Contrafforte Pliocenico - Città metropolitana di Bologna
Transcript
Contrafforte Pliocenico - Città metropolitana di Bologna
The Reserve The geography of the Pliocene age The golden sandstone rocks that shape the Reserve’s spectacular landscapes recount the history of a small sea gulf whose waters submerged this territory during the Pliocene age (5-2 million years ago), when the plain area known today as the Po Valley was still a deep open sea environment, next to which the Apennine mountain range had already, for the most part, emerged. In the area between the valleys of Reno and Idice, there was a coastline which included the ancient river mouths of Reno, Setta, Savena, Zena and Idice. These watercourses carved out valleys which more or less coincided with the present day ones, and flowed to the sea, laying down transported material (during the Pliocene age, hundreds of meters of sediment were deposited in the gulf). The most ancient Pliocene deposits, visible today in the wide quarries and craggy ravines between Setta and Savena, are formed by layers primarily of pebble (conglomerates), typical of river environments near the coast. Higher up, the conglomerate gives way to gray clay, easy to recognize in the ravines (“calanchi”) of Rio Carbonaro, at the foot of Monte Adone, which was deposited in marine environments as deep as 300400 meters (the presence, in the clay, of pebble lenses that were deposited during the more intense flood periods, is a sign of how close the emerged land was). After this first sea invasion, there was a “regression” that led to the withdrawal of the waters and to the emergence of previously submerged areas, again exposed to erosion. At this stage the streams Setta, Savena, Zena and Idice flowed toward the northeast, carving the valley outlines from the recently deposited Pliocene clay. Following this, the area was again submerged by the gulf sea, flooding the new valley contours and progressively sealing them with a cover of sandy sediment which led to the “fossilization” of their V-profiles. It was during this new marine stage that the sandstone and conglomerate rock was formed, as can be seen today in the walls of the Contrafforte Pliocenico. Here the numerous traces to be seen in the rocks recall their place of origin: wave-bashed beaches into which flowed the wild Apennine rivers. Over the course of the entire Pliocene age, while the coarsest and heaviest materials were being laid down by rivers near the coastline, clay, silt and fine sands were deposited further offshore. These materials can be seen to the north of the Reserve, not far from Bologna, in the deep and large ravines of Pieve del Pino and Sabbiuno. After sedimentation, the deposits of the Pliocene gulf were involved in the orogenic movements: rising and shifting that explain how the most ancient sediments in the gulf, from the early Pliocene age, can today be found a few miles to the northeast of their original site, while one can walk today up to the peak of Monte Adone (654 m) on ancient beach deposits of upper Pliocene. Cliffs, pinnacles and grottoes The slender profile of the Contrafforte Pliocenico is the incredible result of the erosive modelling which took place between rocks of different “hardness.” The clay slopes at the base are of average steepness and gouged with ravines, while the sandstone above, more resistant to the erosion, is typified by vertical rocky cliffs which feature, along the steepest parts of the slopes, a distinct morphological step. The cliffs are this high and continuous also because their orientation crosses at a right angle that of the layers, ensuring greater stability. In the opposite side, facing northeast and north, the slopes are in the same direction as the layers, with a softer and more uniform morphology, without cliffs or drops and with wood covering. Along its whole range the Contrafforte Piocenico area is divided into larger valleys (Setta, Savena and Zena), while the smaller streams flow through Parchi e Riserve dell’Emilia-Romagna Riserva Naturale A sandstone tower in Sadurano. with deeper grooves, that at times take the aspect of true canyons (such as the Raibano and Aldani gorges), creating saddles that significantly lower the skyline. Along the slopes, the atmospheric agents, dominated by the wind, have modelled peculiar erosive shapes, more rapidly carving the less cemented or more fractured rocky masses. This is how the magnificent towers near the peak of Monte Adone or along the cliffs of Sadurano were created, along with ravines, rock shelters and ledges, like the marvelous Rocca di Badolo, Monte del Frate and Sadurano (well known to hikers and rock climbers). The presence of fractures and faults that run through the rock has fostered the development of small cavities, such as the Grotta delle Fate at the foot of Monte Adone and the Grotta dei Funghi near Badolo. Contrafforte Pliocenico By Fondazione Villa Ghigi The long rocky face of the Contrafforte Pliocenico. The unmistakable profile of Rocca di Badolo. 