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Wyszukujesz frazę "geoarchaeology" wg kryterium: Temat


Tytuł:
Archaeological distribution of geoheritage for geotourism development in Nakhon sawan province, Thailand
Autorzy:
Singtuen, Vimoltip
Phajuy, Burapha
Powiązania:
https://bibliotekanauki.pl/articles/1050907.pdf
Data publikacji:
2020-09-30
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
geosite
geoarchaeology
geodiversity
geoheritage
SWOT analysis
Opis:
Nakhon Sawan Province is located in Upper Central Thailand, where the Chao Phraya River, the vital river of Thailand, begins. According to the distribution of the archaeological sites, the related geological features were divided into two groups by geodiversity scope: (1) hydrological sites - Chao Phraya river, Bueng Boraphet lake, (2) speleological sites - Tham Phet-Tham Thong cave and Khoa Nor mountain. The hydrological sites are the primary water resources of local people since many hundred years, including transportation, agriculture, and fishery, so there are many archaeological sites around there. In addition, the speleological sites are covered with limestones intruded by the granitic rocks, which has caused ore deposition in the form of skarn. The evidence of antiquities in the archaeological site near speleological sites suggests that ancient people discovered and produced their ores, notably iron in the studied area. Based on inventory, characterization, classification, and assessment methods, this preliminary geoarchaeology study can support Nakhon Sawan to promote geotourism for sustainability by their stunning geological features, fantastic nature as well as beautiful culture, both past and present.
Źródło:
Quaestiones Geographicae; 2020, 39, 3; 57-68
0137-477X
2081-6383
Pojawia się w:
Quaestiones Geographicae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
An importance of neolithic-early dynastic-the end of old kingdom transition in ancient Egypt : geological evidences of climatic oscillations – future project
Autorzy:
Pawlikowski, M.
Szymanowicz, M.
Powiązania:
https://bibliotekanauki.pl/articles/343857.pdf
Data publikacji:
2013
Wydawca:
nakł. Maciej Pawlikowski
Tematy:
Nile Delta
climatic oscillations
geoarchaeology
interdisciplinary research
Opis:
Field as well as archaeological, mineralogical and geochemical investigation of Nile Delta settlement and sediments will be performed, during the future project presented in this paper. Presented project will explain the impact of climatic changes on Neolithic-Early Dynastic-the end of Old Kingdom transition in the history of ancient Egypt.
Źródło:
Auxiliary Sciences in Archaeology, Preservation of Relics and Environmental Engineering; 2013, 16; 1-6
1689-6742
Pojawia się w:
Auxiliary Sciences in Archaeology, Preservation of Relics and Environmental Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The role of neo-tectonics in the variation of the relative mean sea level throughout the last 6000 years on the Taman Peninsula (Black Sea, Azov Sea, Russia)
Autorzy:
Fouache, E.
Porotov, A.
Müller, C.
Gorlov, Y.
Powiązania:
https://bibliotekanauki.pl/articles/1187360.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
sea level
geoarchaeology
neotectonics
Holocene
Black Sea
Russia
Opis:
Sediments, carbon-datings on seashells, allow us to reconstruct the evolution of the average sea level for some 6000 years on the Taman Peninsula. The current sea level, regionally, appears to be the highest level ever reached on the peninsula. It seems that for the Anapa area and Tchouchtchka Spit area it is possible to propose a sea level curve characterised by a slow, continuous rising during the past 6000 years. On the Taman Peninsula itself, the sedimentary record of this slow ascent has been distorted by a heavy tectonic subsidence. We have identified this neo-tectonic subsidence effect on at least two areas on the peninsula. The south of the peninsula, Burgaz Spit and Vityazevos Lagoon, is the most affected area. The Taman Gulf is an intermediate area. The tectonic subsidence is particularly noticeable from 1500 to 500 BC, which we believe to have been misinterpreted until now, and to be at the origin of the notion of "Phanagorian Regression".
Źródło:
Polish Geological Institute Special Papers; 2004, 11; 47-57
1507-9791
Pojawia się w:
Polish Geological Institute Special Papers
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Niektóre zjawiska geologiczne w stanowiskach archeologicznych na przykładzie stanowiska w Dzierżysławiu : komunikat
Some geological events of artefacts on archaeological sites example of Dzierżysław archaeological site
Autorzy:
Pawlikowski, M.
