Regions. Regions (Climate-generational-soil areas). Due to the very heterogeneous natural conditions, the Republic of Macedonia is divided into eight climate-vegetation and soil areas, which represent also vertical zones, and differ in its climate, climazonal vegetation and soils. These areas, along with their altitude and surface, are: I. Sub-Mediterranean (modified Mediterranean) area, 50-500 m; Ⅱ. Continental-sub-Mediterranean area, up to 600 m, along with and area 897,000 ha or 34.9%; Ⅲ. hot continental area, 600-900 m, 704,000 or 27.4%; Ⅳ. cold continental area, 900-1.100 m, 342.000 ha or 13.3%; C. Podgular-continental and mountainous area, 1,100-1,300 m, 250,000 ha or 9.7%; Ⅵ. Gorico-Continental and mountainous area, 1,300-1,650 m, 269,000 ha or 10.4%; Ⅶ. Subalpic mountainous area, 1,650- 2,250 m, 97,000 ha or 3.8%; and ⅷ. Alpine mountainous area, over 2,250 m, 13,000 ha or 0.5%. A map of the prevalence of these areas in the Republic of Macedonia was developed. Sub-Mediterranean (modified Mediterranean) area. It extends to the Vardar Valley in the southeastern part of the Republic of Macedonia, at a height of 50 to 500 m, where the strongest impact of the Mediterranean climate is the strongest impact. It is our warmest region, with an average house at a temperature of 14.2 C and 600 to 700 m per year rainfall. Climosonal vegetation in this area is ASS TSCCIFERIFERI-PERIPUNTOMEALITIALIS (Community of the NRRAR). All substrates, except for pure limestones, dominated by the prominent cinematic forest soils, and the small areas of the limestones occur. Continental-Subdederal Area. It is our largest area (up to 600 m above the sea), which extends in Central Macedonia, where the climate regionalization of the Republic of Macedonia is combined the impact of the East Conocinental and the modified climate. It is our crucial area (average annual rainfall 500 mm), with an average annual temperature of 12.7 S. It is the area of Blagon and White Gaber (Ass. On small areas of limestones, redlets are educated, and on lesucid carbonate sediments, Chernozems, in the driest part of the area. Hot continental area. It extends to large surfaces, mostly in the values of Western Macedonia and far less in Eastern Macedonia. It occurs in the zone of 600 to 900 m above the sea, which means the lower terrain of the mountains. It is a mean annual temperature of O 11 C and with an annual amount of precipitation of 700 mm, as well as with the climazonal vegetation of the oak Pluskor and CER (Ass. In this area, prominent and lusic cinematic soils dominate. Disstructive and eurotic leisiled soils are on very small surfaces and planos. Cold continental area. This area is higher than our valleys, and therefore it extends in the mountain terrain, in the height zone of 900 to 1,100 m, with zonal vegetation of oak Gorun (Ass. Orno-Ljuertum Petrahe) and with Domarder on the average annual quantities of precipitation in MM by height (Peroid 1961 & 1990) Map of the middle-year-old air temperature in C0 in the Republic of Macedonia of the cold continental climate (medium annual temperature 9 C and annual rainfall 800 to 850 mm). In this area, the oak vegetation and soils with textual profile is completed. Here the zone of brown forest soils begins, depending on the substrate, they belong to the eutritional or diligent substrate. Rare are the humorous and lusal opinion. Podgular-continental-mountainous area. In this area, which occurs at an altitude of 1100 to 1300 m, the impact of the mountainicular climate begins, which is combined with the continental (medium-year-old Temoemes 8 C and precipitation 900 mm MM CSO) and begins the beech vegetation (preparation of Bukova Forest ASS FRETUCE Heteropche-Fagetum). Dominate District brown forest soils, and rarely and humbly. Gorddomic continental-mountainous area. It extends in the zone at an altitude of 1,300 to 1,650 m, with strong dominance of the mountain above the continental climate (medium-sized agents at a temperature 6.4 C and 1,000 to 1,100 mm precipitation per year). It is a zone of the Goric Bucolicate Forest (Asses. Czilamanto Grandiflorae – Fagetum). There are less often and beech-ewell, pure elf, prayer and fresh forests. It is the zone of domination of humble (and directional) brown forest soils. In the higher part of the zone, brunipodolated brown forest soils occur and the brown defaults begin to occur. Subalpic mountainous area. It occurs in the zone of 1,650 to 2,250 m above the sea, with the dominance of the mountain climate (medium GOO breathing temperature 3.5 p 1050 mm precipitation per year). It is a region of a number of subalpic acidophile forest communities (mainly coniferous): Subalpian beech forests (ASS Fagetum Subalpinum Sacar-to-Pinditum), forests of the molika (Assembles Pinetum Pinetum Subasis. Alpinum), forests of Smrish (ACC. Pizzout Subalpinum Szirdzoom), Shu-my fight Krivulj (Ass. Pizza Mugchi Macydonitsum), Subalpian Ealel Shests. Most of the forests have been destroyed and converted into secondary high mountain pastures in Verspani (ACC. The dominant soil type is the brown reputation soil, but the previous stages of evolution of evolution appear: fades, lynic and bruniped linear rankers, district, humble and brunipodolated brown forest soils. Organominine and organogenic literally-dolomite mulberry occurs on limestone. More subcovers of Umbris Rounders are educated under the overseas. Alpine mountainous area. It extends at an altitude of over 2,250 m and occupies much smaller surfaces compared to other areas. It features the most pronounced influence on the mountain climate, with negative medium-socket air temperatures of -0.4 C and forests after the form of cultivation of the Republic of Macedonia 790 mm annual amount of precipitation. It is a zone of high-mountain grass communities. There is no forest communities in it. Grass communities and soils depend on a lot of substrate (limestone or silicate walls). More communities from the Alliance of the Alloy of Vidrah, and on the silicate substrate, several communities from the Alliance Omeryae. All soils are the type of A-R or A-C profile and there are no soils with (c) or BT-horizon. Depending on the evolution of plant communities on the limestone substrate, they are educated: organogen (with or without felous horizon o) and rarely in the lower part and the subalpine zone Organic-mineral limestone-dolomite mulberry. On the silicate substrate there are several subdivisions of the Umbrield Roner: Liquit (with or without felous horizon o), haplil and brunipulated. Lit.: F. Filipovski, characteristics of climate-vegetation-soil zones (regions) in the Republic of Macedonia, MANU, Skopje, 1996. F. F.
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