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59-571: Borsh borders with Fterra , Qeparo , Piqeras , Kuç, Çorraj, Kalasa, Zhulat, Tatzat, and has a population of 2,500 registered inhabitants. The region which Borshi is located was part of the Chaonia of the ancient region of Epirus . Borshi was probably fortified from antiquity and it belonged to Kemara (modern Himara ) then part of the Chaonian tribal state, one of the main ancient Greek tribes in Epirus. In

118-465: A dry summer climate , described by Köppen as Cs , is a temperate climate type that occurs in the lower mid-latitudes (normally 30 to 44 north and south latitude). Such climates typically have dry summers and wet winters, with summer conditions being hot and winter conditions typically being mild. These weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to

177-424: A 40 mm (1.6 in) level. The third letter indicates the degree of summer heat: " a " represents an average temperature in the warmest month above 22 °C (72 °F), while " b " indicates the average temperature in the warmest month below 22 °C (72 °F). There is a "c" with 3 or less months' average temperature above 10 °C (50 °F), but this climate is rare and is very isolated. Under

236-867: A Csb climate because of its location inside the Alborz mountains . Winters in this zone are rainy and can be mild to chilly. Some locales in this zone experience some amount of snowfall, while others do not. Csb climates are found in northwestern Iberian Peninsula (namely Galicia and the Norte region and west coast of Portugal ), in coastal Northern California , in the Pacific Northwest (namely western Washington , western Oregon and southern portions of Vancouver Island in British Columbia ), in central Chile , in parts of southern Australia and in sections of southwestern South Africa . A few locations close to

295-456: A Mediterranean climate are near large bodies of water, temperatures are generally moderate, with a comparatively small range of temperatures between the winter low and summer high unlike (the relatively rare) dry-summer humid continental climates (although the daily diurnal range of temperature during the summer is large due to dry and clear conditions, except along the immediate coastlines). Temperatures during winter only occasionally fall below

354-594: A century of intensive agriculture. Much of the Overberg in the southern Cape of South Africa , was once covered with renosterveld , but has likewise been largely converted to agriculture, mainly for wheat . In hillside and mountainous areas, away from the urban sprawls , ecosystems and habitats of native vegetation are more sustained and undisturbed. The fynbos vegetation in the South-western Cape in South Africa

413-426: A characteristic that was previously thought to have been the diagnostic difference between the major Tosk and Gheg divisions, whereby Tosk dialects such as Borsh's lab dialect were previously thought to have all lost nasal vowels when they split from Gheg dialects, which retained the nasality feature. Following is a list of notable people from Borsh. Fterra Fterrë ( Albanian definite form : Fterra )

472-661: A few kilometres inland. Occasionally also termed the "cool-summer Mediterranean climate", this subtype of the Mediterranean climate ( Csb ) is less common and experience warm (but not hot) and dry summers, with no average monthly temperatures above 22 °C (72 °F) during its warmest month and as usual an average in the coldest month between 18 and −3 °C (64 and 27 °F) or, in some applications, between 18 and 0 °C (64 and 32 °F). Also, at least four months must average above 10 °C (50 °F). Cool ocean currents, upwelling and higher latitudes are often

531-544: A mean temperature below 0 °C (32 °F) (or −3 °C [27 °F]), depending on the isotherm used). Regions in the Americas with this climate are influenced by the dry-summer trend (though briefly) that extends considerably poleward along the west coast, as well as the moderating influences of high altitude and relative proximity to the Pacific Ocean. These conditions maintain an unusually narrow temperature range through

590-540: A season earlier than at the Dead Sea . In the Holy Land no rain at all falls in summer but early rains may come in autumn. The majority of the regions with Mediterranean climates have relatively mild winters and very warm summers. However, winter and summer temperatures can vary greatly between different regions with a Mediterranean climate. For instance, in the case of winters, Funchal experiences mild to warm temperatures in

649-447: A warm Mediterranean climate, with an average temperature of 25 degrees Celsius during the summer and 10-12 degrees Celsius during the winter. Borsh is a popular tourist destination for its beaches, beautiful nature, and its connections to the region's traditional and folk culture. Borsh experiences a hot-summer mediterranean climate ( Köppen Csa ). Precipitation in Borsh mainly falls in

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708-597: A yearly cycle in which abiotic (environmental) controls of stream populations and community structure dominate during floods, biotic components (e.g. competition and predation) controls become increasingly important as the flood discharge declines, and environmental controls regain dominance as environmental conditions become very harsh (i.e. hot and dry); as a result, these communities are well suited to recover from droughts , floods , and fires . Aquatic organisms in these regions show distinct long-term patterns in their structure and function, and are also highly sensitive to

