Chełmy

Chełmy Landscape Park encompasses approximately 15,990 hectares (159.9 km²) of protected landscape in Lower Silesian Voivodeship, Poland, in the eastern part of the Kaczawskie Foothills of the Western Sudetes. ^[1] Established in 1992, the park protects volcanic hills and river valleys in the Sudeten foothills, forming part of the UNESCO Global Geopark "Land of Extinct Volcanoes." ^[2] The Bobr and associated waterways shape the park's hydrology, sustaining diverse habitats from wetlands to upland forests. As a landscape park in Poland's protected area system, it balances environmental conservation with sustainable land use while maintaining ecological corridors across the region.

Chełmy Landscape Park supports diverse wildlife across its protected habitats. The park supports populations of red deer, roe deer, wild boar, fox, and badger, with otters and beavers along the waterways. The mouflon — the park's unofficial emblem — inhabits the forested hills. ^[1] Over 130 bird species have been recorded across the park's varied habitats, including the black stork among the raptors and woodpeckers. Twenty-two bat species have been documented. ^[1] The spotted salamander is also characteristic of these Sudeten foothill forests.

The vegetation of Chełmy Landscape Park reflects the ecological conditions of the Kaczawskie Foothills. Mixed forests of pine, oak, hornbeam, and birch cover the higher ground, with species composition varying according to soil moisture, nutrient availability, and light conditions. More than half the park's surface area is covered by deciduous forest. ^[1] Alder carrs and willow thickets line the waterways, while wet meadows support marsh marigold, globeflower, and several orchid species. Meadows maintained through traditional mowing harbour diverse grassland flora. The park's total flora includes several hundred vascular plant species, reflecting the diversity of habitats from dry sandy heathlands to waterlogged fens.

The park's defining geological character is volcanic. The bedrock belongs to the Kaczawa metamorphic unit — Palaeozoic greenschist slates, greenschists, diabases, and phyllites — intruded and overlain by Neogene basalts. ^[1] Across the park territory there are basalt cones, flood basalts, and stone runs; the most notable feature is Bazaltowa Hill (367 m), whose eastern and northern slopes expose inactive basalt quarries revealing columns of columnar basalt up to 10 metres high. ^[2] Gorges and deep stream valleys, including the latitudinally oriented Jawornik River gorge, resemble rocky canyons carved through these ancient volcanic formations. The area forms the geological core of the Land of Extinct Volcanoes UNESCO Global Geopark, recognising the outstanding value of the preserved volcanic relics.

Chełmy Landscape Park experiences a temperate climate typical of the Lower Silesian Voivodeship, with distinct continental influences evident in the temperature range between summer and winter. Average annual temperatures range from 7 to 9°C, with January means of −2 to −4°C and July averages of 17–19°C. Annual precipitation falls between 500 and 650 mm, with the heaviest rainfall from June through August during convective thunderstorms. Snow cover typically persists for 40–70 days during winter. The growing season lasts approximately 200–215 days, from late March through October. The park's varied terrain creates local microclimatic differences, with forests moderating temperature extremes and maintaining higher humidity than surrounding open areas.

The region encompassing Chełmy Landscape Park has a complex human history reflecting Silesia's position at the crossroads of Central European cultures. Archaeological evidence documents settlement from prehistoric times, with significant finds from the Bronze and Iron Ages. Germanic, Slavic, and later Polish and Bohemian peoples successively inhabited the region. Medieval German colonisation brought new agricultural techniques and town foundations. The area is particularly associated with basalt quarrying, which has shaped the landscape for centuries and is evidenced by the inactive quarry exposures still visible at Bazaltowa Hill. Silesia passed through Bohemian, Habsburg, and Prussian sovereignty before becoming part of Poland after World War Two, when the German population was expelled and replaced by Polish settlers. ^[1] Traditional forestry and agriculture subsequently shaped the terrain.

Chełmy Landscape Park was established in 1992 as part of Poland's programme to protect landscapes of outstanding natural and cultural value. ^[1] The decision to create the park reflected growing recognition that the area's distinctive volcanic landscape faced increasing pressures from development, agricultural intensification, and changing land management practices. Prior to the park's establishment, several nature reserves within its boundaries had been designated to protect the most ecologically valuable sites. The landscape park designation provided a broader management framework across a larger area. Since establishment the park has become part of the Land of Extinct Volcanoes UNESCO Global Geopark, formally recognising its international geological significance. Management priorities continue to evolve in response to climate change, rural demographic shifts, and increasing recreational pressure from nearby urban centres.

Chełmy Landscape Park offers a network of marked hiking and cycling trails providing access to its most scenic and geologically interesting areas. The primary geological attraction is Bazaltowa Hill, whose exposed basalt quarry faces reveal striking columnar basalt formations — a centrepiece of the Land of Extinct Volcanoes Geopark. ^[1] Additional basalt sites at Mikołajowice and Pawłowice Wielkie within the park area also expose ancient volcanic geology. Water-based activities including canoeing and kayaking are available along the Bobr during warmer months. Wildlife observation is rewarding throughout, with dawn and dusk providing the best opportunities for encountering deer and mouflon. The park is attractive year-round, with wildflower displays in spring, warm summers, spectacular autumn foliage, and snow-covered landscapes in winter.

Chełmy Landscape Park is accessible by road from Jawor (approximately 10 km) and Złotoryja, the nearest larger towns providing services including public transport connections. Information boards at major trailheads and parking areas orient visitors to the trail network and geopark sites. Accommodation includes guesthouses and agritourism farms in villages within and surrounding the park. A private vehicle or bicycle is recommended for exploring the park thoroughly, as public transport access to the interior is limited. The park is open year-round with no entrance fee. Visitors interested in geological heritage should follow the geopark trail network linking volcanic sites throughout the Kaczawskie Foothills.

Conservation efforts in Chełmy Landscape Park focus on maintaining the ecological integrity of its core habitats — especially the volcanic landscapes and associated grassland and forest communities — while supporting sustainable land use. ^[1] The park participates in monitoring programmes for key indicator species and contributes to Natura 2000 site management. Protection of the basalt geological heritage remains a central management concern, balancing scientific access and geo-tourism with long-term preservation. European Union funding through Natura 2000 and agri-environment schemes provides important financial support for conservation activities. Climate change poses emerging challenges, with shifts in temperature and precipitation patterns potentially altering habitat distribution across the Kaczawskie Foothills.