 takaj, prijelj, za organizacije. Tako, da je tukaj, da se je začal. Jelim je Norbert Fergov, in pa je v mene boš vznačil, da je nisem srečno. Prvome se je opušena, najsrečanje, da boš vse preliminari prizat v rizatni vsepovali v srednjiga, vsepovali. Povrčo, da boš vsepovali vsepovali vo najsrečanj preljavstvenj, z kvaliti v Anglijskih in arkelogij. v terboj burdej tel organization. Would only emphasize, the inner territories of the Carpathian Basin are un yapıyorsunnly scarcely known not just for the international mysevolGH research. The period between the late glacial, maximum and the dome of the whole scene witnessed several climatic fluctuations, but generally the temperature and the precipitation increased together. The inner part of the Carpathian Basin gradually showed the same characteristics as we knew it until the end of the 19th century. As it is shown on the map on the left, the larger part of the great Hungarian plane could have been described as a wetland, defined by the Donjub, the Tissa and several other smaller rivers and streams. Together with the encounter of the free main climatic belt, the continent of the Atlantic and the Submeditarianian, a very diversified environment came into being, thus we should imagine a very patchy flora and fauna both on micro and macro levels. Even nowadays, the general climatic description of the whole country cannot be conducted according to the global climatic classes. The definition is different from region to region, and it is based on different weather and moisture subdivisions. The question of the human adaptation to these conditions is a crucial one in archeological terms, whether the former epigravitian cultures continue to live on, or they give place to a self-enthardigravitian tradition. Nevertheless, this shift in the hunting strategy is reflected in the archeological material by the emergence of the geometric omicrolids. So the influence of the western tankle complex by Uronian-Sovterian cannot be disregarded. Concerning the wider early majority context in Europe, it is interesting that the intersection of the large cultural complexes situated just right inside the Carpathian basin, forming a very patchy general picture in archeological sense also. The main problem is that the Middle Danube region showed insignificant amount of archeological sites and atypical tool types until the middle of the 20th century, which concluded the introduction of agar culture and the theory of Mesolithic hiatus. From the 1990s, new sites were localized either in the Yashak region or in Transdanubia, which revised the later idea why the former term became outdated by moving its sites and finds into chronological different horizons. Begining with self-entransdanubia, the first site to mention is Saksar Polank. It was located during the construction of Shiodem in 1957. The excavation was conducted by Láslo Viertes, who observed six hearts on a 60-square-meter surface. The finds were situated in a loose layer dated to the reyanger dryas, which was deposited on the lowest sand terrace of the Danube. According to the typology of the stone tools, Viertes accepted this chronological frame, positioning the lifetime of the settlement around 10,000 BC. The assemblage of Saksar Polank belonged to the epigraphitean cultural entity with some azillio-tardanesian components. However, this typological point of view went through revision just recently with a detailed technological analysis. According to the revision, an intensive Bipolar technology was applied during the exploitation of the cores. Most of the times, the burins defined by Viertes in the 1960s seemed to be only unintentional technological byproducts. Concerning the utilized geomaterials, 70% are made of radial rights from different origins. Bakoy mountains, Mecek mountains, Croatia, the rest are limno-silicites, Cherhat mountains, Baltic erotic flint, and Volhynium flint. At Saksar Polank, Láslo Viertes tried his best from the means at his disposal in the 1950s. The chronology was reinforced by molecular, antracological, and radiocarbon resides, which were published also. According to the data, the human activity can be dated to a cooler and drier period before the beginning of the Holocene, which witnessed the last period of modestless accumulation since the last glacial maximum young at Reyes again. The vegetation can be reconstructed as a forest step, and one with marshland and deciduous forest components, while in the molecule found a cool tolerant and thermophilist species were both present. The small amount of animal remains belong to bison, deer, and beaver, while fish bones of bikes and sea prins were collected also. The site of Södliget-Walz was found during dam reconstruction works on the center of the Danube in 1954, at 200 meters distance away from the first spot, and a decade later another settlement spot was excavated. This time some fat settlement freatures, two hearts, and the ground plan of a habitation unit came to light. Unfortunately, this latter cannot be revised anymore, but according to the M.A.T.s of the David Kraus, the two industries represents two different chronological phases. The finds of Södliget were analyzed from the Indian typological aspect. The relative absence of the geometric microids and the high number of plague-based tools signifies these assemblages, altogether having a general epigravity and tardinozian impression. There are no points, no burins, and no signs of microburine technique. The shell on which these equipment were made of is mainly limik's site from the nearby Cherhat