767-515: Is a village in the former commune of Lukovë , Vlorë County , southern Albania . At the 2015 local government reform it became part of the municipality Himarë . It is located in a side valley of the Albanian Riviera , within the region of Kurvelesh and 10 km northeast of Borsh . The village is inhabited by Muslim Albanians . Fterrë is located 200 to 250 m above sea level on the western slope of Mt Lajthi (1418 m). The highest peak of

826-493: Is also important in the rural areas of Borsh, with animals such as goats, sheep, and cows. Overall, the economy of Borsh is small and developing, but tourism and the agricultural sector may offer growth opportunities in the future. Borsh has gained popularity due to its beach, which is the largest beach in the Ionian sea (7 km). The Lab dialect spoken in Borsh was reported by Albanian linguist M.Totoni to possess nasal vowels ,

885-424: Is closely associated with Mediterranean climate zones, as are unique freshwater communities, though vegetation native to the Mediterranean climate zone can also be found in the approximate nearby climate zones, which usually tend to be the humid subtropical , oceanic and/or semi-arid zones, depending on the region and location. Particularly distinctive of the climate are sclerophyll shrublands, called maquis in

944-559: Is famed for its high floral diversity , and includes such plant types as members of the Restionaceae , Ericas (Heaths) and Proteas . Representatives of the Proteaceae also grow in Australia, such as Banksias . The palette of California native plants is also renowned for its species and cultivar diversity. This subtype of the Mediterranean climate ( Csa ) is the most common form of

1003-406: Is higher, steppe climates tend to prevail, but still follow the basic pattern of the Mediterranean climates. Irregularity of the rainfall, which can vary considerably from year to year, accentuates the droughts of the Mediterranean climate. Rain does not fall evenly, nor does the rain arrive at the same time or within the same intervals. In Gibraltar , for instance, rain starts falling nearly half

1062-637: Is situated in a mountainous area, with coastal beaches and crystal-clear waters. The village of Borsh is located on a coastal stretch of about 7 km and is surrounded by hills with heights of around 900 meters above sea level. There are many beautiful natural areas in the Borsh region, such as the Llogara National Park, the Bënça River Gorge, the Borsh River, and the Borsh Castle area. This area has

1121-498: Is these fortifications that visitors can view by taking the half-hour walk up to the 'castle rock', the limestone mount clearly visible above the old village. During Ali Pasha's reign, there were 700 houses at Borsh, and below the castle mount you can see a ruined mosque of Hajji Bendo and a madrese (a Muslim theological school), both of which were damaged in Ali Pasha's wars but survived, only to be destroyed in fighting after 1912 when

1180-586: The Greco-Italian War . In 1942 the first council of the National Liberation Movement in the village and its volunteer platoon were founded under Hiqmet Çallo. In total during World War II six volunteer soldiers from Fterrë were killed and forty houses damaged and destroyed. Notes ; Sources ; Mediterranean climate A Mediterranean climate ( / ˌ m ɛ d ɪ t ə ˈ r eɪ n i ən / MED -ih-tə- RAY -nee-ən ), also called

1239-575: The Hellenistic period Borshi was a northwestern-most stronghold of the fortification system of Chaonia after Himara. The Chaonian fortification in Borsh of which Phoenice served as centre controlled a crucial road that connected Chaonia and southern Illyria . The castle remained in use in Roman times and was refortified by the Emperor Justinian in the sixth century. Nothing is known of the settlement in

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1298-568: The Kingdom of Greece . The villagers, who had fled the vicinity of Vlorë, rebuilt the village in 1916 when the Greek army retreated from Albania. In autumn 1916 the village's school was rebuilt and Selim Gjonika became its first teacher. In the Vlora War in 1920 the band of Fterra took part under the leadership of Xhafer Shehu. In World War II part of the village was destroyed by Italian artillery fire during

1357-595: The Köppen climate classification , "hot dry-summer" climates (classified as Csa ) and "cool dry-summer" climates (classified as Csb ) are often referred to as just "Mediterranean". Under the Köppen climate system, the first letter indicates the climate group (in this case temperate climates). Temperate climates or " C " zones average temperature above 0 °C (32 °F) (or −3 °C (27 °F)), but below 18 °C (64 °F), in their coolest months. The second letter indicates

