University Valahia Targoviste
Geography
Remote sensing is a useful tool for assessing, monitoring and conservation of groundwater with advantages of spatial and temporal availability of data from the large and inaccessible areas. Hydrogeological characteristics of a region are... more
Remote sensing is a useful tool for assessing, monitoring and conservation of groundwater with advantages of spatial and temporal availability of data from the large and inaccessible areas. Hydrogeological characteristics of a region are derived by surface indicators-geological features, geomorphology, hydrology, vegetation, land use. The paper deals with geological element as a factor influencing the hydrological and hydrogeological processes in the basin and adjacent areas Dambovicioara. Complexity of data provided by satellites (Landsat TM imagery) has facilitated the study of structural-tectonic (translated by liniaments), lithological and stratigraphic, which together resulted in delineation of perimeters of hydrogeologic potential in this area. In addition to direct benefits-such as geological information, spatial techniques have demonstrated clearly the usefulness and understanding of other factors responsible for maintaining the hydrological cycle-surface water, landforms, carpet plant.
Keywords: Remote sensing, liniaments, groundwater, structural-tectonic elements
Keywords: Remote sensing, liniaments, groundwater, structural-tectonic elements
Romanian Plain occupies from the geotectonic point of view, the northern part of Moesian Platform, a platform forming a rigid block between the Carpathians and the Balkans. Dacian Basin, opened after tectonic movements, badenian, in the... more
Romanian Plain occupies from the geotectonic point of view, the northern part of Moesian Platform, a platform forming a rigid block between the Carpathians and the Balkans. Dacian Basin, opened after tectonic movements, badenian, in the Sarmatian, outside the Carpathian arch, has evolved in a brackish sedimentation environment by the end of the Pliocene, after which was installed a lacustrine environment amid of water body restriction only in the southern part of Romania. The lacustrine system is installed in Quaternary amid climate cooling and morphological changes of the surrounding region and sedimentation basin. Basin silting was originally produced from the Carpathian chain, from north and from the Moesian platform south of Danube, which was in emerged position. Lacustrine sedimentation dominates in this phase of the material transported by river systems in the Carpathians and the southern frame of sedimentary basin. In a later phase, the conditions of sedimentation are diverse amid of dramatic global climate changes and dacic lake system withdrawal to the east.
Closure of the western part of the Moesian Platform determined lake system migration eastward from the Middle Pleistocene, and in the closing phase (the Holocene), to north-eastern Romanian Plain.
Under these conditions Quaternary succession is complete only in the Romanian Plain to the east of the Arges river, where it reaches considerable thickness, above. 400 m.
The lower limit of the Quaternary agreed to 1.8 Ma, since 1948, was confirmed by studying marine sediments from Vrica point (1985), and located approx. 4 km south of the peninsula of Calabria (Italy). Since 2009 the question of changing this limit based on studies made at Monte San Nicola in southern Sicily, to 2.558 Ma, which coincides with the Gauss-Matuyama magnetic reversal and Calabrian - Piacenzian limit, which is also the limit to the Pliocene.
New chronostratigraphical scale of the Quaternary fits much better climatic conditions for the submission of the Romanian Plain sedimentary sequences and can clarify the position of geomorphological subunits.
For example, the lower Quaternary was placed in the final sequence of the Cândeşti strata. After the new geochronological scale this sequence falls completely in Lower Quaternary and corresponds to the evolution realities of the dacic lake system in the Romanian Plain.
Keywords: Romanian Plain, glacial period, sedimentation sequence, collapsible deposits, sedimentation conditions, lacustrine and fluvial, sedimentation sources, Moesian platform.
Closure of the western part of the Moesian Platform determined lake system migration eastward from the Middle Pleistocene, and in the closing phase (the Holocene), to north-eastern Romanian Plain.
Under these conditions Quaternary succession is complete only in the Romanian Plain to the east of the Arges river, where it reaches considerable thickness, above. 400 m.
The lower limit of the Quaternary agreed to 1.8 Ma, since 1948, was confirmed by studying marine sediments from Vrica point (1985), and located approx. 4 km south of the peninsula of Calabria (Italy). Since 2009 the question of changing this limit based on studies made at Monte San Nicola in southern Sicily, to 2.558 Ma, which coincides with the Gauss-Matuyama magnetic reversal and Calabrian - Piacenzian limit, which is also the limit to the Pliocene.
New chronostratigraphical scale of the Quaternary fits much better climatic conditions for the submission of the Romanian Plain sedimentary sequences and can clarify the position of geomorphological subunits.
