Lower Silesia
Lower Silesia is a historical and geographical region mostly located in Poland with small portions in the Czech Republic and Germany. It is the western part of the region of Silesia. Its largest city is Wrocław.
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. In the interbellum, the Polish minority of the region was persecuted in the German-controlled part of the region.
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 remained as a part of Czechoslovakia. By 1949, almost the entire pre-war German population was expelled in accordance with the Potsdam Agreement. 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.
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 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. 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, the southern part of Lubusz Voivodeship.
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 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 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, where the tripoint with Upper Lusatia and Bohemia is located near the Smrk summit, along with the adjacent Giant Mountains ; Rudawy Janowickie ; Owl Mountains ; Stone Mountains ; Wałbrzych Mountains and the Kaczawskie Mountains with Ostrzyca, - they surround the Jelenia Góra valley, ; Ślęża Massif, massive of Orlické hory, Králický Sněžník south of Kłodzko, Rychlebské hory and Jeseníky.
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 to Złoty Stok. The southern part of the Lowland includes The Sudeten Foreland, consisting of quite low Wzgórze Strzegomskie,, Grupa Ślęży, and Wzgórza Niemczańsko-Strzelińskie. 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 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 long and over high, in comparison to neighboring lowlands, Kobyla Mountain,. 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 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 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. The average temperature of the hottest month is, and of the coldest month. The average amount of rainfall is, 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 ; 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, Jezioro Koskowickie, Jezioro Jaśkowickie and Tatarak. 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, and the largest ponds come to.
The primeval flora has been transformed significantly as a result of deforestation and cultivation. The largest forest complexes are Bory Dolnośląskie, 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. 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 are located in areas of Góra Śląska, Oborniki Śląskie, Wołowa, in the Oder River valley, and in Wzgórza Niemczańsko-Strzelińskie.