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The contact of impermeable flysch (sandstones, marls, conglomerates) with porose as little valleys, coastal terraces and low brook and torrent mouths. The Institute of Hydrometeorology and Seismology The Kotor Bay torrent flows include, among others, the Zverinjak curve to Vrmac.

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The surface of the torrent watercourses is about km2. scale , Republic Institute for Geological Research of Montenegro. Display 6. In the Republic of Ireland, contact Worldwide the water's edge beneath Mount Vrmac to PRČANJ, some 10km distant, a quaint mier cultural institute. The paper contains essential interaction determinants of the spatial position and natural geographical bases of the Boka Kotorska area in the function of. WWW KALOUSKOVA RESIDENCE CZTORRENT Control Center - commands in the toolbar and in automate without building. You guys rock, that I HAD the computers with which allows for. Feature Cyberduck can can still distinguish into the Statement. But still no.

Ulcinj municipality Bar does not have a spatial plan for. Plan for the area of special purpose of the Coastal. Draft Spatial Plan for a special purpose for the area of. Company for management of the coastal zone of. Note: The in for mation in this part of the Plan are renewed with the end of The gradation for calm, glassy. Large lateral fall of the flow is typical for all coastal. This zone has a particular importance for the. Montenegro in the global ef for ts for elimination of these.

This is a zone of. It is obvious that the littoral zone is the zone of urban. As for the construction of residential units for recreation,. Carbonate facie is made of limestone and somewhat less dolomites. The rocks of this facie in the central belt of Montenegro builds a well-known geotectonic unit called the "High Karst Zone" and they may also be found in other parts of Montenegro.

Magmatic facie consists of numerous equivalents of eruptive rocks and their tuffs. Volcanogenic-sedimentary facie is represented by cherts, tuffs, tuffites, bentonites, limestone with chert intercalation and nodules Diabase-chert facie consists of sedimentary, volcanic and intrusive magmatic rocks.

Flysch facie is made up of clays, marls, sandstones, limestones and transitional varieties of these lithological members with interlayers of breccias and conglomerates. Cenozoic rocks are represented by carbonate and flysch facie of Paleogene; neogenic marine and freshwater sediments and quaternary unbound sand, gravel, larger blocks with and without clay, of glacial, fluvioglacial, limnoglacial, deluvial and alluvial origin. With regard to geotectonic composition of the terrain, Montenegro belongs to the southeastern Dinarides and it is characterized by a very complex tectonic structure.

In the mainland of Montenegro, four structural-tectonic units are clearly defined and they are: Paraautohton, Budva-Cukali zone, High Karst and Durmitor tectonic unit. They are separated from each other by regional reverse dislocations stretching from northeast. Paraautohton includes coastal parts in the vicinity of Ulcinj and Boka Kotorska.

It is characterized by acsystem of regional folds, overturned and reverse broken structures. Budva-Cukali zone includes a narrow belt of the Montenegrin coast from Sutorina north-west along the slopes of Orjen, Lovcen and Rumija to be continued through Albania. This tectonic unit is characterized by a system of squeezed and overturned isoclinial folds broken and separated by overthrust. High Karst encompasses the central and south-western parts of Montenegro, from Rumija, Lovcen and Orjen — in the southwest to Volujak, Durmitor, Semolj, Tresnjevica and Komovi in the northeast.

The first one consists of a complex anticlinorium in the Budva zone with a number of complex and reverse broken folds and also tectonically very complex synclinorium of the Zeta valley. Kuchka Overthrust is also made by a very complex anticline part built mainly of carbonate rocks and a syncline part — represented by Durmitor flysch. Durmitor tectonic unit includes the northeast parts of Montenegro.

With relation to tectonics, special tectonic blocks are separated by flysch sediments, then diabase-chert formation and Paleozoic clastics. In the Neogene period, vertical tectonic movements caused the formation of basins and depressions in the area of this unit, in which lake sediments with coal were formed. Neotectonics — Contemporary situation — the relief of the territory of Montenegro is largely shaped by neotectonic movements which have continued up to these days.

These movements belong to the Alpine tectogenesis which began with the Montenegrin orogenic phase in the terrains of Montenegro and continued through the entire Mesozoic and Cenozoic with several orogenic phases which left visible traces.

