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Geological and Paleontological Sites of Brazil - 016

Brejões CAVE – Vereda Romão Gramacho – Chapada Diamantina – Bahia State


Mylène Berbert-Born (*)

Ivo Karmann (**)

(*) CPRM-Geological Survey of Brazil  
SGAN 603 Conj. J Parte A 1o andar  
Brasília-DF 70.830-030  
Phone (55)(61) 312-5252 - Fax 225-3985

(**) Department of Sedimentary and Environmental Geology
Geociences Institute, University of São Paulo
CP 1134805422 São Paulo SP
Phone (55)(11) 818 39 43 - Fax 011 818 42 07

© Berbert-Born,M.; Karmann,I. 2000. Brejões Cave, Vereda Romão Gramacho, Chapada Diamantina, Bahia State, Brazil. In: Schobbenhaus,C.; Campos,D.A.; Queiroz,E.T.; Winge,M.; Berbert-Born,M. (Edit.) Sítios Geológicos e Paleontológicos do Brasil.
Published 01/01/20000 on Internet at the address 
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(The above bibliographic reference of author copy rights is required for any use of this article in any media, being forbidden the use for any commercial purpose)


The large Brejões Cave is situated in the northern part of the Chapada Diamantina in Bahia. It was formed in Neoproterozoic limestones of the Salitre Formation of the Una Group, along the Jacaré River Valley at the northeastern margin of the Irecê sedimentary basin. The cave is formed by the two segments: Brejões I and II, which together are 7,750 m long, and are separated by a collapse canyon. The karst canyons host flora and fauna different from those of the surrounding caatinga, and form a special countryside which is both beautiful and has an ecological significance. The cavern stands out in the national speleological context for the sheer size of its galleries and of its speleothems, by the volume of its collapse dolines, and by its impressive 106 m high entrance. All these features have tourist appeal and were the motive for the creation of the Gruta dos Brejões/Vereda Romão Gramacho APA (protected area). Its scientific importance lies in the information on Quaternary paleoclimates which the study of its chemical deposits and fossiliferous sediments may reveal. Large religious meetings are held under its vault, and as popular cultural manifestations show that the cave has been democratically elected to its present place in the regional picture. While the cultural value cannot be denied, the depredation which accompany such huge meetings must be kept to a minimum.


The Brejões cave is an outstanding geomorphological feature of the central-northern region of Bahia State. It has very large subterranean fluvial galleries which contain groups of large speleothems. Its scenic value can be judged even from Brejões da Gruta village, where the cave entrance, over 100 m high, causes considerable impact. Inside the cave, conduits up to about 150 m high have skylights formed by collapse dolines which are up to 100 m in diameter.

In the context of the country's caves, its scientific, historic and cultural relevance is demonstrated by the paleontological deposits which have already been worked, as well as, the promising conditions for new discoveries, and also by the potential of archeological studies as suggested by the findings of rock paintings at the cave entrances and along the collapse valleys.

A point of special interest in the countryside at the surface is the contrast between the caatinga, which dominates the peneplaned (flat) surfaces of the watersheds, and the features found along the Jacaré river, which include the cave with a subterranean stretch of the river together with the segments formed by collapsed galleries forming canyons and dolines, in which the prevailing, more agreeable climatic conditions permit the survival of more exuberant vegetation which remains green the year long, and which is a refuge for the fauna, especially the birds.

The value of the Brejões cave receives popular recognition in the form of the religious ceremonies held there, which attract thousands. The natural relevance of the cave is now expressed by the creation of the Environmental Protection Area, a conservation unit known as the Gruta de Brejões/Vereda do Romão Gramacho APA.

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Figure 1: Localization of the Brejões cave. A) Access roads; b) Hydrographic network and limits of the APA Gruta de Brejões/Vereda Romão Gramacho; c) The 106m high entrance, seen from Brejões da Gruta village.

