The exploration of hunting tourism reveals its multifaceted benefits, encompassing nature preservation and tourism expansion. This study delves into the dynamics and prospective trends within hunting ...tourism, specifically in Prlekija's administrative unit of Gornja Radgona, Slovenia. It commences with a comprehensive international comparative analysis, followed by insightful semi-structured interviews involving key stakeholders within the destination. Hunting tourism emerges as a pivotal facet of tourism within this locale, exhibiting substantial potential for further growth, particularly in terms of diversification, regional integration, and synergy with other tourism offerings. However, it's imperative to address the adverse impacts of hunting tourism on biodiversity. As a counterbalance, the study underscores the increasing global emphasis on sustainable variants of hunting tourism, such as wildlife photography, fostering a more conscientious approach to animal tourism practices.
At the end of May 1950, the Gornja Radgona department of the State Security Administration (UDV Gornja Radgona) arrested Ivan Štrafela Don, and the Party’s district committee questioned him and ...accused him of overt action against the state as a Cominform member. He admitted almost all of the actions he was being accused of and was willing to present them before the workers and the members of the Party as well. At the end of October 1950, after being expelled from the Party, the District Court in Maribor sentenced him to eight years of imprisonment with forced labour and five years of loss of civil and political rights. The attempts of the convict’s wife to achieve a lower punishment were unsuccessful; however, Štrafela was nonetheless pardoned in 1955, and he returned home. He did less demanding and responsible work in the industry and local politics, but he remained under surveillance and was preventively detained during Tito’s visit in the Pomurje region (in 1966 and 1969). His wife’s attempts to achieve a revision of the procedure after his death (1986) were unsuccessful between 1999 and 2001.
Obuhvatnim istraživanjima različitih arhivskih izvora relevantnih za problematiku transfera vlasništva umjetnina neposredno prije i tijekom Drugoga svjetskoga rata te u poslijeratnom razdoblju ...utvrđeni su raniji vlasnici i/ili neke od okolnosti promjena vlasništva nekoliko slika koje su u zbirni fond Strossmayerove galerije starih majstora HAZU pristigle temeljem odluka državnih tijela Federativne Narodne Republike Jugoslavije između 1948. i 1958. godine. Istraživanje sudbine tih slika prije i tijekom Drugoga svjetskoga rata dopunjeno je analizom arhivskih dokumenata koji svjedoče o procesu poslijeratne muzealizacije brojnih umjetnina u hrvatskim muzejima.
Middle to Upper Pliocene (~
3
Ma) Grad Volcanic Field (SW Pannonian basin system) encompasses an area of about 3
km
2, of which some 1.7
km
2 belong to the outcropping volcanics. Pyroclastic and ...syn-eruptively reworked volcaniclastic deposits are the most widespread in occurrence. Remains of an autobrecciated lava flow, a residual neck and their peperites are partially reworked by a large debris flow.
Volcanic activity occurred in a continental depositional environment dominated by alluvial fan and braided river systems. Streams draining from the north-west to the south-east were infilling a rapidly subsiding Radgona Depression.
The style of volcanic activity was mainly explosive and was reinforced by hydrovolcanic processes. Three volcanic centres probably existed, and they migrated spatially and temporally from the north to the south over a distance of some 5.6
km. The rocks of the northernmost volcanic centre are fairly eroded and contain abundant, up to 10
cm sized lherzolite xenoliths.
The largest crater developed about 2.5
km to the south. From an early maar stage, a tuff-cone, and subsequently, a tuff-ring evolved. The crater was filled with eroded pyroclastic material and stream load.
A new vent became active some 500
m to the south. Initial stage was mainly magmatic and produced pyroclastic flow and fall deposits. Late-stage eruptions were predominantly hydrovolcanic (phreatomagmatic and phreatic), and built up a small tuff-cone having some 300
m in diameter.
Trachybasaltic and subordinate basanitic magmas erupting in the Grad Volcanic Field are geochemically distinguishable from the neighbouring occurrences in the South Styrian Basin and the South Burgenland Swell. Relatively lower abundance of TiO
2, MgO, Sc, V and Cu, and higher abundance of MnO, P
2O
5, Zn, Sr, Zr, Hf, Nb, Ba, Ta and U indicate somewhat different source and/or evolutionary pattern.
► The Grad Volcanic Field developed ~3 Ma ago in an active alluvial fan environment. ► Trachybasaltic and basanitic magma affinity prevailed. ► Phreatomagmatic and phreatic explosive activity occurred. ► Various fluvial-volcaniclastic deposits developed.
Extended description:
Gornja Radgona: mejni prehod, posledice bojev, ruševine v Gornji Radgoni, uničeni avtomobili, enote teritorialne obrambe, poškodovana streha, pozdrav z avstrijskimi policaji na ...mostu, vojaška vozila vozijo skozi Radence, izjava Alojz Vogrinčič, župan občine Gornja Radgona.
Information:
Gornja Radgona: The YA retreats from the border crossing; the aftermath of fierce fighting during the siege and the ruins.
Original language summary:
Gornja Radgona: umik zvezne armade z mejnega prehoda; posledice hudih bojev med obleganjem, ruševine.
Extended description:
Zavijanje siren, zatekanje v zaklonišča in oglušujoči zvoki letal s smrtonosnim tovorom ter mučne eksplozije ob srditih spopadih so zaznamovali dan, ki ga ni moč pozabiti. ...Poglejmo kaj se je dogajalo v Gornji Radgoni.
»... Gornja Radgona je zavita v dim, ogen, pa tudi verjetno v kri. Takšnega barbarstva so bili sposobni samo nacisti, to pa so nacisti s peterokrako rdečo zvezdo.«
Information:
Gornja Radgona: An air raid and fierce conflicts; houses on fire, smoke above roofs, tanks, a damaged church belfry, Austrian soldiers, an ÖRF helicopter and a school on fire.
Original language summary:
Gornja Radgona: letalski napad in srditi spopadi; goreče hiše, dim nad strehami, tanki, poškodovan cerkveni zvonik, avstrijski vojaki, helikopter ÖRF, šola v plamenih.
Anton Krempl se je rodil 29. januarja 1790 na Poličkem vrhu pri Gornji Radgoni.Razglednico Radgone in zaledja iz ptičje perspektive je založil Albin Sussitz, Graz, 1912/1914
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