Description: The Emerald Lake (Szmaragdowe Lake, Jezioro Szmaragdowe) in Szczecin is an artificial water body formed in a former limestone quarry. From the late 19th century until 1925, high-quality chalk and limestone were extracted here, mainly for cement production. Mining ended abruptly after a catastrophic collapse, when underground workings filled with water, flooding the quarry and creating the present lake. The water’s striking emerald-green color results from dissolved calcium carbonate and light reflection. The site is framed by steep quarry walls, reaching up to 20–30 meters, which emphasize its dramatic landscape. The area is also prone to landslides and rockfalls, a reminder of its geological instability. Today, the lake is set within the forested hills of the Szczecin Landscape Park 'Puszcza Bukowa', offering both natural beauty and a glimpse into the region’s industrial and geological past.
Property: Public.
Accessibility: Szmaragdowe Lake lies in the eastern part of Szczecin, within the Bukowa Forest. It is easily accessible by foot, bicycle, or public transport, with marked trails leading to viewpoints and recreational areas around the lake.
Use limitations: Access to Szmaragdowe Lake is generally unrestricted, as it lies within a public landscape park. However, swimming and diving in the lake are prohibited. Visitors are encouraged to remain on designated trails.
Safety: Visitors to Szmaragdowe Lake should be aware of natural hazards typical of former quarry sites. Steep cliffs pose risks near the lake's edges. Safety is enhanced by maintained trails and designated viewpoints.
Interpretatives: The Ecological Education Center presents exhibitions on thebiodiversity of the Bukowa Forest, mining traditions, and the military history of the area. Along the trails, information boards provide details on natural habitats.
Infrastructure: The area around Szmaragdowe Lake is equipped with tourist infrastructure that facilitates exploration of the site. A network of marked walking trails leads to several viewpoints located on the quarry rim, offering panoramic views of the lake and surrounding forest. Stairways and paths provide access to steep slopes, improving visitor safety. The vicinity also hosts the 'Szmaragd' Ecological Education Center, which organizes events and serves as an information hub for visitors.
Protection: Szmaragdowe Lake and its surroundings form part of the Szczecin Landscape Park 'Puszcza Bukowa', a protected area under Polish nature conservation law. The site is also integrated into local heritage initiatives that emphasize both its natural and cultural values. Protective regulations aim to preserve the lake, surrounding forest, and associated geological features.
Fragility: The site's physical stability is influenced by geological and environmental processes. Quarry walls are susceptible to erosion and landslides, while vegetation encroachment gradually alters the visual character of the cliffs. Water levels may fluctuate depending on seasonal conditions, potentially affecting the lake's appearance and ecosystems.
Vulnerability: Human activity remains a potential threat to Szmaragdowe Lake. Unregulated tourism, littering, and trampling of vegetation may disturb the natural environment. Unauthorized swimming, climbing, or disturbance of quarry walls could accelerate erosion and pose safety hazards.
| Spatial type | Scale | Relevance | Name | Descriptions | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| group of surfaces | 10-100m |
✅ Abiotic ❌ Biotic ❌ Cultural |
Miocene sands and silts | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| group of surfaces | km |
✅ Abiotic ❌ Biotic ❌ Cultural |
Glacial sands and gravels | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| group of surfaces | km |
✅ Abiotic ❌ Biotic ❌ Cultural |
Glacial tills | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| group of surfaces | 10-100m |
✅ Abiotic ❌ Biotic ❌ Cultural |
Marls, limestones, and writing chalk of the Maastrichtian | Cretaceous | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Themes and processes (3)
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| group of surfaces | m |
✅ Abiotic ❌ Biotic ❌ Cultural |
Landslides | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| group of surfaces | m |
✅ Abiotic ❌ Biotic ✅ Cultural |
Spoil heaps | Mining of Maastrichtian marls for cement production | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| surface | m |
✅ Abiotic ❌ Biotic ✅ Cultural |
Inactive quarries | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| point | m |
✅ Abiotic ❌ Biotic ❌ Cultural |
Spring and landslide | Uncontrolled groundwater discharge led to the flooding of the Cretaceous marl quarry | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Themes and processes (2)
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| group of points | m |
✅ Abiotic ❌ Biotic ✅ Cultural |
Viewpoints | View towards the inactive quarry | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| group of points | m |
❌ Abiotic ❌ Biotic ✅ Cultural |
Former mining facilities | Mining of Maastrichtian marls for cement production | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| group of points | mm |
✅ Abiotic ❌ Biotic ❌ Cultural |
Erratic boulders | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| point | mm |
✅ Abiotic ❌ Biotic ✅ Cultural |
Viewpoint | View from the spoil heap towards Szczecin | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| point | mm |
✅ Abiotic ❌ Biotic ✅ Cultural |
Viewpoint | View from the morainic hill towards Szczecin | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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| line | 10-100m |
✅ Abiotic ✅ Biotic ✅ Cultural |
Trail around the lake, leading to the springs and landslides | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Themes and processes (0)No themes for this element.Biocultural components (2)
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| line | 10-100m |
✅ Abiotic ❌ Biotic ❌ Cultural |
Trail along the edge of the quarry wall and along the landslides | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Themes and processes (2)
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| Process | Feature | Description |
|---|---|---|
| Sedimentation of Miocene sands and silts | Miocene sands and silts | |
| Glacial sedimentation | Glacial sands and gravels | |
| Mining of Maastrichtian marls for cement production | Heap | |
| Landslide | Landslide niche | |
| Sedimentation of marls, limestones, and writing chalk in a shallow sea (Maastrichtian, Cretaceous) | Marls, limestones, and writing chalk of the Maastrichtian | |
| Thrusting and deformation of Cretaceous marls within a glacial raft | Glacial raft | |
| Groundwater discharge | Spring | Uncontrolled groundwater discharge led to the flooding of the Cretaceous marl quarry |
| Formation of spoil heaps resulting from Maastrichtian marl mining for cement production | Viewpoint on a spoil heap |
| Process | Is active | Time scale | Begin | End |
|---|---|---|---|---|
| Sedimentation | passive | million-year | 23 Ma, lower Miocene | 15 Ma, lower Miocene |
| Formation of landslides | active | century | 1925 | present |
| Sedimentation of glacial deposits during the Vistulian glaciation | passive | hundred thousand-year | 30 ka | 15 ka |
| Formation of spoil heaps during mining activity | passive | century | second half of the 19th century | 1945 |
| Sedimentation of Maastrichtian marls (Cretaceous) | passive | million-year | 72 Ma | 66 Ma |
| Glacitectonic deformations during the Vistulian and earlier glaciations | passive | hundred thousand-year | 400 ka | 15 ka |
| Mining of Cretaceous marls in quarries | passive | century | second half of the 19th century | 1945 |
| Groundwater discharge | active | century | 1925 | present |
| Component | Description | Time scale | Begin | End |
|---|---|---|---|---|
| Heaps | Spoil heaps, today used partly as viewpoints | century | second half of the 19th century | 1945 |
| Inactive quarries | Quarries of Maastrichtian marls for cement production | century | second half of the 19th century | 1945 |
| Former mining facilities | century | second half of the 19th century | 1945 | |
| Viewpoint overlooking the center of Szczecin | year | 1945 | present | |
| View of the Bukowa Forest | Plant communities of the Bukowa Forest | century | 1945 | present |