, R.-J. Bijlsma, F. Bioret, C. Biţă-Nicolae, I. Biurrun, M. Calix, J. Capelo, A. Čarni, M. Chytrý, J. Dengler, P. Dimopoulos, F. Essl, H. Gardfjell, D. Gigante, G. Giusso del Galdo, M. Hájek, F. Jansen, J. Jansen, J. Kapfer, A. Mickolajczak, J.A. Molina, Z. Molnár, D. Paternoster, A. Piernik, B. Poulin, B. Renaux, J.H.J. Schaminée, K. Šumberová, H. Toivonen, T. Tonteri, I. Tsiripidis, R. Tzonev and M. Valachovič With contributions from P.A.