29 Pieve del Pino Pian di Macina Sasso Marconi r Castel S. Pietro o et Vado Monzuno Monterenzio Livergnano ro i T. S Loiano nt Rioveggio e ad o T. S Pianoro lla Marzabotto S. Lazzaro di Savena Ozzano Emilia na Pontecchio Tolé Vergato Bologna T. Q u Casalecchio di Reno na Monteveglio T. Z e the shells of gastropods and bivalve mollusks such as the easily recognizable oyster shells. The fossils too provide important data for the reconstruction of their living environment (climate, water depths, salinity, etc.). Frequent fossil traces, reminiscent of large petrified worms, stem from the fossilization of tunnels dug into the sediment by living organisms. Some of the most interesting remains are the phyllites discovered in 1929 in Livergnano by the Bolognese naturalist Giuseppina Gubellini. Among the leaves, packed into multiple layers and with perfectly preserved shapes and ribs, the holm oak, oak, laurel, poplar, willow, elm, plane, ash, hornbeam and many others, can be easily distinguished. The beautiful collection can be seen in the paleobotany showcases of the “G. Capellini” Museum of Geology and Paleontology in Bologna. e The majestic cliffs of Contrafforte are scored by delicate internal lines, along which the wind has chiseled minute sculptures, similar to bas-relief, bringing out the more cemented and resistant parts of the rock. The “sedimentary structures”, as they are called, result from the different ways in which granules were deposited and are an important evidence for a detailed reconstruction of the sedimentation paleo-environments. In Contrafforte, they always stand for shallow sea environments and can be considered a fossilized testimony of the small dunes created by waves and coastal currents, which moved the seabed and foreshore. Even their absence is telling, because it indicates periods in which the sediment was intensely mixed by the organisms living in it. In Contrafforte, on the main “bioperturbed” levels, which are more erodible, ledges that give movement to the walls at different heights have been modeled. Embedded in the rock or scattered in the detritus following rock breakdown, one also finds the fossils of organisms that inhabited the Pliocene gulf: mostly T. S av ena Sedimentary structures and fossils F. Ren beam and some plants typical of mountain woodlands. As well as beech, there is also yew, holly, bladdernut (Staphylea pinnata), spineless butcher’s broom, spring snowflake (Leucojum vernum) and lily of the valley (Convallaria majalis). ta to the sandy soil. Some of the herbaceous plants in the undergrowth include primrose, Apennine lungwort, anemones and, more rarely, the dogtooth violet, snowdrop, and Alpine squill. Down on the cooler valley floor, the microclimate favours horn- av ino Patches of holm oak on the southern walls of Monte Rosso. T. L The morphology of the Contrafforte Pliocenico has generated a wide variety of environments, with highly contrasting microclimates. Correspondingly, there is a rich and varied vegetation which, along with the plants found The woods in the Reserve throughout the Apennine upland and the Bolognese hills, includes The woods that cover most of the rare and unusual forms, often the Reserve are primarily aged woodremains of past landscapes that lands, harvested in the past and tohave survived in these almost inday abandoned or left to be imaccessible refuges. Perhaps the proved as tall stand woodlands. most representative image of the There are also young bushlands Reserve is the dark evergreen fogrowing on former fields that have liage of the holm oak, an oak typinot been cultivated since before cal to the Mediterranean area, the Second World War. On the drithat dots the sunny slopes, in er slopes drought-tolerant oak some sites forming green underwoods prevail, with a predomigrowth along with Mediterranean nance of downy oak (Quercus pushrubs such as phyllirea, Italian bescens) and its retinue of mannabuckthorn, tree heath, sageleaf ash, service tree and the rare rockrose, and poet’s cassia Montpellier maple, along with (Osyris alba). The cliff environscattered holm oak groves. Among ments hosts a characteristic flora the shrubs there is wayfaring tree, which includes lichens and mosshawthorn, wild privet, scorpion es, small succulents such as senna (Coronilla emerus), bladspecies of stonecrop (Sedum), der senna (Colutea arborescens), herbaceous plants with fine flowCanary clover (Dorycnium hirsuers like wood pink (Dianthus tum), common and black broom sylvestris), rock soapwort, globe(Cytisus scoparius, Lembotropis daisy, Alpine and autumn squill, nigricans). In the sparse and dwarf shrubs such as Italian everbright undergrowth, a profusion of lasting, wormwood, white