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Wyszukujesz frazę "geoheritage" wg kryterium: Temat


Wyświetlanie 1-7 z 7
Tytuł:
Geomorphosites of Poland : the role played by the Central Register of Geosites
Autorzy:
Warowna, J.
Migoń, P.
Kołodyńska-Gawrysiak, R.
Kiebała, G.
Zgłobicki, W.
Powiązania:
https://bibliotekanauki.pl/articles/294645.pdf
Data publikacji:
2013
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
Geomorphosites
geoheritage
geodiversity
Polska
Opis:
Poland is a country of considerable geomorphological diversity and includes a range of physical landscapes, from high mountains through uplands, plains, glaciated lowlands, large river valleys, to coasts. Within them, numerous localities may be considered as geomorphosites, illustrating key stages in the geomorphic evolution of the territory, classic landforms and the recent operation of geomorphic processes. The only database that aims to cover all geosites in Poland, including sites of geomorphological interest, is the Polish Central Register of Geosites (PCRG), managed by the state geological survey – the Polish Geological Institute (PIG). Among more than 2200 geosites recorded about 30% can be considered as geomorphosites. Their spatial coverage is very uneven. Most are located in the upland belt of southern Poland (40%) and in northern part of the country, within the extent of the late Pleistocene ice sheet (29%), while the Carpathians are under-represented. Thematically, geosites illustrating various examples of denudational relief dominate (45%). Significantly less common are glacifluvial (13%), glacial (11%) and fluvial (10%) landforms. Tors and residual hills are most common among geomorphosites (205 sites), followed by moraines (52), dunes (49), gullies and their systems (45) and river valleys (34). Thus, PCRG does not yet adequately reflect the diversity of the geomorphological heritage of Poland.
Źródło:
Landform Analysis; 2013, 22; 117-124
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
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:
Existing and Proposed Urban Geosites Values Resulting from Geodiversity of Poznań City
Autorzy:
Zwoliński, Zbigniew
Hildebrandt-Radke, Iwona
Mazurek, Małgorzata
Makohonienko, Mirosław
Powiązania:
https://bibliotekanauki.pl/articles/1052437.pdf
Data publikacji:
2017-09-15
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
urban geosite
geodiversity
geoheritage
cultural heritage
Polska
Opis:
Poznań, a city in central-western Poland, is located in the lowland region but has no less attractive geomorphological and human history. It was here that Poland was born at the end of the tenth century. The city’s location is connected with the meridian course of the Warta River valley. In contrast, in the northern part of the city, there is a vast area of the frontal moraines of the Poznań Phase of the Weichselian Glaciation. Against the backdrop of the geomorphological development of the city, the article presents the existing geosites, classified as urban geosites. The present geosites include three lapidaries with Scandinavian postglacial erratics, one of them also with stoneware, a fragment of a frontal push moraine and impact craters. Besides, three locations of proposed geosites with rich geomorphological and/or human history were identified. These are as follows: the peat bog located in the northern part of the city, defence ramparts as exhumed anthropogenic forms, and the Warta River valley. The existing and proposed geosites in Poznań were evaluated in three ways. In general, it should be assumed that the proposed new geosites are higher ranked than the current ones.
