Provider: - Institution: Koroška osrednja knjižnica dr. Franca Sušnika - Data provided by Europeana Collections- Opis fotografije (po rokopisu dr. Franca Sušnika):V drugi vrsti duhovniki (od leve na ...desno): Nužej iz Pliberka, Serajnik (Kotlje), Viternik, Alojz Kuhar, Serajnik (Dravograd), Križaj, Rozman, …?V prvi vrsti dekleta (Od leve): Petrač Alojzija, Jugova Tončka – Cvitanička, Petričeva …?, Skitek Jožefa (Šimnove matere sestra; bila je mlajša kakor njen nečak dr. Franc Kotnik). V sredini Šimen Kotnik; dalje proti desni: sestra Minka (pozneje poročena Remše), Mira Piskernik (zaročenka dr. Janka Kotnika), Jaroševa sestra Marija Kotnik (izseljena v Srbijo leta 1941), terezija Kotnik – Petračka.Na tleh sedijo (od leve): Pavlika Kotnik (poročena Kordež), Dobrovnica, Alojzija Lopan (poročena Plimen), Marija Poleže – Skitkova (Prežihova), …? Fantek na levi: Jugov Janko (Kotnik), sedaj (1977) dekan pri Lenartu v Slovenskih goricah ali pa njegov brat Ludvik (gospod pri Jugu na Dobrijah)77:929 Kotnik, rodbina- All metadata published by Europeana are available free of restriction under the Creative Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Provider: - Institution: Koroška osrednja knjižnica dr. Franca Sušnika - Data provided by Europeana Collections- Opis fotografije (prepis rokopisa dr. Franca Sušnika):Spredaj sedijo otroci na tleh ...od leve: Petrač Tonč – Ludvik Kotnik p.d. Juh, Franc Kotnik (učitelj, Jarošev brat), dve deklici (Petračeva ?, Lopan Alojzija Plimen), Zorko Kotnik, Rozika Kotnik (pozneje Dobrovnica), Blaže Marija, Bogomil Kotnik (v tiskarni), Franc Petrač (učitelj).Sedeča vrsta od leve: Luka Kotnik (padel v Rusiji), Andrej Kotnik, Križaj Avguštin, Volben Serajnik (prošt), oče Dominik (Županc), Šimen, mati Helena Kotnik, Rozman Jurij, dr. Franc Kotnik, Rezika Kotnik (Francova žena), Minka (sestra).Za temi stojijo: Serajnik (hotuljski župnik), dr. France Kotnik? (oficir? Madžar ?)Elizabeta Kotnik (Miklnova hči iz Šentanela – Juginja), Lika Juh (brat očeta Županca), Terezija Kotnik (potem Petračka), Jugova Tončka (Cvitanička), Mira Piskernik, Kuhar Lojz, Jožefa Skidek (v službi v Hotelu Orel), Marija Kotnik (Jaroševa polsestra), Petrač Alojzija, Petrač Ela?, Viternikova mati, …? iz Črneč, Glavar Jera (Župančeva sestra in “teta”), Klančnica ? Kogelnikova iz Črneč, voznik in farovška kuharica, hlapec in dekla pri Župancu.Stojijo zgoraj od leve: Nužej iz Pliberka, Potočnica z Dobrij, Potočnik (oče rezbarja Rutnika), Oset Andrej in žena, Glavar Marija (Tičlerica), Justina Blaže (materina sestra), Jaroševa mati in oče Franc Kotnik, oče Viternik, Viternik, neznani bogoslovec, Mirko Kotnik (orožnik v Murski Soboti).Zadnja vrsta: Glavar Alojz, Šteharnik, Kogelnik, Glavar Andrej (ta stari Tičler), stari Blatnik (Dominik Glinik).- All metadata published by Europeana are available free of restriction under the Creative Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Provider: - Institution: - Data provided by Europeana Collections- Posnetek vasi Dole, spredaj drevesa- All metadata published by Europeana are available free of restriction under the Creative ...Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
The geotectonic events in Late Cretaceous - Early Paleogene interval, caused essential changes in the architecture of the Tethysian paleogenic sedimentation basins and their relationship with the ...continental source areas. Laramic tectogenetic paroxysm (Maastrichtian/Danian) due to the subduction of the East European craton under the Tisza-Dacia block, plays a double role in the structuralization of the East Carpathian units. In an internal position, the External Dacides are built (The Black Flysch, Baraolt, Ceahlau and Bobu nappes, senso Sandulescu, 1984), and in the external part the Paleogene Foreland basin depozones (equivalent to the "Foreland basin", senso Grasu et al., 1999). The basin worked up to the Lower Miocene, when the styric and moldavic tectogenesis occurred and the Moldavian units were born (from the inner part to the outside are: Marginal Folds Nappe, Macla Nappe, Audia Nappe, Tarcau Nappe, Vrancea Nappe and Subcarpathian Nappe, senso Sandulescu 1, 1984). The Moldavian tectogenesis (intra Volhinian) concludes the Carpathian structogenesis and edification of the major morphostructural lines of the Carpathian contact with the eastern foreland. Between the Suceava and Modova valleys, the transition from the mountainous relief (Obcina Mare) to the plateau is made through the piedmont hills formed on the subCarpathian molasse or the Volhinian platform couverture deposits, accumulated on the wedge-top of the Carpathian orogenic prism.
