Location Administratively, Szopienice-Burowiec is one of the auxiliary units (No. 15) of the city of
Katowice, located in the
Silesian Voivodeship. It occupies the north-eastern part of the city, approximately 8 km from the city centre. Szopienice-Burowiec borders several neighbouring districts of Katowice, as well as the cities of
Sosnowiec and
Mysłowice. To the north, it adjoins
Dąbrówka Mała to the east, Mysłowice (districts: and ); to the south,
Janów-Nikiszowiec; and to the west,
Zawodzie. The boundaries of Szopienice-Burowiec are defined as follows: • Northern boundary: follows from the exit at the height of the Dąbrówka Mała Centrum Handlowe bus stop (southern platform) to the city border with Sosnowiec on the
Brynica river; continues along the route of the former to the intersection with
Warszawa Zachodnia-Katowice line; then runs northeast to the Brynica river and follows the river to the tripoint of the borders of Katowice, Mysłowice, and Sosnowiec at the height of . • Eastern boundary: follows the border between Katowice and Mysłowice through the middle of Hubertus III pond to the intersection of and Stawiska streets; then continues south to Krakowska Street. • Southern boundary: follows Krakowska Street and the southern carriageway of to the junction with , Krakowska, and streets. • Western boundary: follows Obrońców Westerplatte Street to the Rawa river; then runs upstream along the river, encircles the Gigablok Sewage Treatment Plant, and continues through industrial and service areas toward Walenty Roździeński Avenue. In physico-geographical division of Poland, Szopienice-Burowiec lies within the
mesoregion (341.13), which constitutes the southern portion of the
Silesian Upland and belongs to the subprovince. Historically, the district is situated in the eastern part of
Upper Silesia.
Geology Szopienice-Burowiec lies within the , a region characterized by a
horst structure. At the transition from the
Devonian to the
Carboniferous period, the Paleozoic basement of the
Silesian Upland underwent subsidence, forming a basin that was subsequently filled during the Carboniferous with
conglomerates,
sandstones, and clay shales containing
bituminous coal deposits. Carboniferous formations crop out at the surface in several parts of Szopienice-Burowiec. Larger exposures include areas along the border with Janów-Nikiszowiec, the Stawiska area, the site of the former Szopienice Non-Ferrous Metals Smelter at K. Woźniak Street, north of , and the zone between and the Morawa pond. These outcrops primarily consist of the Rudzki Beds, which comprise sandstones, grey shales, and conglomerates with coal seams. The area between J. Korczak Street and the Morawa pond also includes the Saddle Beds (bituminous coal, sandstones, grey shales, and conglomerates) as well as, together with the zone beneath the Borki pond, the Grodziec Beds (grey shales with sandstones and bituminous coal). During the
Pleistocene, the area was covered by
ice sheets, most likely on two occasions: during the
Mindel glaciation and the
Riss glaciation. Deposits from the Riss glaciation, primarily
till, are preserved mainly in the western part of Katowice. In the eastern part, including Szopienice-Burowiec, these tills were partly
denudatiated during periglacial conditions, resulting in extensive surfaces of
diluvial clays intermixed with fluvioglacial sands and gravels. Glacial and fluvioglacial sands and gravels cover substantial portions of Szopienice-Burowiec, while the Burowiec, Wilhelmina, and Bagno areas are underlain by
eluvium derived from till. Holocene deposits in Szopienice-Burowiec are distributed mainly along the valleys of the
Rawa and
Brynica rivers. within the
mesoregion (341.13). The western and southern parts of Szopienice-Burowiec belong to the Siemianowice Upland, which slopes gently downward toward the lower-lying zone along the Rawa river. This lower area represents a segment of the Rawa Depression. Toward the south, along the boundary with Janów-Nikiszowiec, the terrain transitions into the Murcki Plateau. Both the Siemianowice Upland sector and the Rawa Valley have undergone significant anthropogenic modification as a result of long-term settlement, as well as the extraction and processing of mineral resources, particularly
bituminous coal. Additional human-induced landforms include road and railway embankments. Almost the entire district has been leveled through human activity, with only limited areas – mainly the elevations around the Evangelical cemetery, the water tower on J. Korczak Street, and the terrains between Burowiec and Borki – retaining largely natural relief. The Szopienice-Borki pond area constitutes a mining-induced subsidence basin.
Soils In Szopienice-Burowiec, soils have been profoundly altered by intensive anthropogenic activity, resulting in the predominance of
anthropogenic soils in which human influence represents the main soil-forming factor. In the northern part of the district, in the Burowiec area, soils have developed on
tills. The southern part is underlain by sandy loams. Extensive urban development and industrial operations have led to significant degradation and devastation of these soils across large areas. Moreover, the soils are contaminated with
heavy metals, including in wooded zones. Soils of bonitation class IV predominate throughout much of the district. Areas of higher-quality class III soils are present in Burowiec, specifically in the terrains situated between Szronowa Street (along its full length) and .