Źródło:
Quaestiones Geographicae; 2017, 36, 3; 125-149
0137-477X
2081-6383
Pojawia się w:
Quaestiones Geographicae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dziedzictwo geologiczne
Geological heritage
Autorzy:
Urban, Jan
Migoń, Piotr
Radwanek-Bąk, Barbara
Powiązania:
https://bibliotekanauki.pl/articles/2076132.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geodziedzictwo
geostanowiska
geokonserwacja
georóżnorodność
geoheritage
geosites
geoconservation
geodiversity
Opis:
Geoheritage (geological heritage), that is tangible evidence of geological past and contemporary processes, is increasingly recognized as a valuable component of environment, worth conservation and popularization. It comprises elements of Earth's geodiversity, which are significant for scientific, educational, cultural, ecological or aesthetic reasons. Among them, the key role is played by geosites, at which elements of geoheritage are best exposed and have the most evident value. Various classifications of geosites by the main theme have been proposed and various methods of evaluation of geosites exist, involving among others, assessment of their scientific importance, cultural/historical value, threats and educational opportunities. Geoheritage in a given place or area may have global, national, regional or local significance. Globally significant geoheritage is protected at UNESCO World Heritage properties and in UNESCO Global Geoparks. In Poland, geoheritage is protected in national and landscape parks, more than 110 nature reserves, more than 1600 nature monuments and more than 120 sites of special scientific interest (documentary sites). This paper opens a section of "Przegląd Geologiczny", in which representative geosites of Poland will be successively presented.
Źródło:
Przegląd Geologiczny; 2021, 69, 1; 16--20
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Analysis of proposed geosites in the Betong District, Yala Province, Southern Thailand
Autorzy:
Nazaruddin, Dony Adryansyah
Singtuen, Vimoltip
Baharim, Nor Bakhiah
Abdul, Rahman Muhd Nur Ismail
Powiązania:
https://bibliotekanauki.pl/articles/24201076.pdf
Data publikacji:
2023
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
geodiversity
geoheritage
geoconservation
hot springs
waterfalls
georóżnorodność
geodziedzictwo
geokonserwacja
gorące źródła
wodospady
Opis:
This study aims to analyse the geosite candidates of the Betong District (Yala Province) in Southern Thailand by means of several methods including inventory, characterisation, classification, assessment and SWOT analysis. Results of the present study are illustrated through seven proposed geosites that become resources for the development of the Betong District, namely Betong Hot Spring, Inthasorn Waterfall, Chaloem Phra Kiat Waterfall, Mount Silipat and Nakor Hot Spring, as well as Piyamit Tunnel and Aiyerweng Skywalk, two human-modified sites which can be used to observe geological and geomorphological features. The present study is expected to promote the conservation and development of these resources as geological heritage of the district.
Źródło:
Geologos; 2023, 29, 2; 99--116
1426-8981
2080-6574
Pojawia się w:
Geologos
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Analysis of the geotouristic potential of geosites in Divjakë-Karavasta National Park, Albania
Autorzy:
Braholli, Ermiona
Dhimitri, Jostina
Powiązania:
https://bibliotekanauki.pl/articles/2204348.pdf
Data publikacji:
2022
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
geodiversity
geoheritage
protected area
GAM model
SPSS analyses
georóżnorodność
geodziedzictwo
strefa chroniona
model GAM
analizy SPSS
Opis:
Elements of geodiversity evaluated for scientific value should be protected, conserved and promoted as potentially important for geotourism. The Divjakë-Karavasta National Park is a large natural area that comprises six geosites along the Adriatic coastline of Albania. Geosites are elements of the geosphere that should be preserved for geoeducation of the present and future generations, in view of the fact that they yield significant data on Earth’s history. By means of the Geosite Assessment Method (GAM) and the SPSS program (version 20), we have analysed the geotouristic values of the Divjakë-Karavasta geosites and interpreted the importance of each subindicator. A correlation analysis, performed through SPSS and Pearson’s correlation coefficient as a test statistics, has been carried out as well. The Pearson’s correlation coefficient reflects the strong relationship between the scientific/educational values (i.e., representativeness and scientific knowledge) and touristic values (promotion, number of visitors, interpretative panels, hostelry services, restaurant services, touristic infrastructure). These coefficients express the importance of the dependence of additional values in the development of geotourism at protected sites.