Localization and Physiography

The Brejões cave is situated in the northern Chapada Diamantina (in the so called "Dry Polygon" ) within the central-northern part of Bahia State, at about 500 km from the capital city, Salvador (figure 1). The cavern is formed in the Jacaré river valley, also known locally as the Vereda do Romão Gramacho, a tributary on the right bank of the São Francisco river. Its site lies close to the intersection of the Morro do Chapéu, João Dourado and América Dourada municipal boundaries, at latitude 11o00'42.7"S and longitude 41o25'59.6"W. The Chapada Diamantina National Park lies about 150 km to the South.

In the geomorphological unit of the Jacaré river lowland, the climate is hot and semi-arid, and altitudes vary between 480 and 560 m. The vegetation is a tree- and shrub-caatinga. Karst valleys with high limestone scarps are a feature of this unit. The more exuberant vegetation along the Jacaré river valley, with its great floral and faunal diversity, is due to the perennial nature of the river. The land use in the area is severely restricted by the predominantly shallow soils (eutrophic and lithic cambisoils) which are very stony on the steeper slopes (Rocha & Costa, 1995).

The cave lies in the northern part of the eastern border of the Irecê sedimentary basin, where carbonate sequences with minor intercalations of continental detritic sediments of the Salitre Formation predominate. This formation is a neoproterozoic unit of the Una Group, part of the São Francisco Supergroup (figure 2). The cave is formed in gray laminated calcisiltites with fine intercalations of algal laminations belonging to the Lower Nova America Subunit, probably related to the beginning of the first of the four depositional cycles which formed the Salitre Formation (Pedreira, 1993).

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Figure 2: Geology of the Irecê basin, compiled by Pedreira (1993)

Historical aspects

According to the local population, the Brejões cave was discovered in 1877. The first attention must have been given to the geomorphological exuberance of the cave region, but soon after, the great paleontological value of its sediments was recognized. The first discoveries inside the cave were published in 1938 by Father Camilo Torrendt, but a large part of his collection was lost, according to Cartelle (1983).

In 1967, student members of the Caving Group of the Ouro Preto School of Mines decided to traverse the 1800 km which separate south-central Minas Gerais State and central-northern Bahia, in order to explore and survey the cave (Le Bret, 1975). In 1977, systematic studies by members of the paleontological group of the Catholic University of Minas Gerais commenced. More than five thousand items were collected, belonging to sloths, giant sloths, mastodonts, armadillos, ant eaters, horses, rodents, and birds, among others (Cartelle, 1983).

In 1995 the Geological Survey of Brazil (CPRM) described and mapped the cave as part of the Morro do Chapéu Municipal Map, an institutional program aimed to offer basic orientation for Municipal Planning. The survey undertaken by this project prepared a map of the cave, and described its internal zoning, dictating use and conservation measures including access restrictions based on existing physical parameters and a preliminary evaluation of the hipogean fauna (Berbert-Born & Horta, 1995). This material has been the basis of the Management Plan for the Gruta de Brejões/Vereda Romão Gramacho APA.

Socio-cultural and legal aspects

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Figure 3: Example of rock paintings along the Jacaré River valley. (photograph by I. Karmann).

Religious manifestations are common in the cave, and reveal aspects of popular cultures which are in general ruled by natural and socio-economic conditions which stimulate religious feelings. Some of the best known examples are found in very poor regions, such as in the interior of Bahia and Goias States, and attract thousands of followers. Sensitive relationships between faith, subsistence and natural degradation are generated around the celebrations, and their analysis requires case-by-case treatment.

A religious festival which attracts thousands is held annually in the Brejões cave. Even though the available spaces are large, environmental damage is very obvious. Groups of speleothems are irreversibly damaged by breakages and by footsteps. A large quantity of rubbish and residues of offerings are left in the cave. Apart from the processions, Brejões receives smaller but equally uncontrolled visits throughout the year.

Other visible signs of human actions in the cave result from the scientific research, especially the paleontological investigations which leave behind pits, trenches and heaps of excavated sediments. Conservation of the sediment samples obtained during these excavations, and which could be used later for sedimentological and estratigraphical investigations aimed at paleo-environmental studies, leaves a lot to be desired.