For example, the lower Quaternary was placed in the final sequence of the Cândeşti strata. After the new geochronological scale this sequence falls completely in Lower Quaternary and corresponds to the evolution realities of the dacic lake system in the Romanian Plain.
Keywords: Romanian Plain, glacial period, sedimentation sequence, collapsible deposits, sedimentation conditions, lacustrine and fluvial, sedimentation sources, Moesian platform.
The demands of the Romanian contemporary society are indissolubly related to the rapid development and modernization of the infrastructure. At the same time, the scientific research is moving towards the new directions imposed by an... more
The demands of the Romanian contemporary society are indissolubly related to the rapid development and modernization of the infrastructure. At the same time, the scientific research is moving towards the new directions imposed by an increasingly dynamic society and economy. In this context, inter- and trans-disciplinarity are required by the need to prepare new types of approaches, methods, techniques and technologies, to be able to answer the social and environmental impact produced and molded by the infrastructure.
The environment is a pluridimensional reality which includes both the natural and the cultural environment, and the actual concept of “environment” has a dynamic character that allows the knowledge, the analysis and the functioning of the protected systems with all their complexity.
This work proposes an efficient and modern model for the protection and conservation of geodiversity and of the cultural (especially archeological) patrimony by means of non-destructive (geophysical, remote sensing and photogrammetry, geochemical, seismic corroborated with informatic - GIS) techniques and methods with applicability in geosciences and especially with direct prevalence in archeology and geology. The presentation and promotion of these methods and techniques does not include the denial of the use of the traditional methods, which continue to provide numerous possibilities of identification and prognosis.
Keywords: infrastructure, geodiversity, cultural patrimony, non-destructive methods
The environment is a pluridimensional reality which includes both the natural and the cultural environment, and the actual concept of “environment” has a dynamic character that allows the knowledge, the analysis and the functioning of the protected systems with all their complexity.
This work proposes an efficient and modern model for the protection and conservation of geodiversity and of the cultural (especially archeological) patrimony by means of non-destructive (geophysical, remote sensing and photogrammetry, geochemical, seismic corroborated with informatic - GIS) techniques and methods with applicability in geosciences and especially with direct prevalence in archeology and geology. The presentation and promotion of these methods and techniques does not include the denial of the use of the traditional methods, which continue to provide numerous possibilities of identification and prognosis.
Keywords: infrastructure, geodiversity, cultural patrimony, non-destructive methods
Middle and Upper Jurassic deposits from the area of Piatra Craiului are part of the Piatra Craiului Formation [5] and are made up of deep facies appearing at the surface, especially on the western side of the massif. On the eastern side,... more
Middle and Upper Jurassic deposits from the area of Piatra Craiului are part of the Piatra Craiului Formation [5] and are made up of deep facies appearing at the surface, especially on the western side of the massif. On the eastern side, these facies appear sporadically, thinned due to tectonic effects. Also, they may be accompanied aby lowdepth carbonatic facies corresponding to the shelf.
Lithologically, it is possible to highlight microconglomerates, quartzitic gritstones, silts, reef limestone, brown-reddish limestones, black, red and greenish radiolarites, limestones with siliceous accidents disposed in slates, nodulous pinkish or whitish limestone (the Member of Valea Bârsei of Bajocian - Lower Tithonic age), reef limestone, intraclastic breccias (the Member of Şirnea of Upper Oxfordian - Kimmeridgian, the Member of Măgura Codlei of Tithonic). The study of the thin sections shows that these deposits are of the bioclastic rudstone type, turning to bioclastic intraclastic coarse grainstone. The hard ground surfaces and the reef bioconstructions that appear intercalated in the entire series, being embedded and developed on the facieses of carbonatic breccias are the characteristics of this time interval and of this area.
In this study, we intended to present a general outline of the palaeogeographic evolution of the area of Piatra Craiului circumscribed by the Dâmbovicioara Corridor during the time interval corresponding to the Middle and Upper Jurassic and also to highlight some of the important moments of this evolution, situating them in their regional context.
