scholarly journals The mountain Cer: Potentials for tourism development

2003 ◽  
Vol 83 (2) ◽  
pp. 11-18 ◽  
Author(s):  
Mirko Grcic ◽  
Ljiljana Grcic
Keyword(s):  
Water Resources ◽  
National Park ◽  
Local Population ◽  
Good Condition ◽  
Climatic Conditions ◽  
Rural Environment ◽  
Mountain Range ◽  
The West ◽  
The North ◽  
Strategic Factors

In northwest of Serbia in the meridians directions an elongated mountain range of Cer with Iverak and Vlasic stretches itself. On the north it goes down to Macva and Posavina, on the west to Podrinje, on the east to the valley of Kolubara, on the south to the basins and valleys of Jadar and upper Kolubara, which separate it from the mountains of Valjevo and Podrinje area. Cer mountain offers extremely good condition for development of eco-tourism. The variety of relief with gorgeous see-sites, natural rarities, convenient bio-climatic conditions, significant water resources, forest complexes, medieval fortresses, cultural-historic monuments, richness of flora and fauna, preserved rural environment, traditions and customs of local population, were all neglected as strategic factors in the development of tourism. This mountain?s potentials are quite satisfactory for the needs of eco-tourism, similar to the National Park of Fruska Gora, but it has lacked an adequate ecotourist strategy so far. This study aims to pointing to the potential and possibilities of ecotourist valorization of this mountain.

Veii

Classics ◽  
2012 ◽  
Author(s):  
Helen Nagy
Keyword(s):  
Bronze Age ◽  
Urban Sprawl ◽  
National Park ◽  
Local Population ◽  
Archaeological Site ◽  
The West ◽  
The North ◽  
Ancient City ◽  
The Status ◽  
The City

The ancient city of Veii (in Italian, Veio) lies seventeen kilometers northwest of Rome and occupies a plateau of approximately 350 hectares, bounded by the rivers Valchetta (ancient Cremera) on the north and east and Piodoro on the west and south. The city had ample water and was naturally defensible, but sections of tufa walls remain, indicating that it was also fortified. Several major roads crossed the city and led toward other centers, such as Rome, Cerveteri, Tarquinia, Vulci, and Capena, via fortified gates. Impressive Etruscan-made drainage tunnels (cuniculi) flank and traverse the plateau. There is sporadic evidence of late Bronze Age settlements in the area, but it was during the Villanovan period, 9th and 8th centuries bce, that villages appeared on the plateau and on the citadel of Piazza d’Armi. A significant growth in population during the late 8th and 7th centuries bce resulted in urbanization. The strength and wealth of the city reached their peak in the 6th century bce, but by the late 5th century bce, conflicts with Rome weakened Veii, and it was finally taken after a ten-year siege in 396 bce by M. Fulvius Camillus. The triumph was sealed by the transfer of the principal cult of Juno Regina to Rome. Although Veii declined sharply after the Roman victory, some of the old popular sanctuaries continued to be frequented by the local population. In 2 bce the status of municipium was conferred on Veii by Augustus. By this time the city was falling into decay, although a small part of the Etruscan site continued to be inhabited, as evidenced by architectural fragments, sculptures (including one of Tiberius now in the Vatican Museum), and inscriptions. Once considered the richest city of the Etruscan League, Veii declined and was abandoned by the end of the 4th century ce. The plateau today is covered by fields, trees, and remnants of ancient structures. Principal among these is the archaeological site of the extra-urban Portonaccio Sanctuary. Etruscan necropolises and a few Roman tombs surround the city. Archaeological surveys continue to yield results such as the 2006 discovery of the early-7th-century Tomb of the Roaring Lions in the Grotta Gramiccia necropolis. In 1997, the Regional National Park of Veii (37,030 acres) was established to ensure the protection of the ancient city and its surroundings from the ravages of urban sprawl and illegal construction.

