Geomorphological Analysis and Heritage Value of Dobreștilor–Brusturet Cave: A Significant Geomorphosite in the Bran–Dragoslavele Corridor, Romania
Abstract
1. Introduction
2. Study Area
3. Materials and Methods
4. Results
4.1. Geological Features
4.2. Geomorphology
5. Discussion
5.1. Geomorphologic Features of the Dobreștilor–Brusturet Cave
5.2. The Heritage Value of the Dobreștilor–Brusturet Cave Within the Thematic Geotourism Circuit “The Road of Gorges and Caves in the Upper Dâmbovița Basin”
5.3. Ecological and Zoospeological Value of Dobreștilor–Brusturet Cave
6. Conclusions
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Crt. No. | Geomorphosite (G—Indicative) | Structural Value | Functional Value | Restrictive attribute | Total | ||||
---|---|---|---|---|---|---|---|---|---|
VS1 | VS2 | VS3 | VF1 | VF2 | VF3 | ||||
1 | G1 Dâmbovicioarei Gorges and Brusturetului Gorges | 5.00 | 3.25 | 3.00 | 2.75 | 5.00 | 8.25 | 0.75 | 26.50 |
2 | G2 Great Gorge of Dâmbovița, Ghimbavului Gorge, and “Cheița” Gorge | 5.00 | 3.25 | 3.00 | 1.25 | 4.75 | 5.75 | 0.50 | 22.50 |
3 | G3 Orăți Valley, upper sector with Orății Gorge (“Orății Canyon”) | 4.25 | 2.50 | 2.00 | 2.50 | 4.00 | 5.75 | 1.25 | 19.75 |
4 | G4 Miresii Cave | 5.25 | 2.50 | 2.25 | 1.25 | 4.00 | 4.50 | 0.25 | 19.50 |
5 | G5 The karst hydro system “Fundățica swallet and Rudărița Valley–Uluce resurgence” | 5.50 | 1.75 | 2.00 | 1.25 | 3.50 | 5.50 | 1.50 | 18.00 |
6 | G6 Dâmbovicioara Cave | 3.00 | 1.50 | 1.75 | 1.75 | 3.25 | 7.25 | 1.25 | 17.25 |
7 | G7 Bears Cave or Colțul Surpat Cave | 3.75 | 1.75 | 2.00 | 2.00 | 3.50 | 5.25 | 1.25 | 17.00 |
8 | G8 Dobreștilor–Brusturet Cave | 4.75 | 2.00 | 2.00 | 0.75 | 3.25 | 3.75 | 1.00 | 15.50 |
9 | G9 The karst hydro system “Waterfall and Caves from Plai” | 3.50 | 1.75 | 1.50 | 0.25 | 3.25 | 5.50 | 1.25 | 14.50 |
10 | G10 Posada Cave | 4.00 | 1.50 | 1.50 | 1.25 | 2.50 | 5.00 | 1.50 | 14.25 |
11 | G11 Pleașa Cave | 4.00 | 1.50 | 0.25 | 0.25 | 1.50 | 4.50 | 0.75 | 11.25 |
Name | DOBREȘTILOR–BRUSTURET CAVE | |
---|---|---|
Call sign | G8 | |
Geographical location access (elevation 0 m) | In the calcareous marker Colții Pietrei Galbene on the left slope of the upper Brusturetului Gorge (Cheia Strâmtă), at the absolute altitude of 1160 m | |
Administrative territorial unit | Ciocanu village (Dâmbovicioara commune) | |
Types | Speleological geomorphosite | |
Extension | Linear | |
Total value | 15.50 p | |
Structural value | 8.75 p | |
Functional value | 7.75 p | |
Restrictive attribute | 1.00 p | |
Geomorphologic Value (VS1) | 4.75 p | - Genesis (SV 1a): complex speogenesis, involving four morphogenetic factors: tectono-gravitational processes (tectonic tensile diaclase, deposits, and incision forms), chemical corrosion (in some sections), torrential erosion, and chemical precipitation (gravitational dripping and prelingering forms) (1.00 p). - Dynamics (VS 1b): landforms with slow, inferred dynamics (0.50 p). - Complexity (VS 1c): Five elements of geomorphological interest—fossiliferous gallery sections with a quasi-circular cross-section (pressure flow), diversified drip forms (including anemolites), gravity seepage forms, calcitic eccentrites, stalagmitic basement floors (gours), and microgours on gently sloping surfaces of limestone sidewalls (1.00 p). - Integrity or conservation status (VS 1d): geomorphosite slightly affected (0.75 p). - Rarity (VS 1e): regionally unique speleological geomorphosite (Bucegi Mountains–Leaota) due to the diversity and richness of the drip forms (including anemolites), gravitational prelingering and microforms resulting from capillary prelingering (calcitic eccentrites) (0.50 p). - Geological structure (VS 1f): the cave was formed along a tectonic diaclase (developed quasi-parallel to the vertical fault to the south), open in massive carbonate deposits (with fine stratification), monoclinically arranged within the tilted block of Piatra Galbenă (0.75 p). - Cave development (VS 1g): total cave length is 210.3 m (0.25 p). |
Aesthetic Value (AV2) | 2.00 p | - Physiognomy or physiognomy (VS 2a): geomorphosite with a unique physiognomy due to the diversity and richness of speleothems (0.75 p). - Chromaticity (VS 2b): chromatic gradation characteristic of karst voids (0.25 p). - Maximum exposure (VS 2c): selectively received speleological geomorphosite from observation points on the trail (0.50 p). - Landscape Attractiveness (VS 2d): the geomorphosite (with the embedded portal of the Yellow Stone Hills on the left slope of the Narrow Brusturet Gorge) is a component with local landscape attractiveness, but is also protected due to its landscape content. It belongs to RNGG1 (IUCN category IV) and is a nature monument (IUCN category III) included in the SPA (IUCN category Ib) of the PNPC (0.50 p). |
Ecological Value (EV3) | 2.00 p | - Vegetation (SV 3a): bare biotope. - Fauna (VS 3b): 28 invertebrate species were inventoried, including the coleoptera Duvalius duebelianus (local endemic, rare troglobiont/edaphobiont) and Dermestes latissima (endemic to the Southern Carpathians). Chiroptera Myotis myotis and Rhinolophus ferrumequinum were identified (1.00 p). - Degree of protection as part of a protected natural area (SV 3c): fully protected geomorphosite, declared as a natural monument (IUCN category III) (1.00 p). |
FUNCTIONAL VALUE (VF) = VF1 + VF2 + VF3 | ||
TYPE | SCORE | JUSTIFICATION |
Cultural (VF1) | 0.75 p | - Symbolism (VF 1a): the name “Dobreștilor” attributed to the cave is due to its discoverer, Ioan Dobrescu, who named it after his family name [1], an aspect with symbolic significance, in discrete association with geomorphosite (0.50 p). - Artistic and as graphic, cartographic, and photographic representations (VF 1b): the cave has less than 10 graphic representations (sketch—longitudinal profile, map) and photographs in tourist information/popularization works and one scientific paper (0.25 p). |
Scientific (VF2) | 3.25 p | - Scientific references in publications (VF 2a): scientific references in occasional publications, scientific articles in national and one international journal (1.00 p). - Formative scientific resource/economic resource (tourism, etc.) (VF 2b): scientific resource with medium addressability, due to the interest in caving: physical caving and zoospeology—invertebrates (28 species) and chiroptera (0.50 p). - Function as a didactic model of morphogenetic and evolutionary landforms and/or geomorphologic processes (VF 2c): model with illustrative value (0.75 p). - Scientific representativity (relevance) (VF 2d): speleological geomorphosite with regional representativity (0.50 p). - Paleogeographic interest (VF 2e): geomorphosite of moderate paleogeographic interest, useful for deciphering the genesis and evolution of the cave in local and regional contexts (0.50 p). |