The concern about damage to the cave environment is reflected by the current legislation on this theme. Federal Decree no 99,556 of 01/10/1990 states that "any natural subterranean cavity which can be reached by man is Brazilian cultural patrimony and as such will be preserved and conserved to allow technical-scientific studies and research, as well as speleological, ethnical-cultural, touristic, recreational and educational activities to be undertaken", adding the condition that its use and area of influence must obey conditions which assure its physical integrity and the maintenance of the local ecological equilibrium. The study of the environmental impact of any action which is potentially directly or indirectly damaging is obligatory (2nd and 3rd Articles).

The environmental protection area around Brejões cave has an area of 11,900 ha (figure 1). Its supervision and fiscalization were attributed by State Decree 32,487 of 13/11/85 to the Environmental Resources Center of Bahia State (CRA).

Apart from the recent and damaging human remains, Brejões also has much older registers of man's presence in the form of cave paintings and historic inscriptions near the resurgence of the river and at points along the valley scarps, which have not been sufficiently studied (figure 3). It is worth mentioning that rock paintings are now considered as being much more than a simple demonstration of the necessities of simple survival, and are also an artistic expression of cultural features (Barberi, 1995). They are part of the register of the evolution of human conscience and intellectuality.


Figure 4: The entrace to Brejões Cave. At the lower left corner of the entrance, the human figure gives a notion of the scale. (Photograph by E. L. Rubbioli).



The Brejões cave is one of the most outstanding in Brazil for the large scale of its galleries, saloons, skylights, speleothems, and its main entrance (figure 4). A karst canyon formed by collapse divides the cave into the Brejões I and Brejões II segments, which together have a length of 7,750 m (figure 5). Rock shelters and cave painting are found along the canyon.

Brejões I is the main part, along whose 6,570 m are concentrated the most impressive speleothems and morphological features which include two collapse dolines which form enormous skylights. These are cylindrical features whose bases are wider than the tops whose diameters reach 100 m. The cylinders are occupied by rock-falls , while their walls are supported by pillars (figure 6).

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Figure 5: Plan, transverse sections and a schematic profile of Lapa dos Brejões I & II; a) Large-scale stalagmites and travertine dams, with a human figure for scale; b) A group of stalactites, stalagmites, columns and calcite flowstones, with a figure for scale; c) Detail of nested calcite cave pearls in a travertine dam; d)Tabular blocks fallen into the river conduit, emphasizing the rectangular shape. (Photos by M. Berbet-Born).

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Figure 6: The collapse doline of the 2nd skylight. Note the stalactite near the upper border of the photo, and the figure for scale in the lower left corner. (Photo by M. Berbet-Born).

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Figure 7: Travertine dams, "wedding cake" or the "altar", one of the main spelethems of the cave, and an exceptionally fine national example of this type of speleothem. It is undergoing depredation through the accumulation of candle wax, breakages and scribblings. (Photo by J. Allievi).

Brejões I is up-stream above the canyon. The Jacaré river disappears down a sinkhole about 300 m from the main entrance, and reappears inside the cave at about 750 m from the entrance. From this point, it runs North-South along the entire westernmost gallery up to a siphon near the second skylight. Flow is gentle and perennial, with several stretches of slack water.

The river reappears inside Brejões II, and regains the open air about 300 m further on at the entrance to Brejões II. From here on the river flows for several km through scarpments which were probably formed by collapse of conduits. At least two currently undescribed cavities are pesent down-river.

A number of apparently-stagnant pools occur at the lowest points in the galleries inside the cavern. These show the direction of the inaccessible part of the river, since they correspond to the phreatic zone of the cavity.


Brejões I is formed by two mains sub-parallel galleries whose heights reach 80 m, and whose widths are up to 150 m. These conduits are mainly rectilinear, but have some sinuous stretches. The general direction is around N30E.

The connections between the two galleries lend an anastomosed geometry to the plan. Wide halls occur at the intersections, with steeply-stepped floors since each conduit develops its own topographic level. The roofs at the intersections are circular cupolas.