Mountains. The closest parallels of the rectangular form ground plans can be found at Lepenskivir near the Iron Gate. Unfortunately, the excavation of Södliget is lack of any detailed polyenvironmental analysis of radiocarbon dating, but according to M.G.Gabori, the chipped stones were situated just at the edge of the Holocene soil and the yellow sand layer below. The only arosological lapines from the site are the newly preserved teeth of Rodeir. The geomorphological analysis of the nearby Santander Island was conducted independently from the excavation 50 years later, but it may provide some clues about the environment in the early Holocene. In the region of the north and off-fold, the excavations of Yazberi 1 and Yaztelek 1 were parts of a larger systematic project of the amateur collector Dula Keregliato and archaeologist Robert Curtis. They localized many new sites with field walks along the meanders and dead arms of Zajvo and Tarno rivers. Two chronological phases were delinated in the frame of north-off-fold mesolithic industry, an older one, Yazberi, and the younger one, Yaztelek. The finds of the region of Yazsak were analyzed only from a typological view. According to the sites were marked with backpoints, mostly with arched retouch, shouldered and stovterian points were also noted. Geometric microlids like crescents, isoceres and skullenet triangles ruled the assemblages of the crystallization of microbran technique. Curtis highlighted the connections with the western softery and technical complex instead of the southern balkanic tardigravettian groups. The region of Yazsak witnessed the durable paleo-ecological analysis. According to this, the whole surroundings of the sites were reconstructed with complex methods. Polan analysis revealed that the human settlement was placed directly in the gallery woods with oak, elm, vilo, maple and with hazel at the shrub level. At the close vicinity both woodland and forest step were accessible for the hunters, who supposedly took advantage of the varied wide game fauna. The site, which is lying in northern Transdanubia was found during rescue excavation works connected to gravel and sand quarrying of the reconstruction of M86 motorway in 2014. It is situated on a sand dune in the flute plains of Raaba river, one kilometer south from Pali. According to the location of the first finds the excavation took place on the southern slope of the New Leaf open quarry pit in two faces, 2014 and 2015. It covered 60 square meters on which a larger part of a dense occupation spot came to light. Defines were situated in one cultural horizon in a dark grey paleo soil layer which was enclosed from above and below by a blueish greyish yellow brown clay silt. Below this compact strata a place to sink gravel layer could have been found with the thickness of some 10 meters. Apart from a moderately pigmented dark circle spot there were no habitation units recorded. According to our first results only 2% of the complete material proof to be format tool. The most numerous type is end scraper made on flake with 28 pieces. The triangles are second one with 16 pieces but they are not standardized. Only one scale came to light. Next group is the retouch plates, bladelets, which are mostly complete pieces. Sigments could have been found also but they are not standardized either. We have only one point, which at the peak are retouched on both sides. It's remarkable that there were not one single trapeze in the assemblage. At Pali Dombok we took advantage of the rare occasion to analyze a habitation spot like this. We used gamma morphological and sedimentological methods to fully understand the stratigraphy. We took samples for pollen analysis, we have charcoal samples for antracological and radiocarbon analysis and we have samples for OSL dating. Unfortunately, not all the results are available except the OSL dating for pollen analysis. The latter suggested a temporary drying condition of the environment with the complete absence of pollens. The former paleo-environmental investigation at Mezolak, some 20 kilometers away from our site, should suggest a mixed birch pine quarry forest with forest step-step at higher elevations. The general conclusion about the micro-scale environment of the epipelitic-mezolatic settlements may shed some light, why there are so few of them However, it may help to localize more with specific and aimed reconnaissance in the future. All of them are located directly in the full plains or on moderated sand elevations, having advantage of the close proximity both of the wetland, gallery forest and forest step. Unfortunately or fortunately these zones falls out of the scope of ordinary archeological and economical interests. According to the situation of the final paleolithic and mezolatic in the Carpathian basin on a larger scale a very diversified picture can be drawn. In the middle Danub region every macro region shows a different vegetation history which follows different paces. The different attributes of the aforementioned sites cannot be paralleled with climatic reasons directly but their correlation may deserve more attention in the future. And to emphasize this last thought we borrowed the caricature of Jean-George Rosoy from the publication of Jean-George Rosoy which is saying they are upsetting the weather with their flintchipping experiments. This opinion has as much scientific value as saying that changes in environment are the causes of changes in industries. So we have to take into account the cultural aspects as well. Thank you for your attention.