Managing rivers for conservation and ecotourism in the Kruger National Park

1995 ◽  
Vol 32 (5-6) ◽  
pp. 227-233 ◽  
Author(s):  
F. J. Venter ◽  
A. R. Deacon
Keyword(s):  
National Park ◽  
Good Condition ◽  
Kruger National Park ◽  
Rapid Expansion ◽  
Natural Environments ◽  
The West ◽  
The Past ◽  
Management Actions ◽  
Flow Through ◽  
Three Rivers

Six major rivers flow through the Kruger National Park (KNP). All these rivers originate outside and to the west of the KNP and are highly utilized. They are crucially important for the conservation of the unique natural environments of the KNP. The human population growth in the Lowveld during the past two decades brought with it the rapid expansion of irrigation farming, exotic afforestation and land grazed by domestic stock, as well as the establishment of large towns, mines, dams and industries. Along with these developments came overgrazing, erosion, over-utilization and pollution of rivers, as well as clearing of indigenous forests from large areas outside the borders of the KNP. Over-utilization of the rivers which ultimately flow through the KNP poses one of the most serious challenges to the KNP's management. This paper gives the background to the development in the catchments and highlights the problems which these have caused for the KNP. Management actions which have been taken as well as their results are discussed and solutions to certain problems proposed. Three rivers, namely the Letaba, Olifants and Sabie are respectively described as examples of an over-utilized river, a polluted river and a river which is still in a fairly good condition.

scholarly journals FEDERAL JETTY AND SAND DIKE AT THE ENTRANCE OF FIRE ISLAND INLET, NEW YORK

1986 ◽  
Vol 1 (20) ◽  
pp. 85
Author(s):  
Cyril Galvin ◽  
Charles J. Rooney ◽  
Gilbert K. Nersesian
Keyword(s):  
New York ◽  
Cross Sections ◽  
Good Condition ◽  
Inlet Channel ◽  
The West ◽  
North Shore ◽  
The North ◽  
Fire Island ◽  
Longshore Transport ◽  
Severe Erosion

Prior to construction at Fire Island Inlet, Fire Island was moving westward at more than 200 feet per year, the north shore of the inlet was eroding severely, and navigation in the inlet was difficult. The Federal Jetty, completed in 1941, and the sand dike, built in 1959, have halted the westward migration, eliminated the severe erosion, and partially improved navigation, with minimal maintenance or repair to the structures. There has been a large net accretion of sand east of the jetty and west of the dike, an unknown part of which is at the expense of shores to the west of the inlet. At the State Park on the south side of the inlet interior, erosion accelerated, probably because of the dike. The middle and ocean segments of the 4750-foot Federal Jetty are now (1987) in good condition, although the design implies a stability coefficient for the quarrystone jetty head at time of construction that would now be considered risky. Stability has been promoted by a stone blanket under and east of the jetty, a thick stone apron seaward of the jetty, a low (8 feet MLW) crest, and armor stone that has been partially keyed in place. Damage due to scour, common at other single-jetty inlets, is absent here because longshore transport, which easily overtops the low crest, keeps the inlet channel away from the jetty. Although the two seaward segments of the jetty remain in good condition, the inshore segment of the jetty is in poor condition, despite its apparently sheltered location. The cumulative effects of waves, possibly channeled to the site along recurved spits during storms, have damaged 1200 feet, and tidal scour has destroyed about 230 feet. The damaged segment has a design cross section which is onefifth and one-twelfth the cross sections of the jetty trunk and head.

scholarly journals Before the Celts: Cosmology, Landscape and Folklore in Neolithic Northwest Iberia

2018 ◽  
Vol 22 (1) ◽  
pp. 29-45
Author(s):  
Fabio Silva
Keyword(s):  
Iberian Peninsula ◽  
Bronze Age ◽  
Mountain Range ◽  
The West ◽  
North West ◽  
The North ◽  
Celtic Studies ◽  
The Bronze Age ◽  
Northwest Iberia

This paper applies a combined landscape and skyscape archaeology methodology to the study of megalithic passage graves in the North-west of the Iberian Peninsula, in an attempt to glimpse the cosmology of these Neolithic Iberians. The reconstructed narrative is found to be supported also by a toponym for a local mountain range and associated folklore, providing an interesting methodology that might be applied in future Celtic studies. The paper uses this data to comment on the ‘Celticization from the West’ hypothesis that posits Celticism originated in the European Atlantic façade during the Bronze Age. If this is the case, then the Megalithic phenomenon that was widespread along the Atlantic façade would have immediately preceded the first Celts.