The eastern conduit is the larger and was an earlier river course. Transversal cuts have regular lateral walls without levels or benches, with either essentially triangular cross-sections such as that of the main entrance, or rectangular to square cross-. Going down-river from the entrance, a N-S linear stretch suddenly turns to N60W within the illuminated part of the cave. Within the penumbra, the eastern conduit branches off and occupies a lower level. Both conduits gradually turn into the main NE-SW alignment.

Important accumulations of clastic sediments are generally found under fallen blocks in the larger conduit. In turn, the blocks are covered by, or cemented by carbonate concretions. One of the huge skylights occur in this main gallery, and is the extreme product of collapse processes which have modified the original form of the conduit.

Small lateral branches are sometimes completely filled by clastic sediments.

The second smaller conduit has mainly polygonal cross sections. Piles of fallen blocks also occur in this conduit, but their volumes are smaller and the blocks are rectangular slabs rather than the cubes found in the main gallery.

After its resurgence the river runs along the western cavern wall, forming the youngest environment within the cave which is undergoing active incision.


As well as its size, Brejões is also exceptional for its large speleothems. Some groups of stalagmites, calcite flowstones and travertine dams or (popularly called "wedding cakes") are outstanding in size and beauty. They are up to 10 m high with diameters larger than 5 m, and have well defined border basins up to 2 m deep. One of the most impressive formations, the "altar" (figure 7), is used to receive offerings, and thousands of candles are lit here. The accumulation of dark candle wax is a factor which has led to its depreciation.

In some places the travertine dams occupy large areas of the gallery floors. Taking into account their size, the site of growth of these dams indicates places where vadose waters have flowed for some time in direction of the base level. At least four points of this type are seen in the older main gallery. One point is close to the altar, another point is further ahead and supplies the material for the concretions on the floor close to the entrance, while the other two are situated in the median stretch which includes the main inter- gallery connections. From the last point, the concretions are spread over various directions on the way to the conduit now occupied by the river.

Large scale flowstones coming from the highest point of the roof near the first skylight formed deposits over a thick pile of clastic sediments. Other ornaments include cones found in a travertine dam basin which is now dry, stalactites up to 13 m high, and delicate 'corals', nests of cave pearls, cave straws and helictites (figure 5 a, b, c). In stagnant water, floating crusts or rafts proliferate.

The greatest concentration of speleothems is found in two small galleries parallel to the main galleries at the eastern end of the cave (figure 5). Almost no chemical precipitation is occurring at present in this area, which is already outside the area of influence of the river. The groups here are quite phenomenal: flowstones, curtains, stalactites, stalagmites, columns, coraloids (like cauliflowers) and travertine dams, in combinations which occupy the roof, the walls and the floor, with dimensions from a few mm to various m.

Aspects of the cave evolution

The cave is part of the Bambuí Speleological Province in Irecê District, according to Karmann & Sánchez' classification (1979). It is formed in grey laminated calcisiltites of the neoproterozoic Salitre Formation of the Una Group.

Neither the internal sedimentary deposits nor the micro- to meso-scale morphological features have been studied in sufficient detail to allow the establishment of the erosive and depositional dynamics of the Jacaré river, which is the principal agent responsible for the opening of the cavern.

The general evolutionary lines can be set up by analysis of the organization of the gallerieis, of some morphological features, and of the distribution of some of the sedimentary components, which together show that the water course responsible for sculpting the cave underwent changes of its course and drainage direction during the foundering of the regional base level. This model has to be compatible with those established for the regional geomorphological and climatological evolutions.

The parallelism of the main galleries shows that evolution was from east to west, the galleries having developed by laterally entrenchment along progressively lower stratigraphical horizons in the W/NW direction, until the conduit along which the river presently runs is reached, as shown in the profile of figure 5. Ancient meanders can be recognized in some stretches of the galleries, which may have been formed as a result of seasonal or longer-term changes of the flow rate, or by bed migration due to sedimentation. At present changes in the river flow are responsible for the formation of flood plains where fallen blocks are being eroded.