Economic (VF3) | 3.75 p | - Number of possible activities (VF 3a): activities related to scientific research (mainly zoospeological), and geotourism may be practiced only on the basis of a permit issued by the PNPC administration (0.50 p). - Tourism potential (VF 3b): geomorphosite that does not arouse interest in tourism as the cavity is fully protected and is intended for scientific research (0 p). - Accessibility (VF 3c): car access up to 500 m from the geomorphosite, from DC 22 (0.75 p). - Related tourist infrastructure (VF 3d): Brusturet chalet (village Dâmbovicioara) about 1 km away (0.75 p). - Facilities and services (VF 3e): shared accommodation and catering services at the Brusturet Hut (0.25 p). - Distance to nearby localities with complex services (VF 3f): the distance to Rucăr and Zărnești is between 10 and 15 km (0.50 p). - Urban centers in the neighboring region (VF 3g): the nearest urban centers are the cities of Câmpulung (27,574 inhabitants/2021), 35 km away; and Zărnești (21,624 inhabitants/2021), 36 km away (0.50 p). - Tourism exploitation during the year (VF 3h): simple, occasional exploitation (0 p). - Tourism promotion of geomorphosite (VF 3i): brief, incomplete, unprofessional tourism promotion (under the name “Cave of the Foxes”) on a single website page, very rarely accessed. The targeting of the promotion reaches a regional level, at most (0.50 p). |
RESTRICTIVE ATTRIBUTE (AR) = AR1 + AR2 + AR3 | ||
SCORE | JUSTIFICATION | |
1.00 p | - Vulnerability to natural phenomena and processes (AR1): this speleological geomorphosite may be affected due to its vulnerability to seismic movements and other processes that may generate landslides (incachogenic deposits), but not affected as a whole (0.25 p). - Presence of economic activities with negative impacts or that could affect tourism and/or the geomorphosite (AR2): irrational pastoral activities in the area of drainage and water infiltration on the surface of the Piatra Galbenă karst plateau could affect the habitat of the speleological geomorphosite (0.50 p). - Unsightly elements (AR3): the iron fittings of a former metal grating that closed the upstream access about 90 m from the entrance (0.25 p) are visible. |
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Share and Cite
Trif, S.; Bilașco, Ș.; Sanda, R.; Ioan, F.; Vescan, I.; Barta, A.-I.; Irina, R. Geomorphological Analysis and Heritage Value of Dobreștilor–Brusturet Cave: A Significant Geomorphosite in the Bran–Dragoslavele Corridor, Romania. Heritage 2025, 8, 183. https://doi.org/10.3390/heritage8050183
Trif S, Bilașco Ș, Sanda R, Ioan F, Vescan I, Barta A-I, Irina R. Geomorphological Analysis and Heritage Value of Dobreștilor–Brusturet Cave: A Significant Geomorphosite in the Bran–Dragoslavele Corridor, Romania. Heritage. 2025; 8(5):183. https://doi.org/10.3390/heritage8050183
Chicago/Turabian StyleTrif, Septimius, Ștefan Bilașco, Roșca Sanda, Fodorean Ioan, Iuliu Vescan, András-István Barta, and Raboșapca Irina. 2025. "Geomorphological Analysis and Heritage Value of Dobreștilor–Brusturet Cave: A Significant Geomorphosite in the Bran–Dragoslavele Corridor, Romania" Heritage 8, no. 5: 183. https://doi.org/10.3390/heritage8050183
APA StyleTrif, S., Bilașco, Ș., Sanda, R., Ioan, F., Vescan, I., Barta, A.-I., & Irina, R. (2025). Geomorphological Analysis and Heritage Value of Dobreștilor–Brusturet Cave: A Significant Geomorphosite in the Bran–Dragoslavele Corridor, Romania. Heritage, 8(5), 183. https://doi.org/10.3390/heritage8050183