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Lower Silesia

Historical region in Central Europe

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Through Poland, Germany and Middle Ages

The first state to have a stable hold over the territory of what will be considered Lower Silesia was the short-lived Great Moravia in the 9th century. Afterwards, in the Middle Ages, Lower Silesia was part of Piast-ruled Poland. It was one of the leading regions of Poland, and its capital Wrocław was one of the main cities of the Polish Kingdom. Lower Silesia emerged as a distinctive region during the fragmentation of Poland in 1172, when the Duchies of Opole and Racibórz, considered Upper Silesia since, were formed of the eastern part of the Duchy of Silesia, and the remaining, western part was since considered Lower Silesia. The oldest Polish writing and first Polish print were created in the region. During the Ostsiedlung, the Piast rulers invited German settlers to settle in the region, which until then had a Polish majority. As a result, the region became largely German-speaking by the end of the 15th century.

With the Treaty of Trentschin the region fell under the overlordship of the Bohemian Crown in 1335 and thus became part of the Holy Roman Empire. Large parts remained under the rule of local Polish dukes of the Piast, Jagiellonian and Sobieski dynasties, some up to the 17th and 18th century. Briefly under the suzerainty of the Kingdom of Hungary, Lower Silesia fell to the Austrian Habsburg monarchy in 1526.

In 1742, Austria ceded nearly all of Lower Silesia to the Kingdom of Prussia in the Treaty of Berlin, except for the southern part of the Duchy of Neisse. Within the Prussian kingdom, the region became part of the Province of Silesia. In 1871, the Prussian-controlled portion of Lower Silesia was integrated into the German Empire. After World War I, Lower Silesia was divided, as small parts were reintegrated with Poland and Czechoslovakia, which both regained independence.

After Germany's defeat in World War II in 1945, most of the region became once again part of Poland, while a smaller part west of the Oder-Neisse line became part of East Germany and Czech Lower Silesia (Jesenicko and Opavsko regions) remained as a part of Czechoslovakia. By 1949, almost the entire pre-war German population was expelled. Poles displaced from the former Polish lands incorporated into the USSR settled in Lower Silesia after the war, as well as Polish settlers from other parts of Poland.

The region is known for its historic architecture of various styles, including many castles and palaces, well preserved or reconstructed old towns, numerous spa towns, and historic burial sites of Polish monarchs and consorts (in Wrocław, Legnica and Trzebnica).

Geography

Lower Silesia is located mostly in the basin of the middle Oder River with its historic capital in Wrocław.

The southern border of Lower Silesia is mapped by the mountain ridge of the Western and Central Sudetes, which since the High Middle Ages formed the border between Polish Silesia and the historic Bohemian region of the present-day Czech Republic. The Bóbr and Kwisa rivers are considered being the original western border with the Lusatias, however, the Silesian Duchy of Żagań reached up to the Neisse river, including two villages (Pechern and Neudorf) on the western shore, which became Silesian in 1413.

The later Silesian Province of Prussia further comprised the adjacent lands of historic Upper Lusatia ceded by the Kingdom of Saxony after the Napoleonic Wars in 1815, its westernmost point could be found as far west as the small village of Lindenau (now belonging to the German state of Brandenburg). To the north, Lower Silesia originally stretched up to Świebodzin and Krosno Odrzańskie, which was acquired by the Margraves of Brandenburg in 1482. The Barycz river forms the border with historic Greater Poland in the northeast, the Upper Silesian lands lie to the southeast.

Administratively Polish Lower Silesia is shared between Lower Silesian Voivodeship (except for the Upper Lusatian counties of Lubań and Zgorzelec, and former Bohemian Kłodzko), the southern part of Lubusz Voivodeship (i.e. the counties of Krosno, Nowa Sól, Świebodzin, Żagań and Zielona Góra with the city of Zielona Góra, as well as western Opole Voivodeship (the counties of Brzeg, Namysłów and Nysa).

The tiny part of the former Duchy of Żagań on the western shore of the Neisse is today part of the Krauschwitz municipality in the Görlitz district of Saxony, the larger Upper Lusatian parts of Prussian Silesia ("Silesian Upper Lusatia") west of the Neisse comprised the town of Görlitz and the former district of Hoyerswerda, which today forms the northern part of the Saxon Görlitz and Bautzen districts as well as the southern part of the Oberspreewald-Lausitz district in Brandenburg. The southern part of the former Duchy of Nysa, which remained a part of Austrian Silesia after 1742, namely the Jeseník District and Heřmanovice, Mnichov and Železná, as well as parts of Vrbno pod Pradědem in the Bruntál District, today belongs to the Czech Republic.

Lower Silesia is bordered by Greater Poland and Lubusz Land in the north, Upper Silesia in the east, Moravia in the south-east, Bohemia and Kłodzko Land in the south, and Lusatia in the west.

Sudetes

The Sudetes are a geologically diverse mountain range that stretches for 280 kilometres (170 miles) from the Lusatian Highlands in the west and to the Moravian Gate in the east. They are topographically divided into Western, Central and Eastern Sudetes.