Climate and topoclimate The climate of Szopienice-Burowiec is broadly consistent with that of Katowice as a whole, though it is locally modified by topoclimatic factors. The region experiences a
temperate climate, with oceanic air masses prevailing over continental ones. Western winds are dominant (accounting for approximately 60% of occurrences), followed by lesser contributions from eastern and southern directions. Between 1961 and 2005, the average annual air temperature recorded at the nearby station was 8.1 °C. The
urban heat island effect further influences local temperatures. July is the warmest month, with an average of 17.8 °C, while January is the coldest, averaging –2.2 °C. Annual
sunshine duration averaged 1,474 hours between 1966 and 2005, and mean annual precipitation totaled 713.8 mm between 1951 and 2005. Topoclimatic conditions within the district vary according to the degree of afforestation, urbanization, and proximity to river valleys. The higher-lying zone extending from Burowiec to the housing estate near W. Anders Street falls within the topoclimate of built-up, elevated valleys, where conditions range from average to favorable. In densely built-up areas with extensive impervious surfaces, daytime heating is more rapid and nocturnal heat loss occurs more quickly due to lower humidity. specifically in the
drainage basins of three rivers: the
Brynica (draining the north-western part of Burowiec, including the Borki area and the Szopienice-Borki ponds), the
Rawa (covering the western and central parts of the district), and the (encompassing the and areas). The Brynica river flows toward the border between Katowice and
Mysłowice. In Szopienice-Burowiec, it forms part of the north-eastern boundary of the city over a portion of its course. The
Rawa river flows from west to east through the district. It passes between the tram depot and the Gigablok Sewage Treatment Plant, then runs parallel to Obrońców Westerplatte Street, crosses it, and continues eastward parallel to and the Hubertus ponds toward the city boundary. Within the district, the Rawa receives wastewater at 15 discharge points, predominantly municipal. A small eastern portion of the district (parts of Wilhelmina and the Stawiska area) belongs to the drainage basin, although the Bolina river itself does not flow directly through Szopienice-Burowiec. The ponds filled with water in the 1950s and 1960s following the cessation of sand extraction and the discontinuation of dewatering in the excavations. The district is situated within Groundwater Body No. 111. A small northern fragment of the area also overlies part of Major Groundwater Basin No. 329 Bytom, which contains fissure-karst-porous waters in
Triassic carbonate formations.
Nature and environmental protection vegetation on the site of the former Szopienice Non-Ferrous Metals Smelter vegetation on Borki pond Szopienice-Burowiec ranks among the most heavily transformed districts in Katowice, largely as a result of long-term
heavy industrial activity. This has led to widespread soil contamination (particularly with heavy metals), water pollution, and substantial changes to local plant and animal communities.
Barren vegetation areas occupy more than 55 ha, while unmanaged green areas cover nearly 110 ha. No forested areas are present within the district. In the functional-spatial structure, unmanaged green spaces and zones of declining agricultural use extend across the northern part of the district, from to the Hubertus ponds. The most severely degraded and transformed areas – predominantly wastelands and post-industrial sites – correspond to the former Szopienice Non-Ferrous Metals Smelter, located in the south-eastern and western parts of the district. Szopienice-Burowiec contains a site of notable natural value: the Szopienice-Borki nature and landscape complex. Established on 29 November 1999, this 157-ha protected area developed in the site of former sand pits that gradually filled with water. The ponds support more than a dozen fish species, including
roach,
rudd,
perch,
pike,
bream,
crucian carp, and
sunbleak.
Reed beds along the shores provide habitat for waterfowl and wading birds such as
mute swan,
mallard,
pochard,
tufted duck, and
coot. The complex hosts the largest breeding colony of
black-headed gulls in the
Metropolis GZM, along with other protected bird species. Among mammals,
muskrats inhabit the ponds, while
hedgehogs,
weasels,
shrews, and various rodents occur in the surrounding areas.
Willow-
poplar communities dominate the pond margins. In addition to its ecological role, the site serves as a popular recreational space for local residents, cyclists, anglers, and horse riders. In terms of potential natural vegetation, most of Szopienice-Burowiec – outside of river valleys – belongs to a zone of unknown
successional tendency due to severe environmental disturbance. Along the valleys of the Rawa and Brynica rivers, the potential natural vegetation consists of
alder and
ash-alder
riparian forests on periodically waterlogged soils. On devastated and heavily transformed terrains,
synanthropic vegetation predominates, including
ruderal perennials such as
mugwort and
burdock. Trampled sites support mat-like communities dominated by
broadleaf plantain and
ryegrass. The fauna includes species typical of human settlements, such as
house sparrow,
rock dove,
jackdaw,
magpie,
blackbird,
rook, and
starling. In allotment gardens, cemeteries, and managed urban green areas, common bird species include
tits,
jays, starlings,
chaffinches, and blackbirds. The district contains one
natural monument: a common
horse chestnut tree standing 15 meters tall with a
diameter at breast height of 218 cm, located on Ogród Dworcowy Square. It was designated a natural monument on 23 June 2017. Managed green spaces within the urbanized parts of Szopienice-Burowiec cover more than 28 ha in total. • (at the intersection of J. Haller and streets); • Square (between and Obrońców Westerplatte streets); • Square (in the area of Obrońców Westerplatte Street); • Square (in the area of Morawa and Bednarska streets); • Square (between and L. Zamenhof streets); • (near the ); •
Janusz Sidło Square (between and the railway); • (on Wiosny Ludów Street).
Allotment gardens in Szopienice-Burowiec are administered under the Katowice Delegation of the Silesian District Board of the . The main gardens are: == History ==