Powiązania:
https://bibliotekanauki.pl/articles/183932.pdf
Data publikacji:
2007
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
sedymentologia
geoarcheologia
pogrązy
tonięcie
grzęźnięcie
sedimentology
geoarchaeology
sinking
Opis:
W artykule zaprezentowano wyniki badań terenowych i laboratoryjnych nad zjawiskami migracji archeologicznych zabytków krzemiennych po opuszczeniu stanowiska. Zjawiska te, zachodzące w większości stanowisk i obejmujące prawdopodobnie wszystkie rodzaje zabytków, są szczególnie dobrze widoczne w stanowiskach epoki kamienia ze względu na długi okres, który minął od ich opuszczenia przez człowieka. Umiejętność rozpoznania opisanych zjawisk w badanym stanowisku może decydować o poprawności rekonstrukcji faktów, które miały miejsce w przeszłości. W publikacji pokazano zjawiska migracji i grzęźnięcia zabytków krzemiennych na podstawie badań magdaleńskiego stanowiska w Dzierżysławiu i eksperymentalnych badań laboratoryjnych. Eksperymenty dotyczące zjawiska migracji zabytków potwierdziły różne tempo ich przemieszczania się. Zjawisko jest zależne od kształtu zabytków, ich ciężaru oraz środowiska, w jakim zabytki się znajdują. Małe i płaskie obiekty pogrążają się wolno, gdy tymczasem izometryczne i duże - szybciej. To wskazuje, że artefakty odkrywane w stanowiskach archeologicznych znajdują się w różnych stadiach migracji. Można także zauważyć, że migracja zabytków może być zróżnicowana nawet w obrębie jednego stanowiska archeologicznego.
This paper presents field and laboratory investigations concerning artefacts sinking in archaeological sites. These phenomena take place on most of archaeological sites. Most probably this process affect all categories of artefacts. Because of the time stone age sites are the best places to investigate sinking of artefacts. The correct interpretation of archaeological facts on the site could be based only on consciousness of the processes mentioned in this article. The particular example used here is Dzierżysław Magdalenian site and excavations on it as well as laboratory tests with "contemporaneous" flint flakes. Experiments concerning migration of artefacts confirmed various rate of their migration. Phenomenon is the result of shape of implements their weight as well as conditions at sediment. Small and flat objects migrated down slowly while isometric and heavy, faster. Was observed that during sinking tested objects did complicated motions. This suggest that artefacts discovered at archaeological sites are at various stages of migration. Moreover one can see that mentioned "activity" of objects is often various at various parts of one archaeological site.
Źródło:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2007, 33, 4; 463-471
0138-0974
Pojawia się w:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Paleoclimatological and geoarchaeological significance of the holocene loess – soil successions of the tien shan foothills of Uzbekistan
Autorzy:
Welc, Fabian
Suska-Malawska, Małgorzata
Toychiew, Khodjiakbar
Marks, Leszek
Mętrak, Monika
Powiązania:
https://bibliotekanauki.pl/articles/2025613.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Holocene climate change
geoarchaeology
Uzbekistan
Central Asia
loess – soil succession
Opis:
Scenario of climate changes in the Late Pleistocene and Holocene in Central Asia is very fragmentary and inconsistent. Therefore, interaction between the development and decline of ancient cultures and the climate fluctuations are difficult to be traced. To resolve this problem, the key role can be played by multidisciplinary studies of unique Late Pleistocene and especially Holocene loess – soil succession of the Tien Shan foothills in Uzbekistan. This area yields unique successions of paleosols interbedded with loesses that are particularly useful for paleoclimate analysis. They are represented by continuous and uninterrupted sedimentary sequences with a highly varied record of magnetic susceptibility. As such, they contain a full sequence of short-term climatic oscillations of the Holocene in high resolution and therefore, in this case, they are exceptional on global scale. The correlation of Late Pleistocene and Holocene climate changes scenario with stages of development and collapse of the past human settlement in Central Asia seems at present one of the most promising research directions, in line with the substantial course of interdisciplinary research on the interaction between humans and the natural environment.