The Lower Silesian section of the Sudetes comprises the Jizera Mountains (highest peak: Wysoka Kopa, 1,126 metres or 3,694 feet), where the tripoint with Upper Lusatia and Bohemia is located near the Smrk summit, along with the adjacent Giant Mountains (highest: border peak of Sněžka Śnieżka – highest mountain of Czech Republic, 1,603 m or 5,259 ft); Rudawy Janowickie (Skalnik, 945 m or 3,100 ft); Owl Mountains (Wielka Sowa, 1,015 m or 3,330 ft); Stone Mountains (Waligóra 936 m or 3,071 ft); Wałbrzych Mountains (Borowa 853 m or 2,799 ft) and the Kaczawskie Mountains (Okole, 725 m or 2,379 ft) with Ostrzyca, 501 m or 1,644 ft - they surround the Jelenia Góra valley, 420–450 m or 1,380–1,480 ft; Ślęża Massif (Mount Ślęża 718 m or 2,356 ft), massive of Orlické hory, Králický Sněžník south of Kłodzko, Rychlebské hory and Jeseníky (English: Ashes mountains; Praděd, 1,492 m or 4,895 ft).

Silesian Lowland

The adjacent Silesian Lowland includes the Silesian Lowlands and the Silesian-Lusatian Lowlands. These two lowlands are separated with each other by Dolina Kaczawy, and from the Sudetes by a steep morphological edge located along the Sudeten Marginal Fault, extended from Bolesławiec (the Northwest) to Złoty Stok (the Southeast). The southern part of the Lowland includes The Sudeten Foreland, consisting of quite low Wzgórze Strzegomskie, 232 m or 761 ft, Grupa Ślęży (Mount Ślęża, 718 m or 2,356 ft), and Wzgórza Niemczańsko-Strzelińskie (Gromnik Mountain, 392 m or 1,286 ft). Lower hills occur also in areas of Obniżenie Sudeckie, Świdnik, and Kotlina Dzierżoniowska. The eastern part of Silesian Lowland consists of the wide Silesian Lowlands, located along banks of the Oder River. The eastern part includes also Równina Wrocławska with its surrounding lands: Równina Oleśnicka, Wysoczyzna Średzka, Równina Grodkowska and Niemodlińska. Dolina Dolnej Kaczawy (Kotlina Legnicka) separates the Silesian Lowlands from the Silesian-Lusatian Lowlands, which includes Wysoczyzna Lubińsko-Chocianowska, Dolina Szprotawy, and wide areas of Bory Dolnośląskie, located to the north from the Bolesławiec-Zgorzelec road. From the North, the lowlands are delimited by Wał Trzebnicki, consisting of hills that are 200 km (120 mi) long and over 150 m (490 ft) high, in comparison to neighboring lowlands, Kobyla Mountain, 284 m (932 ft). The range of hills includes Wzgórza Dalkowskie, Wzgórza Trzebnickie, Wzgórza Twardogórskie, and Wzgórza Ostrzeszowskie. Obniżenie Milicko-Głogowskie, with Kotlina Żmigrodzka and Milicka, is located in the northern part, within the hills.

The region of the lowlands is coated with a thick layer of glacial elements (sand, gravel, clay) that covers more diverse relief of the older ground. Generally flat and wide bottoms of the valleys are padded with river settlements. Slopes of the hills over 180–200 m (590–660 ft) are coated with fertile clays and therefore, to begin with, the Paleozoic era, they became the lands for people to settle and cultivate intensively. The later form of the economy caused almost complete deforestation of the slopes. Not only fertile grounds, but also the mild climate is conductive to the development of agriculture and market gardening. The annual average temperature of the Wrocław area is 9.5 °C (49.1 °F). The average temperature of the hottest month (July) is 19 °C (66 °F), and −0.5 °C (31.1 °F) of the coldest month (January). The average amount of rainfall is 500–620 millimetres (20–24 inches), with its maximum in July and minimum in February. The snow layer disappears after 45 days. The winds, similar to those appearing in the West side of Poland, are West and Southwest.

Sudeten rivers are characterized by changeable water rates, and high pollution resulting from large industrialization of the area. The greatest rivers are Nysa Kłodzka, which is the source of drinking water for Wrocław (the water is drawn by special channel); Stobrawa, Oława, Ślęza, Bystrzyca with its tributaries—Strzegomka and Piława; Widawa, Średzka Woda, Kaczawa with Nysa Szalona and Czarna Woda. There is also the largest right-bank tributary of the area, Barycz. The other quite large rivers, Bóbr, Kwisa, and Lusatian Neisse, flow into the Oder River beyond Lower Silesian borders. The majority of the rivers is regulated and their basins are improved, which is conductive to the proper water economy. The characteristic feature of the landscape of the lowland is the lack of lakes. The region of Legnica is the only place where a dozen or so of small lakes survived, but the majority of them is already disappearing. The largest one is Jezioro Kunickie (95 hectares or 230 acres), Jezioro Koskowickie (50 ha or 120 acres), Jezioro Jaśkowickie (24 ha or 59 acres) and Tatarak (19.5 ha or 48 acres). In contrast to the number of lakes, there are large groups of artificial ponds founded in the Barycz basin, in the Middle Ages. Their total area amounts around 80 square kilometres (31 square miles), and the largest ponds (Stary Staw, Łosiowy Staw, Staw Niezgoda, Staw Mewi Duży, and Grabownica) come to 200–300 ha (490–740 acres).