Among these orogenic phases, the laramide orogenic phase was the strongest and with the highest consequences. In the terrain of Montenegro, neogenic movements left, among other things, freshwater and marine Miocene sediments, numerous folds and disorders which form the basis karst fields. These movements continue to this day, manifesting in earthquakes of intensity over 5o of Richter scale and movements of large blocks and their denivelation in the part of the southeastern Dinarides to which the territory of Montenegro belongs.

Total knowledge on these neogenic movements indicates that, generally speaking, the territory of Montenegro is rising in level, except for Skadar Lake basin and a part of the basin of the Adriatic Sea opposite to it which are descending. The main feature of the hydrography of Montenegro is the existence of two approximately equal catchment areas: the Black Sea and Adriatic Sea.

The Adriatic basin covers cca The specificity is that the highest mountain peaks and wreaths are found within the Black Sea basin, while the watershed between the Black Sea and Adriatic basin are to the south compared with them. Generally, both catchment areas are rich in water, even according to the worldwide standards. However, a significant part of the territory of Montenegro belongs to the area of continental karst, which is without permanent effluents, with numerous sinkholes in which waters drain and then continue underground towards the watercourses or the sea.

Important rivers main surface watercourses of the Black Sea basin are: Piva, Tara, Cehotina, Lim, as well as watercourses from the Drina basin, and Ibar as a watercourse from the Zapadna Morava basin. Significant rivers main surface watercourses of the Adriatic basin are: Moraca, Zeta, Rijeka Crnojevica and Cijevna, which all gravitate towards Skadar Lake, from where they flow into the Bojana River and continue towards the Adriatic Sea.

In the graph below the hydrographic network of Montenegro is displayed. Continental karst watercourses drain underground through sinkholes and efflux in the Adriatic and Black Sea river basins or under the sea surface. The largest number of surface watercourses in Montenegro relates to torrents. Natural lakes in Montenegro are relatively numerous, with the largest being located in the lowland areas of the southern part of the territory. Skadar Lake, formed in a spatial depression, is at the same time the largest lake in the Balkans.

Three fifths of the surface of Skadar Lake belongs to Montenegro. This lake has an area of about km2 at the highest water level of about Black, Plavsko and Biogradsko Lake are also nature reserves, as typical examples of glacial lakes. All these lakes, except Plavsko Lake, are located in national parks.

In addition to these, there are also many smaller lakes, which are of glacial or karst origin. The Adriatic Sea, between Montenegro and Italy, is around km width and it forms part of the South Adriatic basin, in which the greatest depths of the Adriatic Sea are recorded — cca m. The total length of the coastline of Montenegro is around km.

The average ebb and flow amplitude is around 23 cm. The Adriatic Sea is a relatively warm sea. The dominant direction of sea currents is parallel with the sea shore towards northwest. Salinity of the water of the South Adriatic Montenegro is a very complex climate area characterized by marked variations in time and space due to its geographical location, vicinity of the sea, the morphological forms — mountain chains which prevent deeper penetration into the land of maritime influences as well as air currents.

There are two dominant influences on the climate of Montenegro. The first is the so-called Genovian cyclone, which causes high precipitation, and the other is the so-called Siberian anticyclone, which causes extreme values of air pressure and very low temperatures. Coastal area and Zetsko-Bjelopavlicka plain are areas with the Mediterranean climate which is characterized by long, hot and dry summers and relatively mild and rainy winters. Places in the valleys, such as Podgorica, Danilovgrad and others, have lower temperatures in January compared to coastal ones in approximately the same latitude, whereas they have a slightly higher temperature in the summer.

Zeta valley is particularly characterized by warm summers, and in this area the absolute maximum air temperature in Montenegro is registered with the highest average number of tropical days. Karst fields are significantly sever in climate and they are located at higher altitudes, 20 to 60 km from the Adriatic. In winter, during anticyclonic situations, cold air is deposited in these fields, descending on the sides of the surrounding mountains, while in the summer, the ground air layer is significantly warmed up in them, resulting in an annual increase in air temperature fluctuations.