An interdisciplinary study (cartographic and historical records, geomorphological, geological and bathymetric survey, water analysis, sediment coring and analysis and AMS radiocarbon dating) of two ...small and previously unreported lakes (Iezer and Bolătău) in Obcina Feredeului Mountains, northeastern Romania, provides new data into the environmental history and possible human impacts over the last millennium in this region. The first recorded historical reference to Iezer Lake dates to 1594 AD, and to Bolătău Lake to 1806 AD. Two sediment cores (420 cm for Iezer and 540 cm for Bolătău) of finely banded lake sediments and a radiocarbon age estimate at Iezer Lake suggest that this lake may represent the oldest landslide lake in Romania. The geomorphological, geological, and morphometric surveys indicate that these lakes' origins relate to landslide activity. Coarse grained, lighter sediment bands are generally characterized by higher values in magnetic susceptibility, Saturation Isothermal Remanent Magnetisation (SIRM), as well in geochemical indicators such as Ti and Zr, and low organic content, possibly indicating periods of increased runoff. Conversely, finer-grained, dark sediment bands show lower values in magnetic susceptibility, SIRM, Ti and Zr and higher organic content, and are likely to suggest quieter deposition periods. However, there are two significant episodes of markedly increased surface erosion. The oldest occurs between 100 and 110 cm, and might be coincident with the terminal part of Little Ice Age (LIA), whereas the youngest in the top 30 cm coincides with recent land use. These lakes hold significant potential in providing an important perspective on the environmental conditions over the last millennium and, more specifically, to supply new information about the Medieval Warm Period (MWP) and LIA signals in the NE Romanian Carpathians. These two landslide-dammed lakes should be defined as scientific reserves to ensure their protection and to enhance their use as a scientific and educational resource.
Harta L-35-003-D-b Direcția Topografică Militară General de Divizie „Constantin Barozzi
1991
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Provider: - Institution: - Data provided by Europeana Collections- 1:25000- Proiecția Stereografică 1970- All metadata published by Europeana are available free of restriction under the Creative ...Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Harta L-35-003-B-d Direcția Topografică Militară General de Divizie „Constantin Barozzi
1991
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Provider: - Institution: - Data provided by Europeana Collections- 1:25000- Proiecția Stereografică 1970- All metadata published by Europeana are available free of restriction under the Creative ...Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Harta L-35-004-C-c Direcția Topografică Militară General de Divizie „Constantin Barozzi
1991
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Provider: - Institution: - Data provided by Europeana Collections- 1:25000- Proiecția Stereografică 1970- All metadata published by Europeana are available free of restriction under the Creative ...Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Harta L-35-003-B-c Direcția Topografică Militară General de Divizie „Constantin Barozzi
1991
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Provider: - Institution: - Data provided by Europeana Collections- 1:25000- Proiecția Stereografică 1970- All metadata published by Europeana are available free of restriction under the Creative ...Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Harta L-35-016-A-d Direcția Topografică Militară General de Divizie „Constantin Barozzi
1991
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Provider: - Institution: - Data provided by Europeana Collections- 1:25000- Proiecția Stereografică 1970- All metadata published by Europeana are available free of restriction under the Creative ...Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