The primeval flora has been transformed significantly as a result of deforestation and cultivation. The largest forest complexes are Bory Dolnośląskie (3,150 km2 or 1,220 sq mi), Bory Stobrawskie in Stobrawa and Widawa areas, and smaller fragments of forests in Barycz and Oder River valleys. These forests are kind of multi-species deciduous forests, occurring in fertile grounds. The Oder River valley is reach in groups of mixed forests (beech, oak, hornbeam, sycamore maple, and pine). These forests, with protected status, are: Zwierzyniec, Kanigóra near Oława, Dublany, Kępa Opatowicka near Wrocław, Zabór near Przedmoście, and Lubiąż. The other forest areas are The Natural Park in Orsk, the areas of Jodłowice, Wzgórze Joanny near Milicz, and Gola near Twardogóra. Such types of forest like those which are the mainstay for wild game or nurseries, are inaccessible because of permanent fire hazard. Territories partly accessible (marked specially) are located in areas of Góra Śląska, Oborniki Śląskie, Wołowa, in the Oder River valley, and in Wzgórza Niemczańsko-Strzelińskie.

Flora

The flora of Lower Silesia is specific and different for each zone. From the bottoms to the top, plants form groups that are arranged in wide or narrow belts, called floral zones. Subsequently, these zones are divided into narrower belts, called vegetation belts.

The zone of mountain forest is divided into two belts: subalpine and lower subalpine forest. Above, there is a forestless zone divided into the subalpine belt with dwarf pine, and the alpine belt without shrubs. This vegetation is glacial; the former vegetation—from the Tertiary—was destroyed by the climate of the Ice Age. Along with glaciation from the North, some tundra plants appeared, for example downy willow (Salix lapponum) and cloudberry (Rubus chamaemorus). The flora of Lower Silesia is strongly influenced by geological and climatic history. The vegetation is formed by species deriving from various geographic regions. Particular regions are represented by:

  • Central European species: fir (Abies alba), beech (Fagus silvatica), oak (Quercus petraea), maple (Acer pseudoplatanus)
  • European Syberian species: European spindle-tree (Evonymus europaea), alder (Alnus glutinosa), wicker (Salix purpurea)
  • Boreal-Sub arctic species: cress (Cardamine pratensis), yellow marsh marigold (Caltha palustris), liverleaf (Hepatica nobilis)
  • Boreal-Arctic species: bearberry (Arctostaphylos uva-ursi), dwarf willow (Salix herbacea), black crowberry (Empetrum nigrum), Sudetic Lousewort (Pedicularis sudetica), alpine saxifrage (Micranthes nivalis), cloudberry (Rubus chamaemorus), lake quillwort (Isoëtes lacustris)
  • Alpine species: Alpine bastard toadflax (Thesium alpinium), Alpine coltsfoot (Homogyne alpina), mountain avens (Geum montanum), mountain pine (Pinus mugo)
  • Sudetic and Sudetic-Carpathian species: mossy saxifrage (Saxifraga moschata ssp. Basaltica), Sudetic lousewort (Pedicularis sudetica)

Lower subalpine forest

Lower subalpine forest (Polish: Regiel Dolny), 450–1,000 m (1,480–3,280 ft), is characterized by deciduous or mixed forest. The fragments of forests similar to natural complexes of pine-fir-beech with admixture of larch, sycamore maple and lime occur near the Szklarski waterfall, in the Jagniątkowski complex, and Chojnik Mountain. Particular species of trees have different climatic requirements. The lowest parts are covered with oak and ash, up to 500 m (1,600 ft). On the level of 500–600 m (2,000 ft) occurs pine; in the higher parts, up to 800 m (2,600 ft), there occurs European larch; and above 800 m, fir and beech.

Despite transformation of the basic tree vegetation, the same form of undergrowth survived. There occurs: daphne mezereum, red elderberry, hazel, platanthera bifolia, sweet woodruff, Herb Paris, cranberry, wood sorrel, chickweed wintergreen, Common Cow-wheat and lily of the valley. The parts over 800 m are mainly covered with grasses, purple small-reeds, cranberries, and willow gentian.

In highlighted places, on meadows, and along roads, there occurs: spotted orchid, bugleweed, yellow archangel, arnica montana, sword-leaved helleborine, rosebay willowherb, groundsel, and foxglove. Along riversides, there occurs white butterbur.

Pine forests are rich in spruces, which are permanently weakened by atmospheric factors. Frayed roots are easily infected by harmful fungus and insects. The most damaging is honey mushroom, with edible specimen, which grows in pulp, between the bark and timber, causing the death of tree. The other damaging fungus is bracket fungus, which destroys roots and trunks from the inside. The honey mushroom devastates the tree within a few months, and the bracket fungus, within a few years, as a result of mechanic changes in wood structure.

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