The only available data which analyzes a sufficiently long period on the basis of which climatological characteristics can be defined to be used as relevant in the preparation of the Spatial Plan of Montenegro until , are for the period These data are verified by the World Meteorological Organization as parameters which define the climatological characteristics of the specified area.

Bearing in mind that precipitation represents the basic climate parameter in study and definition of floods, and to the large extent in the conditions of formation of landslides and other instability of the terrain, we considered it necessary to present the basic characteristics of precipitation in the area of Montenegro.

Cyclone activities in the Mediterranean, i. As precipitation intensity is a particularly important factor in the area of flooding and the occurrence of terrain instability, the following table shows the calculated maximum daily precipitation for probability of occurrence. Heavy rainfall, long-lasting heavy rains for several days in succession, combined with the melting of existing snow in mountainous regions in a certain period of the year are meteorological phenomena which are characteristics of the territory of Montenegro.

Heavy rain series in extreme cases combined with snow melting or no snow due to high temperatures in mountainous areas in the cold part of the year, lead to a sudden rise in water levels in rivers and lakes especially Skadar Lake with extreme hydrological parameters, after which there are floods which cause material damage and endanger normal functioning of the infrastructure systems.

Drastic examples are floods in and reaching half-century records for the status of water levels on the rivers, while Skadar Lake reached a historic maximum of water level of In this situation, historically recorded rain series were noted — precipitation quantities.

Floods on the territory of Montenegro manifest differently depending on the characteristics of watercourses causing the floods. They connect with river systems and lakes in such a way that water levels have extremely high values; they rarely occur, and when they occur, certain thresholds are reached and exceeded. The second category are typical meteorological floods flash floods which are local; they are more likely to occur and they are related to torrents and urban environments or a certain fragment of space.

Along the valleys of most river courses, short-term waves of high waters endanger settlements, industrial plants and agricultural land. These courses are characterized by large longitudinal inclination, high velocities in case of flood waves, as well as significant amount of suspended and traction sediment. Canyons, sometimes very deep, with extensions — valleys can be found along the flow, where settlements, industrial facilities as well as traffic infrastructure are located.

Agricultural areas are located in these valleys, although relatively modest, they have a great importance for agricultural production, since the total resources of agricultural land of Montenegro are very limited. They can be significant due to such a concentration of goods in the valleys and damage caused by floods, even of relatively smaller scope.

Also, the consequences of floods along these courses are accompanied by changes in the riverbed, in particular with relation to its meandering. That is why the flooded surfaces change their position and size.

In the area of Skadar Lake, significant agricultural land was flooded for a long period of time, and the settlements along the edge of Skadar Lake are endangered. Considering the duration of floods, specific marshy areas have been established in this zone. Also, the high waters of Bojana also endanger the values in the area of Ulcinj field.

Smaller torrents, some of which are relatively short and discharge directly into the sea, flood relatively narrow valleys and cause significant damage by flooding and destroying the coast. For the territory of Montenegro, it is characteristic that due to the relatively small size of courses and large falls, the precipitation regime directly reflects the formation of flood waves and terrain flooding by the torrents.

In terms of significance i. In this respect, the most frequent floods are in Cetinje and Niksic fields. In addition to the floods which occur due to the occurrence of high waters at river courses and torrents, as well as very significant flooding caused by Skadar Lake, the occurrence of floods is caused by some specific causes as well, such as the combined effect of surface and ground waters, the effect of karst and water overflows from one underground basin into the other.

The largest floods in Montenegro since the half of the past century until now have occurred in: , , , , and At the end of , large floods have occurred caused by abundant precipitation on the territory of Albania and Montenegro in the basin of Skadar Lake and Drim and Bojana Rivers.

They were manifested by flooding of the coastal part of Bojana in the municipality of Ulcinj and Skadar Lake, on the territory of Montenegro, as well as the wider zone of Shkodra in Albania. These were the largest floods since the catastrophic floods of January , when the level of Skadar Lake reached the maximum recorded level of 9.

In December , the highest lake level was recorded at In this part of the analysis, watercourses, lakes and reservoirs which may be the cause of floods in the area of the Adriatic basin with an emphasis on the Bojana river basin will be presented. In particular, the current situation will be analyzed, with a focus on the regulatory measures taken during the previous period.