rockgrasses and the rare and beautiful rose, thyme, wild marjoram, and flowers of burning bush, Canterheath-rose. The landscape is simibury bells (Campanula medium) lar to the variegated and scented and the various orchids (Orchis Mediterranean “garrigue” purpurea, O. simia, Cephashrubland and, in less extreme lanthera damasonium, areas, gradually gives way to Dactylorhiza romana) stand arid plains dominated by out. Extensive grasses and dotted with jumesophilic woods cover niper, Spanish broom and seathe cool damp slopes buckthorn bushes. In the facing north, where prairies grow such diverse floral hop hornbeam stands species as Siberian bellflower, alongside doany and various orchids (Orchis corioTurkey oaks, maples phora, O. morio, O. tridentata, (sycamore, field and Serapias cordigera) and Italian), wild service tree, feather-grass (Stipa pennaCornelian cherry, hazel ta), a rare graminaceous and laburnum. Chestspecies native to the nut is also common, southeastern steppes of having been cultivated Europe. While in the over the centuries by ravines and gulleys of the local populations the “calanchi” grows the vegetation typical to Orchis coriophora. and flourished thanks the city as well as from Sasso Marconi, Pianoro and Monzuno, along pleasant hillside roads. From Bologna, you take the Savena valley road to Pian di Macina, and then the secondary road SP 58 Pieve del Pino, which goes up to Badolo. A more scenic alternative is the hilltop road from Bologna to Badolo through Sabbiuno and Pieve del Pino. From Pianoro, in the Savena valley, another road leads up to Brento, at the foot of Monte Adone, or you may follow the SP 65 Futa to Livergnano. From Sasso Marconi just take via Ganzole which after the Prati di Mugnano park leads on to the SP 58 towards Badolo. The SP 36 Val di Zena skirts around the most eastern sector of the Reserve. For those coming from further away, the Sasso Marconi exit of the A1 highway is less than one kilometer from the road to Badolo. The Contrafforte Pliocenico Nature Reserve in the Bologna hills, extending in the municipalities of Sasso Marconi, Monzuno and Pianoro, protects a peculiar and imposing line of sandstone rocks which, for about 15 km, stand out widthways to the valleys of Reno, Setta, Savena, Zena and Idice. The Contrafforte Pliocenico culminates in the peaks of Monte Adone, Rocca di Badolo and Monte Rosso. In the Setta valley, the Reserve faces the most northern section of the Historical Regional Park of Monte Sole. Contrafforte’s particular morphology is at the basis of diversified and contrasting environments, of great interest in terms of flora and fauna components (the Reserve territory is included in the Site of Community Importance list). The protected area, which lies about 20 km from Bologna, can be easily reached both from og g ia these environments, which includes many legumes such as Spanish broom, French honeysuckle (Hedysarum coronarium), silver broom (Argyrolobium zanonii), Masquiller’s restharrow (Ononis masquillerii) as well as goldilocks aster and various orchids. T. Sa m Cliff plants and Mediterranean vegetation Contrafforte Pliocenico T. Idic Vegetation Grizzana Morandi F Bologna a .S er n Fauna The most interesting fauna is found in the steep cliffs, where the most protected ledges provide perching spots and breeding places for rare and protected birds in Europe. The bastions of Contrafforte Pliocenico were one of the few places of refuge for the peregrine falcon, even during the most critical period, which lasted until the late ’80s. Today, its presence in the Bologna area is gradually increasing, also thanks to the project “Pellegrino” Life Natura, sponsored by the Province of Bologna, which has chosen this elegant bird of prey with pointed wings as its symbol. Another extremely rare falcon, which also nests on cliffs, is the lanner falcon, very similar to the peregrine falcon but different from the latter in the reddish instead of black head and the lower parts with no stripes. From the ridge areas, young golden eagles sometimes push themselves to the highest points of the Reserve. In the winter, when it leaves the mountainous areas to retreat to the rocky hills, you can spot the wallcreeper. Around the cliffs, it is also possible to see Alpine swifts darting in groups, forming small colonies in the most inaccessible places. On the southern slopes and the upper parts of Contrafforte Pliocenico, are the ortolan bunting and the tawny pipit, two small birds typically found in shrub and sunny meadows. In the same environments during an excursion, one can often hear a rustling sound produced by reptiles on the run, such as the green lizard, the Italian three-toed skink, the southern smooth snake, the green whip snake (often allblack coloured) and, more rarely, the viper. Points of Interest 1 The Prati di Mugnano park, The