Keywords: palaeogeographic evolution, regional correlations, Middle and Upper Jurassic deposits
Lithologically, it is possible to highlight microconglomerates, quartzitic gritstones, silts, reef limestone, brown-reddish limestones, black, red and greenish radiolarites, limestones with siliceous accidents disposed in slates, nodulous pinkish or whitish limestone (the Member of Valea Bârsei of Bajocian - Lower Tithonic age), reef limestone, intraclastic breccias (the Member of Şirnea of Upper Oxfordian - Kimmeridgian, the Member of Măgura Codlei of Tithonic). The study of the thin sections shows that these deposits are of the bioclastic rudstone type, turning to bioclastic intraclastic coarse grainstone. The hard ground surfaces and the reef bioconstructions that appear intercalated in the entire series, being embedded and developed on the facieses of carbonatic breccias are the characteristics of this time interval and of this area.
In this study, we intended to present a general outline of the palaeogeographic evolution of the area of Piatra Craiului circumscribed by the Dâmbovicioara Corridor during the time interval corresponding to the Middle and Upper Jurassic and also to highlight some of the important moments of this evolution, situating them in their regional context.
Keywords: palaeogeographic evolution, regional correlations, Middle and Upper Jurassic deposits
- by Alin Frinculeasa and +1
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In 2011 the Museum for History and Archaeology of Prahova County conducted a series of rescue archaeological works in the area surrounding the city of Ploieşti. As a result, six tumuli (detected prior to this excavation at Ariceştii-... more
In 2011 the Museum for History and Archaeology
of Prahova County conducted a series of rescue archaeological
works in the area surrounding the city of Ploieşti. As a result,
six tumuli (detected prior to this excavation at Ariceştii-
Rahtivani (2), Păuleşti (3) and Strejnicu (1) were investigated.
Inhumation graves were uncovered (both principal and secondary
ones) with the individuals lying crouched on dorsal or lateral
decubitus positions, having their legs constricted, fallen or
lying laterally. Few grave goods were present. The burials
were dated to the Bronze Age, probably the Jamnaja funerary
horizon. Two other funerary complexes discovered at Păuleşti
and Strejnicu were attributed to horsemen populations from the
beginning of the IInd millenium AD. The grave from Păuleşti
contained, alongside the human remains remains, parts of a
horse skeleton. The human skeleton was lying on the back,
head towards the west, arms along the body, legs stretched.
The horse parts comprised the skull and the extremities of the
legs, found together with a horse bit, two arrowheads, a ring
and an iron object (whose functionality could not be determined
because of its precarious state of conservation). The tomb from
Strejnicu (probably a cenotaph) contained only the skull and
leg extremities from a horse, together with a horse bit, an
arrowhead and another iron object whose functionality could
not be determined for the same reason as above.
of Prahova County conducted a series of rescue archaeological
works in the area surrounding the city of Ploieşti. As a result,
six tumuli (detected prior to this excavation at Ariceştii-
Rahtivani (2), Păuleşti (3) and Strejnicu (1) were investigated.
Inhumation graves were uncovered (both principal and secondary
ones) with the individuals lying crouched on dorsal or lateral
decubitus positions, having their legs constricted, fallen or
lying laterally. Few grave goods were present. The burials
were dated to the Bronze Age, probably the Jamnaja funerary
horizon. Two other funerary complexes discovered at Păuleşti
and Strejnicu were attributed to horsemen populations from the
beginning of the IInd millenium AD. The grave from Păuleşti
contained, alongside the human remains remains, parts of a
horse skeleton. The human skeleton was lying on the back,
head towards the west, arms along the body, legs stretched.
The horse parts comprised the skull and the extremities of the
legs, found together with a horse bit, two arrowheads, a ring
and an iron object (whose functionality could not be determined
because of its precarious state of conservation). The tomb from
Strejnicu (probably a cenotaph) contained only the skull and
leg extremities from a horse, together with a horse bit, an
arrowhead and another iron object whose functionality could
not be determined for the same reason as above.