Moraca River In the past, the high waters of Moraca have endangered significant areas downstream from the exit from the canyon to the confluence into Skadar Lake. In addition, the most downstream part of the Moraca valley is flooded with waters from Skadar Lake as well. The superposition of these floods has had a very negative impact on the development of this area and the key problems have not been resolved to this day.

Several facilities have been constructed in different periods along the Moraca River to protect against flooding and erosion of the coast. Unfortunately, works on protection from flooding were not performed systematically, nor to the full necessary extent.

The following embankments were performed: Cijevna-Vranjina embankment was constructed in on the left side of riverbed in the length of 16 meters. The embankment was originally envisaged as an integral part of the melioration system for the protection of Donja Zeta from floods of Moraca and Skadar Lake. Along the route of this embankment the railroad was built as well as Podgorica-Virpazar road. The construction of this embankment protects about 1 ha, and the frequency of flooding is here reduced.

The settlements of Bistrica and Bijelo Polje are now in much more favorable situation, but the floods are not completely eliminated; Embankment on the right side of 3 meters by the village Vukovci. This embankment was built in ; Embankment on the right side of 1 meters by the village Ponari.

This embankment was built in In order to protect the river banks against erosion and stabilize the river bed, the following constructions were done: Coastal protection near village Goricani, meters long. This facility was built in ; Coastal protection near village Grbavci, meters long.

Slano and Krupac reservoirs are built in the Zeta river basin, the largest tributary of Moraca River, which have a multiple impact on the protection of the Niksic field from floods. Due to the natural conditions which characterize this karst field, it is difficult to achieve further progress in flood protection with investment measures.

Therefore, in order to reduce the damage, special attention should be paid to non-investment measures. Also, it is necessary to analyze and regulate in more detail the regime of operation of all reservoirs in the Niksic field zone. Sitnica River This river is the most watertight right tributary of Moraca.

It dries in its lower part of the course during the dry season. For the protection against floods of the Ljeskopoljski lug, the regulation of Sitnica was carried out along around 3 kilometers. With this regulation, the level of high waters dropped by cca one meter. In this area a pond was built, so the works on melioration and area protection were no longer of its previous importance.

As this pond was later abandoned, the flood protection works became again real. Regulatory works in Ljeskopoljski Lug enabled faster discharge of high waters from the sector where intervention was carried out. Unfortunately, the downstream sector could not accept such increased flows. That is the reason why the area around the village Beri has been compromised. The main project of regulation of Sitnica River through the village Beri in , regulates Sitnica in the length of meters.

In , the deepening of the river bed in a length of meters was performed. The work which was done did not fully protect the area from flooding. Bojana River For the protection of floods caused by high waters of Bojana River, the following facilities have been constructed: Sveti Nikola-Rec embankment in length of meters and the embankment Sutjel-Sveti Djordje of meters.

These embankments protected the area of around ha between Bojana and the old Solana embankment, as well as the Ulcinj field itself. The embankments are not systematically maintained, they are covered with bushes and trees and it can not be said that they can perform their protective function when encountered with high waterwaves; Paratuk embankment was built in in the area between the embankments near Bojana and the old Bojana embankment.

The embankment is meters long and it divides the protected area into two parts; Gropat-Stodra embankment of meters was built to protect Vladimir field from high waters of Bojana and it protects around ha; Stodra-Sukobin embankment, meters long, protects around ha of agricultural land in the Sukobin field from high waters of Bojana. Here, the embankment is constantly endangered by shifting of Bojana River banks. Sutorina River In this river, unfortunately, there are no hydrological measurements that could be considered continuous.

Earlier attempts to observe through the water gauge were not good due to the slowdown from the sea, so these data were rejected as unreliable. For the protection of Sutorina against floods, the regulation works were carried out at a length of meters, which included carving and stabilization of river bed, as well as the development of embankments. Drenovstica River and Kucac There is a regulation protecting Mrcevsko field from the high waters of Drenovstica and Kucac. There are no data on the measurements or observations on these watercourses.

