The Lower Silesian Voivodeship (Polish: Województwo dolnośląskie) is
located in south-western Poland and borders on the Greater Poland and
Lubusz Voivodeships to the north, the Opole Voivodeship to the east, the
Czech Republic to the south and Germany to the west. Lower Silesia is
one of the most culturally rich regions in Europe, where different
cultures have mixed over the centuries. Lower Silesia is characterized
by the Silesian lowlands on the Oder in the north and by the mountains
and hills of the Sudetes in the south. The capital and largest city is
the university town of Wroclaw in the north-east of the voivodeship.
Apart from the capital, there are two other major cities, Wałbrzych and
Legnica.
In this region you will find numerous brick Gothic and
Baroque churches, fortified towers and castles and beautiful pond
landscapes. There are good water sports opportunities (kayaks, swimming,
sailing, diving) at the reservoirs, the Militsch lakes and the numerous
mountain rivers. The kayak route along the Glatzer Neisse is very
varied. Hikers and winter sports enthusiasts get their money's worth in
the Giant Mountains, which reach an altitude of over 1,600 meters in the
voivodeship area with the Sněžka. The other mountain ranges of the
Sudetes are also interesting hiking and winter sports areas. The hilly
foothills of the Sudeten, for example the Zobten Mountains, have their
own charm. In particular, the provincial capital Wroclaw offers an
interesting cultural program. With its numerous castles and palaces, the
Hirschberg valley is a unique cultural landscape in Europe.
In
the south are the Sudetes with the mountain ranges of the Giant
Mountains, the Jizera Mountains, the Heuscheu Mountains and the Glatzer
Bergland. In the north lies the valley of the Oder.
The Lower
Silesian Voivodeship was part of the Great Moravian Empire at the time.
From about 990 it belonged to Poland and from 1138 it was part of the
Polish Seniorate as a part of the Principality of Silesia. In the 14th
century almost all areas of Lower Silesia, which were further ruled by
the Silesian Piasts, came under Bohemian fiefdom and in the 16th century
to the Habsburgs. After the Silesian Wars, Lower Silesia became
Prussian.
In the area of today's Lower Silesian Voivodeship, a
significant German-speaking population settled before the First World
War, arising from the Holy Roman Empire of the German Nation and the
time as the Prussian province of Lower Silesia. After the Lower Silesian
part of the former German eastern territories was retained by the German
Reich after the First World War, this, among other things, went under
Polish administration after the Second World War as part of the westward
shift of Poland. The population historically settled there fled from the
Red Army or was expelled and replaced mainly by Poles, who in turn were
expelled from the eastern Polish territories. Today's Lower Silesian
Voivodeship was formed in 1999 from the areas of four old Voivodeships.
Polish is the official and colloquial language.
In Lower
Silesia, a mixed dialect, which developed from various East Polish
dialects, is spoken. The younger Poles speak English at the same high
level as the Germans or Austrians. German, French, Spanish and Italian
are spoken sporadically.
The name possibly comes from the prehistorically significant cult
mountain Ślęża (Latin: Silensi, German: Zobtenberg). According to other
theories, the Slavic Slensanen or the Germanic Silingen gave their name.
The name Lower Silesia is confusing at first, because the area has
higher peaks with the Sudetes than Upper Silesia with the West Beskids.
In fact, however, Lower Silesia lies downstream of the Oder from the
point of view of Upper Silesia. The name Lower Silesia is therefore
justified, even if southern Lower Silesia is significantly higher than
the Silesian Plateau in Upper Silesia.
Most of the region is made
up of historical Lower Silesia, the original capital of which was
Wroclaw. In the west, small parts of Upper Lusatia also belong to the
Lower Silesian Voivodeship. Parts of the north are in historical
Wielkopolska and the Glatzer Ländchen in the south was part of
historical Bohemia. On the other hand, parts of historical Lower Silesia
are now in the Voivodeships of Opole, Lubusz and, to a small extent,
Greater Poland, Saxony and the Czech Republic.