County Museum of History and Archaeology Prahova has conducted archaeological research since 2008 inside the St. Nicholas parish precinct, Slobozia district of the city of Câmpina. The site identified here is placed on a high terrace at... more
County Museum of History and Archaeology Prahova has conducted archaeological research since 2008 inside the St. Nicholas parish precinct, Slobozia district of the city of Câmpina. The site identified here is placed on a high terrace at the confluence of rivers Doftana and Prahova, in the sub-Carpathian hills at an altitude of 500 m, near the Carpathian Mountains. After the archaeological research conducted in 2008-2010 in the south of the parsonage over 30 graves dating from the Bronze Age were discovered. Regarding the funeral rites both inhumation and cremation are present, the first prevailing. It is remarkable the diversity and complexity of rituals present in this prehistoric cemetery. Inhumation graves have rectangular pits with rounded corners. Pit depth is about 40-50 cm for inhumation tombs. For cremation tombs the bones were placed in small pits lined with stones, over which a small mound was made. Cremation burials were identified at 30-50 cm deep, while inhumation graves at 60-90 cm. Above the interred individual a mound of stone and/or soil was arranged, exceeding in size the dimensions of the pits. These mounds were visible and marked the graves. Some graves, both inhumation and cremation, were plated on the sides and bottom hole with rocks. In the case of cremation graves, the bones were placed, after they were collected from the pyre, in an urn (container) or fitted directly into the pit. The pieces of bone found in the inventory of such tombs show traces of secondary burning, which indicates that they burned together with the deceased. The buried deceased were laid down crouched on the right or left side, rarely on the back, their arms were taken to the front. They were oriented approximately east-west, head east or west. There are also two skeletons with the head oriented to the north. The grave inventory consisted of vessels, but also pieces of jewelry made of bone, bronze, amber, glassy paste, clay. The richest in terms of inventory are graves 2, 6, 7, 11, 14, 20, 27. There are graves with a pot or two, but also three cremation graves that have four pots and remains from other vessels. Most of the deceased had deposited in the area of the head (towards the face or neck) decorated or undecorated pottery. The most frequently encountered form is the cup with one or two raised handles. Bowls, amphorae and jugs are also present. Some of the pots from cremation graves were placed upside down. Ornaments occur relatively frequently in the inventory of graves. There are small parts, made neatly. On the left arm of the deceased in the tomb 26, who belonged to a child, is a small bronze bracelet. In a grave (M5) a bronze earring was found in the area of the right ear, two bronze earrings in tomb 20. In the same tomb were found three „pearls” of clay and four of green or white, translucent glassy paste. A small wand of bone was discovered in an amforoidal dish which was placed in a cremation grave (M27). The same situation was found in another tomb (M6) where an ornament of bone was found along with the bones deposited in a beautifully decorated urn. A bead of amber was discovered along with a cup in the M10 inventory. A bone needle was found in the M31, and 30 tali, some of them processed, were found in M30. In M30 were also found two pieces made of a bronze plate with jagged edges. In some graves animal bones were discovered, probably from the offerings made near the deceased. All vessels from these tombs show traces of secondary burning. They are modeled of clay, not always of best quality. They are decorated with incisions, stitches and vertical grooves resulting specific motifs for the late phase of Monteoru culture. A bowl decorated with stitches discovered in M2 with a form of Kantara is specific for Tei culture. In another tomb (M32) was found a cup decorated Tei manner. More undecorated vessels, with raised handles, can be attributed to Noua cultural background. Another Noua pot discovered in M23 was decorated with circular grooves placed under the rim and was provided with small lugs applied below the rim, symmetrically arranged. A truncated cone cup with slightly curved walls had besenstrich decor. Anthropological examinations showed that the tombs belong to young people, aged 25-35 years, men and especially women. In 2010 graves were discovered belonging to children, some under the age of three years. Also, there are a few graves attributed to people who are aged over 50 years old. It should be noted for the inhumation graves that despite different orientations, all individuals were sitting crouched ventral, dorsal less, which indicates certain beliefs about this position through analogies with fetal position. Based on the rite, ritual, archaeological inventory, but also from absolute dating, the cemetery seems to have functioned in the Late Bronze Age. The exceptional nature of this cemetery is the appearance in it of tombs dating from three distinct cultural manifestations, namely Tei, Monteoru and Noua, a unique situation in Wallachia until now, in fact in the entire area of such cultural manifestations.
This paper draws attention to the unexploited potential of cartographic material related to Ploieşti city, Romania, from the oldest reports to the modern. The cartographic document may bring valuable, more often than not original,... more
This paper draws attention to the unexploited potential of cartographic material related to Ploieşti city, Romania, from the oldest reports to the modern. The cartographic document may bring valuable, more often than not original, information in order to improve understandings of behavioural patterns and the evolution of prehistoric communities. The study of the distribution and dynamics of burial mounds (tumuli) associated with the Bronze Age, within the perimeter of Ploieşti city and its metropolitan area, is one of the first applications of this kind of analysis made in Romania, and succeeds in showing the importance of using direct or indirect data from this category of cartographic documents for archaeological studies. Moreover, it demonstrates that, because geosystems and social systems are not static in space and time, a diachronic cartographic study provides the opportunity for a phenomenological focus on the evolutional issues of tumuli – spatiality, boundaries, distances and density.
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