Źródło:
Studia Quaternaria; 2016, 33; 57-68
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Disturbances of the holocene lake-bog sediment succession as revealed by pollen record from wietrzychowice (south eastern kujawy, central poland)
Autorzy:
Břízová, Eva
Roman, Małgorzata
Powiązania:
https://bibliotekanauki.pl/articles/2025780.pdf
Data publikacji:
2015
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
pollen analysis
geoarchaeology
post-depositional disturbances
human activity
Holocene
central Poland
Opis:
Re sults of geo log i cal and pol len in ves ti ga tions of the lake-bog sed i ments from the sec tion Wietrzychowice W5, located nearby the Neo lithic Fun nel Beaker Cul ture (FBC) mega liths, are pre sented. The pol len data re veal that sed imen ta tion at Wietrzychowice has be gun at the be gin ning of the Ho lo cene (Preboreal). Pol len anal y sis was used to determine stratigraphy with regard to sediment characteristics. The pollen spectrum was divided into 8 LPAZes (1-7Xa, 7Xb) which were also, where pos si ble, stratigraphically clas si fied. Ra dio car bon dat ing of 6 730 ± 90 BP (5 730–5 480 BC, MKL-702) at depth of 1.20 m con firmed the pol len anal y sis age es ti ma tion. Five set tle ment ep i sodes were found in or ganic sed i ments in the up per part of the W5 core. The first was pre sum ably dur ing the Preboreal, the sec ond in the early At lan tic, the third in the late At lan tic (prob a bly Neo lithic FBC), the fourth in the early Mid dle Ages and the last one in the late Mid dle Ages. The pol len anal y sis was use ful to point ir reg u lar i ties in sed i ment suc ces sion. Such a sit u a - tion made palaeoenvironmental in ter pre ta tion dif fi cult, but fur ther re search is still needed to en able an ac cu rate re construc tion.
Źródło:
Studia Quaternaria; 2015, 32; 91-97
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geoarchaeological evidence of late and post-Antiquity (5th-9th c. AD) climate changes recorded at the Roman site in Plemići Bay (Zadar region, Croatia)
Autorzy:
Welc, Fabian
Powiązania:
https://bibliotekanauki.pl/articles/2025093.pdf
Data publikacji:
2019
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
geoarchaeology
climate change
Roman period
Croatia
eastern Adriatic
Nauki o Ziemi
Opis:
Remains of a vast Roman pottery production complex were found on the shore of the Plemići Bay (Općina Ražanac, Zadar county) in 2012, and confirmed by geophysical survey. Ground-penetrating radar measurements revealed outline of a rectangular building that finds analogies with Roman storehouses (horreum). The area occupied by remains of the Roman pottery workshop was covered by immense soil-debris flows. Three geological exposures located to the north of the remains of the Roman building were documented using lithological and malacological analysis, and magnetic susceptibility measurements. The profiles revealed at least three generations of slope sediments, formed in result ofintensive soil or debris flows in a dry climate, most probably in 5th c. AD. In the next, wet phase sediments were transported downslope and deposited on the Roman structures after 5th c. AD. Environmental conditions at Pelmići weresupply with paleoclimate evidence from the Adriatic region. At ca. 1.5 cal. BP lake levels in the eastern Adriatic area were drastically reduced, probably because of strong decrease in humidity, correlated with the so-called North Atlantic Bond event 3. The drought was followed by a humid episode, also attested at the Plemići archaeological site.
Źródło:
Studia Quaternaria; 2019, 36; 3-17
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zapis geoarcheologiczny działalności człowieka w neoholocenie w południowo-wschodniej części Przedgórza Iłżeckiego (centralna Polska)
Geoarchaeological record of human activity during the Neoholocene in the south-eastern Iłża Foothills (Central Poland))
Autorzy:
Szeliga, Marcin
Dobrowolski, Radosław
Chodorowski, Jacek
Pidek, Irena Agnieszka
Mroczek, Przemysław
Powiązania:
https://bibliotekanauki.pl/articles/578389.pdf
Data publikacji:
2018
Wydawca:
Łódzkie Towarzystwo Naukowe
Tematy:
geoarcheologia
neoholocen
aktywność człowieka
antropopresja
Wyżyna Małopolska
geoarchaeology
Neoholocene
human activity
anthropopressure
Małopolska Upland
Opis:
W artykule zaprezentowano wyniki geoarcheologicznych badań przeprowadzonych w obrębie oraz otoczeniu dwóch wielokulturowych stanowisk archeologicznych w Tominach i Zawadzie (południowo-wschodnia część Przedgórza Iłżeckiego), w bezpośrednim sąsiedztwie północnej krawędzi pokrywy lessowej Wyżyny Sandomierskiej. Ich zasadniczych celem była kompleksowa rekonstrukcja osadniczej i gospodarczej aktywności człowieka w analizowanym obszarze w okresie ostatnich około 5 tysięcy lat, wraz z identyfikacją wszelkich jej uwarunkowań, zarówno na poziomie chronologiczno-kulturowym, jak i środowiskowym. Uzyskane wyniki pozwoliły na określenie przebiegu i skali lokalnych zjawisk kulturowych oraz związanych z nimi procesów osadniczych między późnym neolitem a czasami współczesnymi. Na podstawie uchwyconych śladów eksploatacji oraz przekształceń środowiska naturalnego podjęta została również próba określenia charakteru i stopnia lokalnej antropopresji w neoholocenie.