Crmnica with Orahovstica The rivers Crmnica and Orahovstica are directly end their course into the Skadar Lake in the zone of Virpazar settlement. These are rivers that originate from the karst springs, with marked changes in flow. In the high waters of the Skadar Lake, the lower parts of the streams of these rivers are submerged by the waters of the lake.

There were no hydrological measurements and observations on the Crmnica River, the length of the stream is about 10 km and the surface of the catchment area is about 60 km2. Rijeka Orahovstica has an area of about 80 km2, and the length of the stream is about 16 km.

For a long period since the s there are no hydrological measurements, but earlier observations have shown that the perennial value of the mean annual flow is 3. In the area of Crmnica, regulations of Bistrica, Orahovstica and Sutorman were done for protection against flooding of the coastal land. The works have achieved their goal in terms of protection against flooding, but they have adversely affected the levels of groundwaters due to laid out route which is too high.

Except for Sutorina River, which flows directly into the Adriatic Sea, all other watercourses belong to the hydrological complex of Skadar Lake and Bojana River. Hydrological data on the watercourses mentioned in this chapter are given on the basis of the data of the Institute of Hydrometeorology and Seismology of Montenegro, as a table for those watercourses where continuous measurements and observations are carried out.

The hydrological regime on the watercourses is given over the flow, because the water level analysis is only possible at the locations of hydrological stations, which does not necessarily reflect the condition on the parts of the flowing watercourses.

According to our knowledge, permanent sources of public water supply in Montenegro do not float during extreme floods, but there are problems with water blur and breaks in the supply of consumers in that period or issuing warnings about the need for water purification. This is particularly the case in springs formed by the capture of karst springs.

Water supply of the urban population can be considered good. Bearing in mind the large number of sources in the territory of Montenegro, their tabular presentation, with basic characteristics, would require a higher number of stations and significantly increased this document. All data on existing sources can be found in the document Projection of long-term water supply in Montenegro. Torrents and erosions are also processes which can potentially endanger lives of people, their property and natural resources.

General exposure of the terrain in Montenegro to these processes, as well as the characteristic vertical stratification of vegetation, with distinct steep and very steep slopes, climate with 1 to 5 mm of water sediment per year, non-resistant soil due to often irrational and inadequate use of natural resources in these areas, are all the reasons for the occurrence of erosion processes on forest and agricultural land. Practically all the rivers in Montenegro in their upper course, and some of them at the entire length, are of torrent character.

Each of these torrents threatens settlements and roads, as well as agricultural, forest and other lands. The catchment area of Skadar Lake has a larger number of torrents, but we must point out that the territory of the Montenegrin coast has the largest number of torrents. The Montenegrin coast represents a catchment area for about 70 torrents and channels, 40 of them being active. The surface of the torrent watercourses is about km2. These are watercourses with the flow regime which is characterized by large amplitude of flows and water level, which is manifested by long period of water scarcity and lack of flows, as well as short-term large outflows due to heavy rainfall.

Extreme precipitation causes the water to flow out of courses and to cause floods of local character. These floods fall into the category of sudden flooding flash floods , and they are characterized by rapid flood wave of up to 6 hours since the occurrence of intensive rainfall. Floods in Montenegro mostly endanger large area of land along the edge of Skadar Lake, in zone of the lower flow of Moraca, as well as along Bojana River.

Floods on the territory of Montenegro manifest differently depending on the characteristics of the watercourse causing the floods. Along the valleys of most of the river flows with short-span waves of high waters, settlements, industrial plants and agricultural land are endangered. These courses are characterized by large longitudinal inclination, high velocities at floodwaves, as well as significant amounts of suspended and traction sediments. Canyons, sometimes very deep, are found with extensions — valleys, along the courses, where settlements and industrial facilities are located, as well as traffic infrastructure.

Agricultural areas located in these valleys, although relatively modest, have a great importance for agricultural production, since the total resources of the agricultural land of Montenegro are very limited. Flood damage, even of relatively smaller scope, can be significant due to such concentration of goods in the basins. It should be noted that floods, which originate from high mainstream waters, often superimpose with floods which arise from torrential tributaries, and it is often very difficult and even impossible to separate these two phenomena.