scholarly journals The Tsakonian Dialect.—I

1913 ◽  
Vol 19 ◽  
pp. 133-173 ◽  
Author(s):  
C. A. Scutt
Keyword(s):  
East Coast ◽  
Mountain Range ◽  
The South ◽  
The West ◽  
Northern Boundary ◽  
Grazing Land ◽  
Bare Rock ◽  
The North ◽  
Cultivable Land ◽  
The Village

The area over which the Tsakonian dialect is spoken lies on the east coast of the Peloponnese between the Parnon range and the sea. Its northern boundary is roughly the torrent which, rising on Parnon above Kastánitsa, flows into the sea near Ayios Andréas, its southern the torrent which, also rising on Parnon, passes through Lenídhi to the sea. A mountain range stretches along the coast from end to end of the district, reaching its highest point (1114 metres) in Mt. Sevetíla above the village of Korakovúni. Between Tyrós and Pramateftí, the seaward slopes of this range are gentle and well covered with soil. Behind these coast hills there stretches a long highland plain, known as the Palaiókhora, which, in the north, is fairly well covered with soil, but gradually rises towards the south into a region of stony grazing land, and terminates abruptly in the heights above Lenídhi. The high hill of Oríonda rises out of the Palaiókhora to the west and forms a natural centre-point of the whole district. Behind it stretching up to the bare rock of Parnon, is rough hilly country, cut here and there by ravines and offering but rare patches of cultivable land.

W. Germany: Looking at Gotterdammerung

Worldview ◽  
1983 ◽  
Vol 26 (3) ◽  
pp. 4-6
Author(s):  
Gary L. Guertner
Keyword(s):  
National Park ◽  
Arable Land ◽  
English Channel ◽  
Open Spaces ◽  
The West ◽  
The North ◽  
The Right ◽  
National Park System ◽  
The Last Man ◽  
Radical Transformation

If a war broke out today, much of the combat in open spaces would have to take place in the West German national park system.—Paul Bracken, On Theater Warfare (The Hudson Institute, July 1, 1979)In the time of the Roman historian Tacitus (circa 55-117 A.D.), the area now watched over by NATO and Warsaw Pact armies was covered by a vast forest penetrated only by a network of narrow trails. A traveler could walk from Poland to the Rhine without even glimpsing the sun. As populations grew, forests gradually gave way to pastures and arable land. By the beginning of the twentieth century German geography—and military strategy—had undergone such radical transformation that Field Marshal von Schlieffen could see the North German Plain as a corridor for maneuvering thirty-four of the kaiser's divisions to outflank the French “if the last man on the right brushed the [English] Channel with his sleeve.”

scholarly journals Archaeology of the Gyranda region, Dawson River, central Queensland

1987 ◽  
Vol 4 ◽  
pp. 96-114 ◽  
Author(s):  
M.J. Morwood ◽  
L. Godwin
Keyword(s):  
Water Resources ◽  
Environmental Impact ◽  
Future Research ◽  
Impact Study ◽  
The South ◽  
The West ◽  
The North ◽  
Environmental Impact Study

This paper presents the results of survey and excavation in the upper Dawson area of the Central Queensland Sandstone Belt, a sandstone-dominated environment bounded by the townships of Banana in the east, Blackall in the west, Springsure in the north and Injune in the south, and which includes the Central Queensland Highlands (Walsh 1984:1). The work was undertaken as part of the environmental impact study for the Gyranda Weir commissioned by Cameron McNamara for the Queensland Water Resources Commission (Morwood 1985, 1986; Godwin 1985). However, the results of the study, and the potential of the area for future research, have a wider interest.

ASPECTS OF GEODIVERSITY IN THE WEST OF ACRE STATE - BRAZIL

2021 ◽  
Vol 2 (1) ◽  
pp. 2-10
Author(s):  
FRANK OLIVEIRA ARCOS ◽  
ELISANDRA MOREIRA DE LIRA ◽  
HILZA DOMINGOS SILVA DOS SANTOS ARCOS
Keyword(s):  
National Park ◽  
The State ◽  
Mountain Range ◽  
The West ◽  
Natural Heritage ◽  
The Andes ◽  
Andes Mountain