Źródło:
Geologos; 2022, 28, 2; 141--155
1426-8981
2080-6574
Pojawia się w:
Geologos
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Residual rocky forms in the landscape of the Outer Carpathians (Silesian Beskid Mts, Poland) – geotourist and sedimentological case study
Ostańcowe formy skałkowe w krajobrazie Karpat zewnętrznych (Beskid Śląski, Polska) – geoturystyczne i sedymentologiczne studium przypadku
Autorzy:
Strzeboński, Piotr
Powiązania:
https://bibliotekanauki.pl/articles/27323849.pdf
Data publikacji:
2021
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
relict landform
sandstone-conglomerate tor
rocky geosite
geoeducation
geotourism
geodiversity
geoheritage
geoconservation
Carpathian flysch
ostańcowa forma terenu
piaskowcowo-zlepieńcowa skałka
geostanowisko skałkowe
geoedukacja
geoturystyka
georóżnorodność
geodziedzictwo
geoochrona
flisz karpacki
Opis:
This study investigated residual landforms developed within of the flysch bedrock in the Outer Western Carpathians as sand-stone-to-conglomeratic tors. The studied relic rocky forms are locally exposed on the valley slopes in the top and plateau parts of the Sile-sian Beskid Mts. The cognitive values of such relic landforms, especially in the context of their morphogenetic traits and shaping of their macro- and microrelief, are well known and described. In contrast to epigenetic processes, the sedimentological aspect of the origin of such siliciclastic rocky deposits is still subject to different approaches in terms of terminology and interpretation. Thus, the aim of this study is to describe the conditions of environmental settings and character of the sediment transport and deposition processes from gravity flows, and to present a depositional system model for such a variety of flysch deposits. This study also attempts to present geotourist and geoed-ucational attractiveness of the tors against the background of regional geodiversity, geoheritage, and geoprotection. The results yielded a synthetic morpho-litho-sedimentological and geotouristic specification of the rocky forms analysed. The residual rocky landforms are polygenic geomorphological elements developed as a consequence of multistage and different scale of morph-forming activity operating on the basis of litho-sedimentological and tectonic assumptions under the influence of denudation processes.
Przedmiotem artykułu są ostańcowe formy terenu rozwinięte na bazie fliszowego podłoża skalnego w zachodnich Karpatach ze-wnętrznych jako skałki od piaskowcowych do zlepieńcowych. Omówione ostańcowe formy skałkowe lokalnie eksponowane są na stokach dolinnych w przyszczytowych i wierzchowinowych partiach Beskidu Śląskiego. Walory poznawcze, jakie ze sobą niosą, w szczególności w kontekście morfogenetycznym oraz kształtowania ich makro- i mikroreliefu, są dobrze poznane i opisane. W przeciwieństwie do procesów epigenetycznych aspekt sedymentologiczny pochodzenia takich silikoklastycznych utworów skałkowych jest natomiast nadal przedmiotem dociekań zarówno w kwestii terminologicznej, jak i interpretacyjnej. Celem badawczym artykułu jest zatem próba przybliżenia warunków środowiskowych ustawień, natury procesów transportu i depozycji osadów ze spływów grawitacyjnych oraz modelu systemu depozycyjnego takiej odmiany utworów fliszowych. Zamierzeniem autora było także przedstawienie geoturystycznej i geoedukacyjnej atrakcyjności ska-łek na tle regionalnej georóżnorodności, geodziedzictwa i ich geoochrony. W rezultacie przedstawiono w ujęciu syntetycznym specyfikację morfologiczną, litologiczną, sedymentologiczną i geoturystyczną badanych form skałkowych. Ostańcowe skałkowe formy terenu stanowią poligeniczne elementy geomorfologiczne rozwinięte w następstwie wieloetapowej i różnoskalowej działalności rzeźbotwórczej zachodzącej w utworach o określonych uwarunkowaniach litologiczno-sedymentologicznych i tektonicznych za pośrednictwem procesów denudacji.
Źródło:
Geotourism / Geoturystyka; 2021, 1--2 (64--65); 3--22
1731-0830
Pojawia się w:
Geotourism / Geoturystyka
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-7 z 7

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