The voivodeship
has a share of the Milicz lakes in the north-east.
Most of the Lower
Silesian Heath is located in the north-west of the voivodeship.
The
Oder Valley, which runs through the voivodeship in the north and
north-east, makes up the majority of the Silesian Plain.
To the south
of the Oder Valley is the hilly foothills of the Sudeten Mountains,
which stretch as far as Opole.
The voivodeship shares the Sudetes in
the south, which are very popular with winter sports enthusiasts and
hikers, especially on the Sudetes Main Hiking Trail (part of the
Polish-Czech Friendship Trail in the Krkonoše Mountains). On the Polish
side of the Sudetes, there are these mountainous regions in the Lower
Silesian Voivodeship:
West Sudetes
The Giant Mountains with
its cirque lakes, waterfalls, rock formations and high moors is the
highest and most famous mountain range that is also protected in the
Giant Mountains National Park.
The Jizera Mountains with their high
moors and abandoned villages are the western extension of the Giant
Mountains.
The Bober-Katzbach Mountains adjoin the Giant Mountains in
the north-west and are surrounded by the Bober and the Katzbach.
The
Landeshuter Kamm is located north-east of the Giant Mountains and is
known for its bizarre rock formations. Its western part is also known as
the Falcon Mountains.
Central Sudeten
The bizarre
Heuscheuergebirge is located at the transition to Glatzer Ländchen and
its rugged rock labyrinths are also protected in the Heuscheuergebirge
National Park.
The Eulengebirge impresses with its blaze of color in
autumn. It is known for the World War II project Riese.
The Zobten
Mountains lie in front of the main ridge of the Sudetes to the north and
are within sight of Breslau. The historically significant Zobtenberg is
said to have given Silesia its name.
The Rabengebirge joins the
Riesengebirge in the east. Here is the beautiful baroque Grüssau
Monastery
The Waldenburger Bergland is the eastern extension of the
Rabengebirge. Here is the Fürstenstein Castle, one of the largest, most
magnificent and most beautifully situated castles in Europe.
The
Wartha Mountains are characterized by the picturesque breakthrough of
the Glatzer Neisse near Bardo.
The Eagle Mountains nat with Zieleniec
one of the most important winter sports areas of the Sudetes in Glatzer
Ländchen. The mountains are located on the Polish-Czech border.
The
Habelschwerdter Mountains are the south-eastern extension of the Eagle
Mountains. There are some nice shelters on the alpine pastures.
Eastern Sudetes
The Reichenstein Mountains are located in the border
triangle of Opole and Moravia. Gold has been mined here in the mountain
streams since the Middle Ages.
The Bielen Mountains are located in
the border triangle of Bohemia and Moravia. In Lądek-Zdrój there is
treatment and in Stronie Śląskie skiing.
The Śnieżka Mountains are
known for the Big Śnieżka Mountain, the stalactite cave at Kletno and
the waterfall at Międzygórze.
Prehistoric and Early Medieval Period (up to ~10th century)
The
area saw human settlement from prehistoric times, with evidence of rural
communities, pottery, agriculture, and animal husbandry dating back to
4000–1700 BCE. After the Migration Period (4th–7th centuries), Slavic
tribes—including the Silesian tribes (Ślężanie)—settled the lands around
the end of the first millennium. In the 9th century, the short-lived
Great Moravia (under rulers like Svatopluk I) exerted influence over
parts of the region.
Piast Poland Era (10th–14th centuries)
Around 990, Mieszko I of the Piast dynasty incorporated Silesia into the
early Polish state. His son, Bolesław I the Brave, consolidated control
and established a bishopric (initially at Smogorzów, later moved to
Wrocław in 1000), marking strong ties to the Kingdom of Poland.