peregrine falcon and other rocky habitats species Swift. The species of the wooded slopes The woods of the Reserve, and especially the northern slopes, are populated by roe deer, wild boars, foxes, and other hill mammals, including several species of forest bats (for which artificial nesting boxes have been prepared). There is no lack of important European birds of interest such as the honey buzzard, wryneck and nightjar, which are flanked by more common species such as jays, cuckoos, wrens and chiffchaffs. Among the reptiles, one can find the Aesculapian snake, a long slender snake that climbs nimbly on shrubs and trees in search of nests to prey on. Particularly significant are the limited and circumscribed signs of the spectacled salamander, a rare amphibian found in the cavities of the undergrowth near rivers or in other very cool and wet places, ideal habitats for the common toad, the agile frog, the Italian stream frog and the Apennine yellow-bellied toad. Among the invertebrates are some interesting significant environmental indicators, such as the stag beetle (Lucanus cervus), in the most extended wooded stretches, and white-clawed crayfish in the clear sheltered waters of streams. Lanner. the different layers, one can notice a peculiar V shaped geometry in the part between the Pliocene clays and the overlying sandstone. This is almost certainly a paleo-valley, namely the fossilization of the valley carved by the river during the Pliocene age. The stream is flanked by large specimens of white and black poplar, white willow and other riparian species, while near the river banks, patches of willow shrub go down as far as the gravel river bed (colonized by a grassy vegetation adapted to seasonal flooding). owned by the Municipality of Bologna, extends over 100 hectares in the territory of Sasso Marconi, with broad meadows, mixed oak woods and the remnants of chestnut groves. Here grow such rare and protected species as snowdrops, fire lily, Turk’s cap lily, and various orchids. The park, opened in 1973, reaches its highest point in the south with the panoramic summit of Monte Mario. 2 Beneath Monte Mario is part of the initial tract of the Roman underground aqueduct, the ingenious hydraulic works built in the Augustan age, which brought to Bologna the waters of the Setta by way of the excavation of a narrow passage about 20 km long and with a gradient of just 30 meters. In late antiquity, the aqueduct ceased to function and was discovered only in the second half of the nineteenth century, thanks to Antonio Zannoni, Municipality of Bologna engineer and archaeologist, who saw to its restoration and reopening. 3 In the winter, at the base of the steep southwestern wall of Monte Mario, the foliage of the umbrella pines stands out in the “Battedizzo pinewood,” already noted in midnineteenth century by the botanist Antonio Bertoloni, who recorded that despite its artificial origin, it is a confirmation of the mildness of the microclimate. In Battedizzo, in the twelfth century, the existence of a castle was documented. Its remains were destroyed by a landslide in 1775, while in the fourteenth century, a church dedicated to San Martino as is the present one, was one of the dependencies of the Pieve del Pino. spring snowflakes, anemones, violets, hellebores, while the presence of the fire lily and Turk’s hat lily is more localized. 5 The steep walls of the western slope of Rocca di Badolo, a traditional gym for climbing enthusiasts from Bologna, are the site of some interesting sedimentary structures created by wave movement, and brought to light, like minute linear sculptures, by the wind’s erosion. Near the top, in a storeroom carved into the rock, approximately forty axes from the Bronze Age were found in 1881. The fortress, mentioned along with the Battedizzo castle in 1164, was knocked down in the mid ’300s. The church of San Michele Arcangelo in Badolo and the oratory of the Madonna della Rocca, which can be reached by a picturesque path, are the result of postwar reconstruction. 6 On the majestic rocky face of Monte del Frate the sandstone is scored by a dense web of sedimentary structures, with many traces of fossils, associated with beach environments. In the ridge areas, along with juniper, brooms and bushes of rock-rose and Italian everlasting, the clumps of the southern plumet (Stipa austroitalica) stand out in the spring with their striking but delicate feathery blooms. On the rock face, not far from Badolo, is the opening to an artificial cave, discovered in 1966, with many small niches, almost A remarkable sandstone pinnacle on Monte Lolla. certainly a late medieval dovecote, probably already in use in Roman times as a place of worship. 