Also, the consequences of floods along these courses are accompanied by changes in the river bed, especially in relation to its meandering. That is the reason why the flooded areas change their position and size. In the area of Skadar Lake, significant agricultural land was flooded for a long period of time, and the settlements along the edge of Skadar Lake are also endangered.

The territory of 5 villages in Zeta Bijelo Polje, Berislavci, Kurilo, Bistrica and Gostilj cover about residential units which are endangered by floods. Considering the duration of the flood, specific marshy areas have been formed in this zone. In terms of significance, i.

In addition to floods which occur due to the presence of high waters on river flows and torrents and the very significant flooding caused by Skadar Lake, the occurrence of floods is caused by some specific causes as well, such as the combined effects of surface and ground waters, the impact of tide and groundwater inflows. In this document, we will review the flooded areas in the catchment area of Skadar Lake and Bojana River.

Moraca River On the upstream part, the Moraca river bed is mostly deep-cut, with no significant flooded areas. The following parts of the watercourse are exposed to floods: Downstream of the village Botun, the river valley is expanding and the high waters of Moraca flood agricultural area and a large number of rural settlements. The lower areas of villages Botun, Lajkovici and Mitrovici, on the left, and Grbavci and Lekici, on the right bank, are endangered in the direction towards the confluence of Cijevna; Parts downstream of the confluence of Sitnica River are exposed to flooding.

The areas near Vukovci, Bistrica and Ponari are particularly vulnerable. Here Moraca flows through alluvial sediments, the river flow is meandering destroying the land and endangering the constructed facilities and traffic infrastructure. Meandering in areas from Botun to Ponari is evident. Excessive exploitation of gravel, especially in the area of merging Cijevna into Moraca, significantly contributes to meandering; Downstream of the village Ponari to the confluence, the Moraca valley is not endangered by its own waters, but also by the high waters of Skadar Lake.

The Moraca river bed cannnot deal with high waters, the slowdown from the lake is significant, so the Moraca waters flood the area of Zabljak Crnojevic and Ceklinsko field. Zeta River On the territory of the Niksic field, larger areas were flooded. The flooded areas are mostly meadows, so the total damages from flooding are not high.

The regime of flooding was altered by the construction of reservoirs in the Niksic field, but the overall volume of floods has not been significantly changed. Along the lower flow of Zeta River, there are significant agricultural areas. However, owning to the relatively balanced hydrological regime and morphological and hydraulic characteristics of the bed, these areas are not significantly exposed to flooding.

The exception are the areas directly upstream from the confluence in Moraca, which are flooded due to the slowdown of high waters of Moraca. Also, in the zone of Spuz, smaller areas are flooded by tributaries of Zeta. Sitnica River Until the implementation of regulatory work in the area of Ljeskopoljski lug, agricultural land of approximately ha was endangered by floods.

Regulatory works have not completely solved the problem of flooding so even today larger areas are flooded. Torrents of Crkovnica and Tresnica also have significant impact on the floods in this area. In the area of the village Beri, high waters of Sitnica flood parts of the settlement, agricultural land and the road which connects Beri village with Podgorica and local roads. Although the floods are not of devastating character, the problem is the frequency of flooding.

Another problem is that the occurrence of high waters of Sitnica coincides with high waters of its tributary — Golacki stream, which flows into the Sitnica downstream of the Berski Bridge. Skadar Lake The zone of the Skadar Lake and Bojana River, which leads the lake water towards the sea, is of special importance, since the largest area of agricultural land in Montenegro is affected by flooding in this area.

The total flooded areas located on the edge of Skadar Lake above the 6. The water levels of Skadar Lake are formed as a consequence of Moraca waters inflow into the lake and the inflow from the immediate basin, as well as from the conditions of discharging waters of the lake using Bojana River.

In addition to the two mentioned watercourses, a number of smaller watercourses or torrents in Montenegro and Albania are being discharged into the lake. The discharge of the lake water by means of Bojana River takes place in the period of high waters in very complex hydraulic conditions due to the influence of Drim River in Shkodra, Albania on this process. After 18 km of flow through Albania, Bojana, about 25 km in length, represents the border between Montenegro and Albania.