After
Bolesław III Wrymouth's death in 1138 and his testament dividing Poland
among his sons, the fragmentation of Poland began. Silesia became a
duchy under Piast princes. In 1163–1172, the Duchy of Silesia split: the
western part became Lower Silesia, while the eastern part formed Upper
Silesia (Opole-Racibórz duchies).
Lower Silesia fragmented further
into numerous small Piast duchies (e.g., Wrocław, Legnica,
Świdnica-Jawor, Głogów). This period saw intensive German settlement
(Ostsiedlung / eastward migration), urban development (Magdeburg rights
in many towns), Cistercian monasteries, and cultural flourishing.
Wrocław emerged as a major center. The Mongol invasion of 1241
culminated in the Battle of Legnica, where Duke Henry II the Pious was
killed, halting further Mongol advance into Europe but devastating the
region.
Bohemian / Czech and Hungarian Interludes (14th–16th
centuries)
In 1335–1339, most Silesian duchies came under the Crown
of Bohemia (Holy Roman Empire) through treaties and feudal homage,
ending direct Polish rule over Lower Silesia. The region experienced
brief Hungarian control in the 15th–16th centuries amid Hussite wars and
Jagiellonian succession struggles.
In 1526, after the Battle of
Mohács, Bohemia (and thus Silesia) passed to the Habsburg monarchy under
Ferdinand I. Lower Silesia remained under Austrian Habsburg rule for
over two centuries, with German cultural and linguistic dominance
growing stronger in towns and lowlands.
Prussian / German Period
(1742–1945)
The decisive shift came during the Silesian Wars
(1740–1763). In the First Silesian War (1740–1742), Frederick the Great
of Prussia seized most of Silesia from Austria via the Treaty of Berlin
(1742). Only a small southern fragment (around Glatz/Kłodzko) remained
Austrian.
Lower Silesia became part of the Province of Silesia within
the Kingdom of Prussia, later the German Empire (from 1871). It
underwent intensive industrialization (textiles, mining, machinery),
Germanization policies, and infrastructure development. Wrocław
(Breslau) grew into a major German cultural and academic center. The
population was overwhelmingly German-speaking by the 19th–early 20th
centuries.
After World War I, Lower Silesia remained entirely within
Germany (unlike divided Upper Silesia, where Polish uprisings led to
partition). During the Nazi era (1933–1945), the region was part of the
Province of Lower Silesia (Niederschlesien).
Post-1945: Polish
Era and Modern Voivodeship
At the end of World War II (Potsdam
Agreement, 1945), nearly all of Lower Silesia was transferred to Poland
as compensation for eastern Polish territories lost to the Soviet Union.
The Oder-Neisse line became the new border; a small western part stayed
in East Germany.
The German population was largely expelled or fled
(1945–1947), and the area was repopulated mainly by Poles from central
Poland and—significantly—Poles repatriated from former eastern Poland
(Kresy). Wrocław and other cities were rebuilt after heavy wartime
destruction.
From 1945–1975, the area formed the Wrocław Voivodeship.
The 1975 administrative reform split it into smaller voivodeships
(Wrocław, Legnica, Wałbrzych, Jelenia Góra). The current Lower Silesian
Voivodeship was established on January 1, 1999, during Poland's major
local government reform, merging those four former voivodeships into one
large province centered on Wrocław.
Topography and Landforms
The topography of Lower Silesia is
characterized by a mix of low-lying plains in the north and central
areas, transitioning into hilly forelands and rugged mountain ranges in
the south. Much of the voivodeship lies in the Silesian Lowlands and the
Oder River Valley, where elevations are relatively modest, with the
lowest point at 69 meters (226 feet) above sea level in the Oder Valley.
In contrast, the southern border incorporates the Sudeten Foreland and
parts of the Sudetes Mountains, which form a natural barrier along the
Polish-Czech border. The highest peak is Mount Śnieżka (1,603 meters or
5,259 feet) in the Karkonosze (Giant Mountains) range, part of the
Sudetes.