Long stretches of former galleries are completely blocked by clastic sediments which may well be related to phases of detritus flows discovered in the Iraquara caves by Laureano (1998).

The recent river down cutting observed in the lower gallerieis appears to be evolving laterally rather than vertically. The predominantly tabular fallen blocks in the lower cave levels contrast with the approximately cubic blocks of the upper levels, and cave cross sections with horizontal long axes in the lower sections can be attributed to lithological control. In the lower levels, the rocks have a finer and more penetrative lamination defined by stratification and clay intercalations , while the rocks of the upper levels are more massive and less laminated.

In a general fashion, structural control is shown by the presence of sub-vertical fractures present at small scale and in the rectilinear stretches of wide galleries and in the collapse valley. The sinuous and curved pattern with anastosmosed stretches in the lower conduits show that the enlargement of the cave took place preferentially along the bedding planes of the rocks.

With the present data it is possible to interpret a syngenetic evolution of the cave in terms of a phase of phreatic initiation and enlargement, poorly developed or poorly accessible at the top of the conduits, followed by vadose down-cutting up to depths of 80 - 100 m, accompanied by lateral broadening up to a width of about 100 m. The original morphology of the conduits is poorly preserved, the collapsed form predominating.

Sediments and fossil material

A step about 15 m high in the floor of the main gallery is the result of erosion of a thick sedimentary deposit formed by poorly-sorted clastic sediments covered by chemical concretions and speleothems.

The sedimentary pile, still undescribed from a sedimentological point of view, hosts an important accumulation of fossils represented by the material collected by PUC - Minas Gerais research workers in 1977. About 1,500 pieces belonging to 17 examples of Paleolama sp (lhama), 6 samples of the sloth Nothrotherium maquinense and Eremotherium laurillardi, the giant sloth, parts of 3 examples of the giant armadillo Glossotherium (Ocnotherium) giganteum, 4 individuals of Pampatherium humboldti (giant armadillo), 1,000 pieces of birds, 2 exemples of Mymecophoga tridactyla (ant-eater), Coendou sp. (hedgehog), Lutra sp. (otter), rodents, deers, mastodonts, hogs, horses, tapirs and bats (Cartelle, 1983)

Environmental impact and suggestions

A number of relatively well-marked trails and one main route have been established along the cavern, over the rock falls and speleothems, and represent easy transit between the main entrance and the canyon, passing the two skylights (figure 5a). The large choice of routes allows easy access to a number of stretches of the cave which are only partly naturally lit, or are dark. Wall scribbling and rubbish are found along all these stretches, but are concentrated in the lighter parts, or along the main route.

A number of rudimentary altars which receive icons, statues, candles and offerings, attract larger agglomerations of people. It is thought that no restrictions on the altars already set up in the entrance vault are necessary, since the site is sufficiently large to accommodate the large number of people. Orientation about scribbling, rubbish and the use of fireworks is, however, essential. The situation of the altar set up on the large "wedding cake" stalagmite about 500 m from the entrance is entirety different. This speleothem is recognized as one of the main features of the cavern, and represents one of the major underground ornaments of this type in Brazil. The stalagmite is in a restricted space, insufficient for large groups of people, and the delicate outlines of the travertine dams are being destroyed.

Another locality which is being seriously damaged is the "fossil stretch" in the southern galleries, with its major concentration of speleothems. Transit here should be restricted. Each group of ornaments should be carefully surveyed, and the stretch should receive special zoning which restricts and supervises the visits. No modification of the natural environment is necessary, neither by removal of the natural objects nor by the introduction of artificial objects, since the simple solution of visits accompanied by trained and equipped guides may be sufficient, both in this and other stretches of the cave (Berbet-Born & Horta, 1995).

Is should be emphasized that for any type of management of the area, multidisciplinary studies of environmental impact on the cave and its surrounding, including the flora and fauna, are necessary. These studies should aim at a clear definition of the load capacity of the system, special restrictions and measures necessary in time or in space. Finally, the interests of the nearby communities must always be taken into account, and they should be invited to participate in these studies whose results should always be directed towards their benefits.



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