1416-710: The garrigue or maquis in the European Mediterranean Basin, the chaparral in California, the fynbos in South Africa , the mallee in Australia, and the matorral in Chile. Areas with this climate are also where the so-called "Mediterranean trinity" of major agricultural crops have traditionally been successfully grown ( wheat , grapes and olives ). As a result, these regions are notable for their high-quality wines, grapeseed/olive oils, and bread products. Under

1475-415: The subtropical ridge migrates towards the equator and leaves the area, making rainfall much more likely. As a result, areas with this climate receive almost all of their precipitation during their winter and spring seasons, and may go anywhere from four to six months during the summer and early fall without having any significant precipitation . In the lower latitudes, precipitation usually decreases in both

1534-592: The Andes in Northern Ecuador , Peru , Colombia , and Western Venezuela . The cold-summer subtype of the Mediterranean climate ( Csc ) is rare and predominantly found at scattered high-altitude locations along the west coasts of North and South America having a similar climate. This type is characterized by cool, dry summers, with less than four months with a mean temperature at or above 10 °C (50 °F), as well as with cool, wet winters, with no winter month having

1593-644: The Byzantine era, until it is mentioned as Sopotos in 1258 when it was part of the Despotate of Epirus that grew out of the failing Byzantine empire. Borsh then went through a period of considerable turmoil, changing hands several times between the Despotate of Epirus and Norman crusades invaders before being taken by the Turks in 1431. Fifty years later it was captured by Albanians led by Skanderbeg's son Gjon Kastrioti II , but

1652-399: The Köppen classification, dry-summer climates ( Csa , Csb ) usually occur on the western sides of continents. Csb zones in the Köppen system include areas normally not associated with Mediterranean climates but with Oceanic climates, such as much of the Pacific Northwest , much of southern Chile , parts of west-central Argentina , and parts of New Zealand . Additional highland areas in

1711-662: The Mediterranean Basin, chaparral in California, matorral in Chile, fynbos in South Africa, and mallee and kwongan shrublands in Australia. Mediterranean vegetation shows a number of adaptations to drought , grazing , and frequent fire regimes. The small sclerophyllous leaves that characterize many of the perennial shrubs of this biome, help conserve water and prevent nutrient loss. The soils generally are of low fertility , and many plants have mutualistic relationships with nitrogen-fixing bacteria . Aquatic communities in Mediterranean climate regions are adapted to

1770-506: The Mediterranean climate typically experience hot, sometimes very hot and dry summers. Winters can be mild, cool or chilly, and some cities in this region receive somewhat regular snowfall (e.g. Kermanshah ), while others do not receive any (e.g. Casablanca ). Csa climates are mainly found around the Mediterranean Sea , southern Australia, southwestern South Africa , sections of Central Asia , northern sections of Iran and Iraq ,

1829-448: The Mediterranean climate, therefore it is also known as a "typical Mediterranean climate". As stated earlier, regions with this form of a Mediterranean climate experience average monthly temperatures in excess of 22.0 °C (71.6 °F) during its warmest month and an average in the coldest month between 18 and −3 °C (64 and 27 °F) or, in some applications, between 18 and 0 °C (64 and 32 °F). Regions with this form of

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1888-507: The Pacific portions of the United States and Chile, extreme west areas of Argentina, around Cape Town in South Africa, parts of Southwest and South Australia , and parts of Central Asia . They tend to be found in proximity (both poleward and near the coast) of desert and semi-arid climates , and equatorward of oceanic climates . Mediterranean climate zones are typically located along

1947-471: The Turks left the region. Between 1912 and 1914, serious inter-ethnic conflict took place between Greeks and Albanians, and significant portion of the old village was destroyed, however some buildings remain in fine condition. Modern Borsh was built after that, but became seriously depopulated, firstly due to malaria , and following severe reprisal killings by Germans in World War II . However, depopulation

2006-431: The average annual precipitation must not exceed 900 mm (35 in), as well as satisfying Köppen's precipitation requirements. [Chile] has four months of winter, no more, and in them, except when there is a quarter moon, when it rains one or two days, all the other days have such a beautiful sunshine that is not necessary to resort to fire. The summer is so temperate, with delicious airs, that man can go all day under

2065-434: The cold current has a stabilizing effect on the surrounding air, further reducing the chances for rain, but often causing thick layers of marine fog that usually evaporates by mid-day. Similar to desert climates, in many Mediterranean climates there is a strong diurnal character to daily temperatures in the warm summer months due to strong solar heating during the day from sunlight and rapid cooling at night. In winter,