Geodiversity is associated with aspects of geoconservation, natural geological and hydrogeomorphological heritage in each morphoclimatic domain in Brazil. In the Amazon domain, such aspects have been forged in an environment of sedimentary origin since the Cretaceous, identified in the Rio Branco, Juruá-Mirim, Moa and Jaquirana mountains, composed predominantly of sandstones and siltstones. The Serra do Divisor National Park (PNSD) is located in the state of Acre, on the border with Peru and the Andes mountain range. The region has a natural heritage and a geological-geomorphological structure, where waterfalls, caves, valleys and high hills are found, endogenous to the site. The general objective of this article is to present elements of the Geodiversity of the Serra do Divisor National Park (PNSD) focused on the category of geotourism aiming at dissemination at regional, national and international levels.

Sierra Motherlode, Domain 2

2007 ◽  
Author(s):  
Earl B. Alexander ◽  
Roger G. Coleman ◽  
Todd Keeler-Wolfe ◽  
Susan P. Harrison
Keyword(s):  
Sierra Nevada ◽  
Western Slope ◽  
Mountain Range ◽  
Serpentine Soils ◽  
East Side ◽  
The West ◽  
Eastern Side ◽  
The North ◽  
Great Valley ◽  
Block Faulting

The Sierra Motherlode domain is in a series of allochthonous terranes, sometimes called the “Foothill Belt,” along the western edge of the north-northwest–south-southeast trending Sierra Nevada, adjacent to the Great Valley of California. It is a discontinuous belt from the southern Sierra Nevada, in Tulare and Fresno counties, to Butte County in the northern Sierra Nevada , but a branch within the belt is practically continuous from El Dorado County about 140 km north to Plumas County at the north end of the range. Cenozoic block faulting has lifted the Sierra Nevada and tilted the mountain range toward the west; therefore the highest elevations are on the east side of the range. Uplift is more pronounced in the southern than in the northern Sierra Nevada. Altitudes range from <200 m adjacent to the Great Valley to more than 4000 m along the crest of the central to southern part of the mountain range. The highest altitudes in the Sierra Motherlode domain are 1939 m (6360 feet) on Red Mountain and 1935 m (6335 feet) on Red Hill in Plumas County, and even higher on some of the granitic plutons that are within the outer limits of the serpentine domain. These plutons were intruded into the allochthonous terranes after the terranes had been accreted onto the continent. Much of the western slope of the northern Sierra Nevada is an undulating to rolling plateau. This plateau is a remnant from the early Tertiary when its surface was deeply weathered to produce lateritic serpentine soils with silica deposited in the subsoils and in fractures in the bedrock (Rice and Cleveland 1955, Rice 1957). The ancient plateau was capped by volcanic flows that produced a practically continuous cover in the northern Sierra Nevada (Durrell 1966). Uplift along the eastern side of the northern part of the Sierra Nevada to initiate its current relief commenced 4 or 5 Ma ago (Wakabayashi and Sawyer 2001). Since the range began to rise a few million years ago, the larger streams flowing across it have cut deep canyons up to about 600 m below the plateau.

scholarly journals The first evidence for Late Pleistocene hominin populations on the southern Caspian Sea coast

Antiquity ◽  
2017 ◽  
Vol 91 (355) ◽  
Author(s):  
Hamed Vahdati Nasab ◽  
Kourosh Roustaei ◽  
Mohammad Ghamari Fatideh ◽  
Fatemeh Shojaeefar ◽  
Milad Hashemi Sarvandi
Keyword(s):  
Water Resources ◽  
Late Pleistocene ◽  
Caspian Sea ◽  
Climatic Conditions ◽  
Human Settlement ◽  
The Caspian Sea ◽  
The North ◽  
Dispersal Corridors ◽  
Sea Coast ◽  
Southern Caspian Sea

The southern shore of the Caspian Sea is well known for its great potential in relation to sites of Mesolithic date (e.g. Coon 1951; Jayez & Vahdati Nasab 2016). Situated between two major geographic barriers—the Alborz Mountains to the south, and the Caspian Sea to the north—this area has been considered one of the major hominin dispersal corridors during the Pleistocene–Holocene transition (Vahdati Nasab et al. 2013). Furthermore, the relatively stable and mild climatic conditions, vast and lush temperate forests, and abundance of fauna and water resources have all made this region an attractive niche for human settlement.

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