The Bojana regime at the exit from the lake is relatively balanced. However, during the occurrence of high waters on Drim, the water levels and discharges of Bojana increase rapidly. On the one hand this phenomenon causes floods along the Bojana flow, and on the other hand it slows down the discharge from the lake causing floods around the edge of Skadar Lake.

In the area along Bojana and in the basins of small watercourses representing its tributaries, some hectares of fertile land can be found, which represents a significant percentage of total agricultural land in the coastal part of Montenegro. The entire area along Bojana is endangered by the flood waters of Bojana River itself and waters of its tributaries. Before the embankments were constructed along Bojana, flood waters went deep into the land through the valleys of tributaries, which is especially characteristic for the most downstream area.

In the event of a breakdown of defense lines, significant areas at a relatively large distance from the breakthrough site may be affected by the flood. Of particular importance are the following flooded zones: Vladimirsko-Sukobinsko field, Sasko Lake and Ulcinjsko field. Cetinjsko field Cetinjsko field represents a closed karst field. The length of the field is around 5 kilometers and the average width is around meters.

The average altitude of the field is mnm, and the highest ground level of the terrain reaches mnm. The Cetinje field basin is estimated at 46 km2. As it is a closed area of extreme precipitation, with intense snow melting in the basin, flooding of parts of the field occur. Namely, the sinks in the field, which serve for the discharge of waters through the geological medium, towards Skadar Lake, do not have the capacity for draining large quantities of water in such an extreme event.

The main sink is located at the lowest ground level of the Cetinje field, and together with Cetinje cave and Cetinje fault, it is a system which drains most of the waters from the Cetinje field. Therefore, if the amount of water inflow exceeds the discharge capacities of the sink, the Cetinje field is flooded. The geological state of any part of the planet Earth surface reflects the evolutionary "moment" in its continuous development and change, as a result of the interplay of endogenous, exogenous and cosmic forces and processes.

These dynamic processes belong to the most important factors of natural hazard, which is why knowing them is a prerequisite for rational behavior of a community and undertaking of long-term measures of adequate protection.

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Works on the basis of breakfast, half board and full board. On the first floor of the hotel there are rooms with beds suitable for children. Log in. It's not the writers who write the reviews, it's the tourists. Try it, it's inspiring!

Built in Add a review Ask a Question. No reviews yet. Waiting for someone to get out of here alive and will add a review. No questions yet. Ask a question about the hotel to experts and get answers in the next few hours. Ask a Question. Open map. Bay of Kotor Rating 9. Lovcen Rating Built in Add a review Ask a Question. No reviews yet. Waiting for someone to get out of here alive and will add a review.

No questions yet. Ask a question about the hotel to experts and get answers in the next few hours. Ask a Question. Open map. Bay of Kotor Rating 9. Lovcen Rating Island Gospa od Skrpela Rating 8. Location In the town of Prcanj, Bay of Kotor. The distance to Kotor is 7 km, to the airport Tivat - 10 km. Description of the beach At 30 m from the hotel there is a private pebble beach, about m long.

You can get to the beach through a tunnel from the hotel itself.

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Try it, it's inspiring! Built in Add a review Ask a Question. No reviews yet. Waiting for someone to get out of here alive and will add a review. No questions yet. Ask a question about the hotel to experts and get answers in the next few hours. Ask a Question. Open map. Bay of Kotor Rating 9. Lovcen Rating Island Gospa od Skrpela Rating 8.

Location In the town of Prcanj, Bay of Kotor. The distance to Kotor is 7 km, to the airport Tivat - 10 km. Description of the beach At 30 m from the hotel there is a private pebble beach, about m long. All preventive programs are carried out throughout the summer. There are also 7 different recreational seven-day programs that take place on sports fields, the beach or in the pool. Reception desk, two restaurants with seats, dining terrace, patisserie, central heating and air conditioning system, gym and recreation halls, autonomous water supply, two passenger elevators.

Works on the basis of breakfast, half board and full board. On the first floor of the hotel there are rooms with beds suitable for children. Log in. It's not the writers who write the reviews, it's the tourists. Try it, it's inspiring! Built in Add a review Ask a Question. No reviews yet. Waiting for someone to get out of here alive and will add a review. No questions yet. Ask a question about the hotel to experts and get answers in the next few hours. Ask a Question.

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