2124-557: The freezing point and snow is generally seldom seen. Summer temperatures can be cool to very hot, depending on the distance from a large body of water, elevation, and latitude, among other factors. Strong winds from inland desert regions can sometimes boost summer temperatures up, quickly increasing the risk of wildfires . Notable exceptions to the usual proximity from bodies of water, thus featuring extremely high summer temperatures and cooler winters, include south-eastern Turkey and northern Iraq ( Urfa , Erbil ), surrounded by hot deserts to

2183-673: The interior of northern California west of the Sierra Nevada , along the Wasatch Front in Utah , and inland areas of southern Oregon west of the Cascade Mountains . Southern California's coasts also experience hot summers due to the shielding effect of the Channel Islands . However, unshielded areas of that coastline can have warm-summer Mediterranean climates with hot-summer areas just

2242-432: The lowland areas, temperatures which can sometimes prohibit the growth of typical cold-sensitive Mediterranean plants. Some Spanish authors opt to use the term 'continental Mediterranean climate' ( Clima Mediterráneo Continentalizado ) for some regions with lower temperatures in winter than the coastal areas, but Köppen's Cs zones show no distinction as long as winter temperature means stay above freezing. Additionally,

2301-491: The ocean, altitude and geographical location. The dry summer climate is found throughout the warmer middle latitudes , affecting almost exclusively the western portions of continents in relative proximity to the coast. The climate type's name is in reference to the coastal regions of the Mediterranean Sea , which mostly share this type of climate, but it can also be found in the Atlantic portions of Iberia and Northwest Africa,

2360-470: The place as Ifteran with 24 extended families and in later years is listed with 45 extended families. During the early Ottoman era it was part of the nahiye of Sopot, while in the 16th century it was incorporated into the kaza of Kurvelesh . In the Albanian Revolt of 1910 the çetë (military unit) from Fterrë was led by Lazo Kofina. In 1914 the village was destroyed during the advance of army of

2419-562: The precipitation pattern (" s " represents dry summers). Köppen has defined a dry summer month as a month with less than 30 mm (1.2 in) of precipitation and as a month within the high-sun months of April to September, in the case of the Northern Hemisphere and October to March, in the case of the Southern Hemisphere, and it also must contain exactly or less than one-third that of the wettest winter month. Some, however, use

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2478-519: The reason for this cooler type of Mediterranean climate. The other main reason for this cooler type is the altitude . For instance, Menton on the French coast has a Csa climate while Castellar, Alpes-Maritimes , the adjacent town just north of Menton, with an altitude between 100 and 1,382 m (328 and 4,534 ft), has a Csb climate instead. The village of Siah Bisheh in Northern Iran also has

2537-636: The recent effects of climate change . The native vegetation of Mediterranean climate lands must be adapted to survive long, hot summer droughts in summer and prolonged wet periods in winter. Mediterranean vegetation examples include the following: Many native vegetations in Mediterranean climate area valleys have been cleared for agriculture and farming. In places such as the Sacramento Valley and Oxnard Plain in California , draining marshes and estuaries combined with supplemental irrigation has led to

2596-419: The south and mountains to the north. Those places routinely experience summer daily means of over 30 °C (86 °F) and daily highs above 40 °C (104 °F), while receiving enough rainfall in winter not to fall into arid or semi-arid classifications. As in every climatologic domain, the highland locations of the Mediterranean domain can present cooler temperatures in the summer and winter than

2655-542: The south coast of England such as Weymouth and Portland just scrape into this climate classification due to very low rainfall in July. A trend towards slightly drier summers during the 1971–2000 climate average period, meant that this classification previously extended slightly further to include a few other weather stations in southern England, such as Bognor Regis and Teignmouth . Rarer instances of this climate can be found in relatively small and isolated high altitude areas of

2714-722: The subtropics also meet Cs requirements, though they, too, are not normally associated with Mediterranean climates. The same goes for a number of oceanic islands such as Madeira , the Juan Fernández Islands , the western part of the Canary Islands , and the eastern part of the Azores . Under Trewartha 's modified Köppen climate classification, the two major requirements for a Cs climate are revised. Under Trewartha's system, at least eight months must have average temperatures of 10 °C (50 °F) or higher ( subtropical ), and

2773-476: The summer, Borsh is a popular tourist destination, especially for its beautiful beaches and rich natural environment. Tourism is the main source of income for the town and offers many business opportunities for hoteliers, restaurants, and other tourism-related businesses. In addition to tourism, Borsh has an economy based on livestock farming and agriculture. Crops such as olives, oranges, lemons, grapes, peppers, and other food plants are cultivated. Livestock farming