Key mountain ranges and landforms include:
Karkonosze
Mountains: A prominent granite range with steep slopes, glacial cirques,
and popular ski resorts like Karpacz and Szklarska Poręba. It features
unique rock formations and is a hub for hiking and winter sports.
Table Mountains (Góry Stołowe): Known for their flat-topped plateaus and
eroded sandstone formations, creating dramatic landscapes with gorges
and labyrinths.
Owl Mountains (Góry Sowie): Historically significant
for underground structures from World War II (e.g., Project Riese),
these are lower hills with dense forests.
Sudeten Foreland: A
transitional zone of rolling hills and plateaus between the lowlands and
mountains, including areas like the Silesian-Lusatian Lowlands in the
north.
Rivers and Hydrography
The voivodeship's hydrology is
dominated by the Oder River (Odra), Poland's second-longest river, which
flows through the central and northern parts, including Wrocław. The
Oder and its tributaries form a vital drainage system, supporting
navigation, agriculture, and industry. Major tributaries within the
region include the Bóbr, Kaczawa, and Nysa Kłodzka rivers. These
waterways create fertile floodplains but also pose flood risks, as seen
in historical events like the 1997 Millennium Flood.
There are fewer
large natural lakes compared to other Polish regions, but artificial
reservoirs and ponds are common, often linked to mining or hydroelectric
projects. Mineral springs are abundant, feeding 11 spa towns—the highest
number in Poland—including Kudowa-Zdrój, Lądek-Zdrój, and
Polanica-Zdrój. These springs emerge from the region's fractured
geology, providing therapeutic waters rich in minerals.
Climate
Lower Silesia experiences a temperate climate with oceanic influences in
the lowlands and more continental traits in the mountains. Average
annual temperatures range from 8–10°C (46–50°F) in the plains to cooler
4–6°C (39–43°F) at higher elevations. Precipitation is moderate,
averaging 500–700 mm (20–28 inches) annually in the north, but increases
to 1,000–1,500 mm (39–59 inches) in the Sudetes due to orographic
effects. Winters are mild in the lowlands (0–5°C or 32–41°F) but snowy
in the mountains, supporting ski tourism. Summers are warm (18–22°C or
64–72°F), with occasional heatwaves. The region's microclimates,
especially in valleys and spas, are noted for their health benefits,
attracting visitors for climatotherapy.
Natural Resources
Lower Silesia is resource-rich, underpinning its industrial history. Key
deposits include:
Minerals and Metals: The Legnica-Głogów Copper
Basin is one of Europe's largest copper-producing areas, yielding
copper, silver, rhenium, and associated metals like nickel and cobalt.
Historical mining also extracted gold, tin, uranium, and bituminous
coal.
Energy Resources: Brown coal (lignite) reserves support power
generation, though extraction has declined due to environmental
concerns.
Building Materials: Granite from Strzegom (Poland's
"granite capital"), along with sandstone and other rocks.
Other:
Forests provide timber, and geothermal/mineral waters are harnessed for
energy and spas.
These resources have shaped the economy but also
led to environmental challenges like land subsidence from mining.
Forests, Protected Areas, and Biodiversity
The voivodeship boasts
extensive forests, including the Lower Silesian Forest—the largest
continuous forest in Poland—covering vast areas in the northwest.
Biodiversity is high, with habitats ranging from riverine wetlands to
mountain meadows. Protected areas are comprehensive:
National
Parks: Two—Karkonosze National Park (a UNESCO Biosphere Reserve, shared
with Czechia) and Table Mountains National Park—preserve unique flora,
fauna, and geological features like glacial lakes and caves (e.g.,
Bear's Cave).
Other Protections: 67 nature reserves, 20 landscape
parks (e.g., Rudawy Janowickie), over 3,100 natural monuments (including
Poland's oldest tree, a 1,200+ year-old yew in Henryków Lubański), and
numerous Natura 2000 sites.
Endangered species include lynx,
wolves, and birds like the black stork in forested areas. Efforts focus
on balancing conservation with tourism and industry.