The article presents the results of geoarchaeological research carried out within and around two multicultural archaeological sites in Tominy and Zawada (south-eastern Iłża Foothills), in the immediate vicinity of the northern edge of the loess cover of the Sandomierz Upland. The main objective of the research was to comprehensively reconstruct human settlement and economic activity in the study area in the last ca. 5,000 years, along with identifying its conditions, both at the chronologicalcultural and the environmental level. The results allowed a determination of the course and scale of local cultural phenomena and related settlement processes between the late Neolithic and modern times. On the basis of traces of exploitation and transformation of the natural environment, an attempt was made to determine the nature and extent of local anthropopressure in the Neoholocene.
Źródło:
Acta Geographica Lodziensia; 2018, 107; 155-173
0065-1249
Pojawia się w:
Acta Geographica Lodziensia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Environmental history of the Csorna Plain (Western Danube Plain, NW Hungary) from the Late Glacial to the Late Holocene as seen from data of multiproxy geoarchaeological investigations
Autorzy:
Törőcsik, Tünde
Gulyás, Sándor
Sümegi, Pál
Sümegi, Balázs
Molnár, Dávid
Benyó-Korcsmáros, Réka
Powiązania:
https://bibliotekanauki.pl/articles/2025095.pdf
Data publikacji:
2019
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
fluvial geoarchaeology
environmental history
flood cycles
Danube Plain
NW Hungary
Nauki o Ziemi
Opis:
This study presents the results of a comprehensive geoarchaeological study implemented at an archeological site covering ca. 5 ha near the city of Csorna on the NW part of the Danube Plain, NW Hungary. The site itself exposed a complex fluvial system of an ice age creek with near bank and overbank areas (levee, point bar, back swamp). Spatial distribution of archeological features allowed for the interpretation of differential use of the fluvial landscape by different cultures. According to our data, the referred fluvial system must have emerged during the Late Glacial. At this time, creeks originating from hills to the SE followed a uniform NW trajectory. From the Holocene, small creeks were beheaded turning into inactive flood channels. It was the time when the gradual infilling of the floodplain started. Alternating layers of floodwater coarses and floodplain fines mark recurring floods at our site. These could have been correlated with cooler, wetter climatic phases of the North Atlantic, Western Europe and high stands in Central European lakes. Highest floods are recorded during the Late Bronze and Iron Ages besides the Neolithic. Pollen data enabled us to make inferences on the vegetation as well.
Źródło:
Studia Quaternaria; 2019, 36; 19-43
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Influence and Impact of Bioclimatic Indicators on the Evolution of Biosociety. A Geoarchaeological approach
Autorzy:
Malaperdas, George
Powiązania:
https://bibliotekanauki.pl/articles/1076724.pdf
Data publikacji:
2019
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Archaeology
Aspect
Bioclimatic Indexes
GIS
Geoarchaeology
Heat Load Index
Humidity
Solar Radiation
TWI
Wind Intensity
Opis:
The present paper attempts to attribute the role of bioclimatic indexes and their importance in the development and evolution of cultures. With the aid of GIS, a case study is presented aiming to point out the use of GIS is the study of bioclimatic indexes in theoretical study fields, such as, in this case, in Archaeology and more specifically, in the field of Geoarchaeology. Geoarchaeology is not a discipline, but an interdisciplinary approach, which has everything to gain by taking geomorphological methods and techniques into account (Fouache et al., 2010). Τhe study area is the Prefecture of Messenia, located in south west Greece. The Prefecture of Messenia is one of the best documented areas of mainland Greece. It has been both extensively surveyed and excavated. The archaeological finds are numerous, dating from prehistory to the modern times. Thus, a vast amount of information has helped historians, archaeologists and other scientists to recreate the past.
Źródło:
World News of Natural Sciences; 2019, 24; 183-198
2543-5426
Pojawia się w:
World News of Natural Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł

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