2832-537: The sun. Poleward extension and expansion of the subtropical anticyclone over the oceans bring subsiding air to the region in summer, with clear skies and high temperatures. When the anticyclone moves Equator-ward in winter, it is replaced by traveling, frontal cyclones with their attendant precipitation. During summer, regions of the Mediterranean climate are strongly influenced by the subtropical ridge which keeps atmospheric conditions very dry with minimal cloud coverage. In some areas, such as coastal California ,

2891-457: The temperature and rainfall pattern for a Csa or even a Csb climate can exist as a microclimate in some high-altitude locations adjacent to a rare tropical As ( tropical savanna climate with dry summers, typically in a rainshadow region, as in Hawaii). These have a favourable climate, with mild wet winters and fairly warm, dry summers. The Mediterranean forests, woodlands, and scrub biome

2950-674: The tropics, on Haleakalā Summit in Hawaii. In South America, Csc regions can be found along the Andes in Chile and Argentina. The town of Balmaceda, Chile is one of the few towns confirmed to have this climate. Small areas with a Csc climate can be found at high elevations in Corsica . In Norway, the small fishing village of Røstlandet , in Røst Municipality , above the Arctic Circle has

3009-573: The village's area is that Gjeshnikoshi (1478 m) and the lowest that of Leka (315 m). There are also numerous karst springs and six caves. A road from Borsh to Vlorë passes through the village. Fterrë was first mentioned in 1431, in the Sûreti defter-i sancak-i Arvanid ( defter of the Albanian Sanjak ). At that time, it consisted of twelve – affluent – families. In 1583, the Ottoman Defter mentioned

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3068-452: The western coasts of landmasses, between roughly 30 and 45 degrees north or south of the equator . The main cause of Mediterranean, or dry summer, climate is the subtropical ridge , which extends towards the pole of the hemisphere in question during the summer and migrates towards the equator during the winter. This is due to the seasonal poleward-equatorward variations of temperatures. The resulting vegetation of Mediterranean climates are

3127-527: The winter and summer due to higher evapotranspiration . Toward the polar latitudes, total moisture usually increases; for instance, the Mediterranean climate in Southern Europe has more rain. The rainfall also tends to be more evenly distributed throughout the year in Southern Europe, while in places such as Southern California , the summer is nearly or completely dry. In places where evapotranspiration

3186-410: The winter, with frost and snowfall almost unknown, whereas Tashkent has cold winters with annual frosts and snowfall; or, to consider summer, Seville experiences rather high temperatures in that season. In contrast, San Francisco has cool summers with daily highs around 21 °C (70 °F) due to the continuous upwelling of cold subsurface waters along the coast. Because most regions with

3245-402: The winter, with little rain in the summer months. Borsh experiences mild winters and hot, dry summers. The average annual temperature is 13.3 °C or 55.9 °F, with 1598 mm or 62.9 inches of precipitation per year. The village is very stable and growing in prosperity thanks to tourism and olive oil production. The economy of Borsh is mainly based on tourism, livestock farming, and agriculture. In

3304-543: The year for climate zones at such distances from coasts. In North America, areas with Csc climate can be found in the Olympic , Cascade , Klamath , and Sierra Nevada ranges in Washington, Oregon and California. These locations are found at high altitude nearby lower altitude regions characterized by a warm-summer Mediterranean climate ( Csb ) or hot-summer Mediterranean climate ( Csa ). A rare instance of this climate occurs in

3363-503: Was a turbulent economic time and due to Orthodox revolts and conflicts with Orthodox powers such as the Russian Empire , Ottoman governors at times applied pressures including drastic tax raises on the local Christian population as well as other pressures caused towns to convert. Borsh converted in 1744 and followed it up by raiding nearby Piqeras , which remained Christian. The fortress was renovated again by Ali Pasha Tepelena , and it

3422-471: Was balanced by an influx of refugees from Vlora, fleeing into partisan territory from the city which was heavily contested until late in the war.In 1914 the greek military massacred albanians in Borsh Borsh is a coastal village in southern Albania , in the district of Vlore. The geographic coordinates of the village are 40.0667° N, 19.9389° E. Borsh is located about 25 km south of the city of Vlore and

3481-519: Was retaken by the Turks eleven years later and heavily refortified. On June 10, 1570 the castle of Sopot was taken by James Celsi, Proveditor of the Venetian navy, who left after leaving in charge the commander of Nauplion , Emmanuel Mormoris . This also caused part of the nearby Himariotes to submit to Venetian rule. The next year the Ottoman army recaptured it and took Mormori as a prisoner. The 18th century

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