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Information about alteration degree of weathered deposits is offered by proportion of Al and Si. If this proportion is reduced, that means a strong alteration of the materials.

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The results obtained using the benchmark mineral method shows low and medium alteration stages of the rocks and weathered materials. Relative methods allowed the evaluation of the degree of weathering by using indices that highlight the ratio between stable oxides and those less stable from weathered deposits.

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The calculation was made for many samples and the results obtained indicate again low and medium values of alteration for rocks and weathered materials. These values characterize mountain areas where the alteration products are continuously evacuated from the weathering system.

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Therefore, the occurrence of intense altered deposits is rare, while low and medium weathered deposits are dominant. Berindei, I. Bland, W. Chittleborough, D. Krauskopf, K. Săndulescu, M.

Smith, B. Morphology, Archaeology and Topography. Porolissum, the northest Roman city of Dacia, that derives its name from the Dacian settlement of Porolisson, was built mainly on Pomet hill, close to Moigrad village.

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It comprised the large amphiteatrum castrense, access gates, temples of different Gods, an aerial aqueduct coming from Meseş, a large necropolis, therms, a series of other public and private buildings and auxiliary fortresses.

The Roman road ski last minute suisse anti aging went along the north-western border of Dacia Porolissensis, that started at Bologa and ended at Porolissum, was of great importance in the area, being used even in the 19 th century.

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Keywords: Geosite, Roman roads, cartography, archaeological topography, morphology, territorial characteristics, construction. The Roman settlement of Porolissum is to be found on the teritorry of villages of Moigrad commune of MirşidBrebi, Viile Jacului, Jac commune of Creaca and of suburban settlement of Ortelec falling in the administration of Zalău municipalityfollowing the cremă înșelăciune riduri contact between Meseş Mountains and Almaş-Agrij Depression.

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From the point of view of petrography, the morpho-tectonic contact separates the magma rocks of Pomet mCitera and Corniştea m — Moigrad Tectonic aspects are defined by Parameseş Fault, which outlines to the west the contact with the tectonic basin of Şimleu, while the Fault of Moigrad, defines the eastern limit, separating the area from the Transylvanian Basin by Agrij and Almaş depressions.

The valley of Ortelec overlies on a graben area, called the Ser anti-îmbătrânire 7 codificare Gate Poarta Meseşeanăwhich defines the northern limit of the Meseş mountains, while the valleys of Pomet, Jac and Lunca Brazilor, represent the hydrographic limit, bordering the Roman settlement of Porolissum. The wide opening of Agrij Depression favours the presence of climatic characteristics which are specific to high hills and plateaus.

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They define a complex topoclimate in the geographical porolissensis area, with a slight local influence on the regime of climatic elements, as a result of the sheltered position given by the presence of Meseş Mountains a slight föehn effect appears. The altitudes in the interfluvial area exceed mthat being more specifically the case of Moigrad — Pomăt BisericuŃa Peak, m — Citera interfluve, Moigrad knoll having an absolute altitude of9 m.

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The average altitude of Agrij Depression is m. Terraces have appropriate features in terms of tectonic and neo-tectonic stability, hydro-geological resources, favourableness in designing extended rural settlements and of clear opening to the neighbouring areas, allowing them to be monitored and observed, thus recommending themselves as appropriate to developing communal activities urbanistic, agriculture, tourism and transport.

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Most of the buildings of Porolissum settlement, both civil and military, are concentrated in the interfluvial area of Pomet, that covers an area of over ha. The quasi-horizontal levelling surfaces of Pomet or Citera favoured the settlement of large buildings, such as the amphitheatre, the Roman custom, and ski last minute suisse anti aging for about 25 soldiers and civilians.

The geosite and geoarchaeological site of Porolissum — set-up and structure.

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It developed primarily along the Roman road that crossed the settlement and passed by the praetoria gate of the large Pomet camp. The southern limit of the city was set around the Roman customs area, m south-west of the camp, and it extended eastwards on a distance of about m.

A series of buildings 25 I. Also, the terrace found southwards from porta decumana of Pomet camp, where civilian buildings and the amphitheatre were found, was intensely humanized.

Important archaeological material was thus brought to light, including inscriptions, coins, fibulae, tegular material etc.

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However, it never reached the status of colonia. Among the leaders of the city, besides the ordo decurionum, citizens gathering also played an important role, mentioned as respublica municipii Septimii Porolissensium on epigraphs.

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The direction of the Roman road inside the military complex of Porolissum is SE- NW going round the military camp on Pomat Hill on its north-western side. This road appears also on the military map since it can be easily used. The large camp of Porolissum is set at about m south of Moigrad village and at about m from the isolated houses of Tamba family, in the area where a range of hills separates the archaeological territory from the village on its north and north-western side, the range including the Hill of Porcar, Comorii Hill, Ferice Hill, Ursoaia Hill and Goronişte Hill.

At the point where it crosses the earth mount, the Roman road leaves the archaeological complex through the northern entrance set between Ferice and Ursoaia Hills.

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