7 Two rocky towers, fifteen meters high, flank the summit of Monte Adone, marked by a large cross made of metal. The more cemented sandstone layers, which protrude from the profile of the towers, have also formed a sturdy hat that has protected the rock column below from erosion. Below the summit, at the base of the rock marked by old stumps of holm oak, is the opening to the Grotta delle Fate (Cave of Fairies) of tectonic origin and accessible for about fifty meters (already used in prehistoric times, in past centuries it has been haunted by fantastic legends). On the northern side, the valley of the Rio Favale is covered by a dense forest rich in mesophilous plants. which goes from the bed of the Savena up to Livergnano is marked by high linear walls that culminate in Monte Lolla. The top of the ridge, shaped like a wall, has been carved into mushroom-like forms by the action of wind. 11The peculiar houses of Livergnano, an ancient village built along the road of Futa, partly because of their “rockiness” and partly because of their bright colors, are an example of spontaneous construction almost unique to the Bolognese Apennines. From the plateau of the church, rebuilt after the war as almost all buildings in the village, one can see a large portion of the Bologna hills. 12 From Monte Rosso to the stream Zena, the rocky face of Contrafforte appears in all its grandeur. The walls are characterized by very thick layers of conglomerates: in the large stones of different shapes and colours, one can recognize sandstone, limestone, gabbro, serpentinites and jasper (all rocks that still emerge 8 On the panoramic plateau of Monte Castellazzo, stood the Brento castle, built by the Byzantines in the sixth century (kàstron Brinton), which passed in the twelfth century to the bishops of Bologna and the Municipality of Bologna, only to fall into ruin. At the base of the mountain going toward the Savena, hidden in the woods, lie the ruins of the ancient church of Sant’Ansano, bombed in 1944. The new village church was built in 1959 by Father Marella along with the nearby “Casa del Pellegrino”. 4 The Raibano stream sculpts a deep valley between Monte Mario and Rocca di Badolo, flowing through smooth rock walls (colonized by mosses and maidenhair fern) and forming small waterfalls. On the valley floor, the beech tree, which here reaches one of the lowest altitudes in the Bologna area, is mixed with hop hornbeam and hazel. The undergrowth is full of 10 The section of Contrafforte The conglomerates in the rocky walls. 9 In the portion of Contrafforte which crosses the valley of Savena, along the lines that separate The picturesque houses of Livergnano. of poplars and willows, and sometimes patches of common alder, becomes denser, to form a sort of tunnel that shades the stream. Just to the east, outside the Reserve, stands the Monte delle Formiche (Mount of Ants) with the sanctuary of Santa Maria di Zena, where every year in early September, coinciding with the celebration of the Nativity of the Virgin, swarms of winged ants go to die on the mountain slopes. le Ganzole 98 PARCO AGRICOLO NATURALE PRATI DI MUGNANO ce rna Fo e le Quiete um Mugnano di Sopra a 1 243 Piazza Fi C. de Boschi 289 Fos so d Monte Mario 466 3 256 2 ago d Ca Orto ell el L o o Ri Ren Battedizzo Par During World War II, the rocky Fo s s o Raibano 4 St La Rocca 476 5 1 6 547 Monte del Frate ostr tta Fosso A1 o e M ada nal Aut Se gio 124 degli A ld a ni Campiuno nte 471 ta So o di C F oss à Bru cia Raieda di sopra le Quercia Lama di Setta 170 424 7 654 Brento 481 8 Monte Castellazzo Monte 343 Adone Ca Nova naro F o osso Pian Important religious building Tor ren “Calanchi” (ravines and gulleys) 3 Route number S Reserve boundary Fields and arable land Woods and shrublands N Ca di Luca 396 San Ansano 10 0 500 Querceto di Gorgognano 1000 m Monte Lolla 476 473 I Gruppi Ca di Castello or 11 Livergnano Point of interest Molino di Zena Piccola Siberia 481Bortignano Ca Poggio di Casola Casola o Mainly rocky formations 1 e avena 9 223 b id Path Itinerary route Zena 296 T Dirt road o in str Rio Legend po C. Nuova Querciolo bo am t R i o Car 342 C te Re Cinque Cerri Ri o ico Torren or 378 Badolo Rio Favale co 242 Uscita Sasso Marconi tance from the Contrafforte bastions of Contrafforte Pliocenico culminated in the Pliocenico were used by the Ger- terrible massacres of Monte man army as a defensive front Sole, are collected in documentaagainst the advancing Allied tion centers maintained by the troops. Bloody battles took place two communities. Still others in the area with involvement of may be seen along the routes civil populations, and villages promoted by the project “Gothic like Livergnano and BrentoZulaLine” (the charge of IBC - Instiwere completely leveled by the tute for Cultural Heritage of Rebombing. Many witnesses of the gione Emilia-Romagna, as part tragic war, which a short dis- of a European project). Poggio dell’Oca 434 Raibano 2 From the Zena valley, one goes up to Livergnano, along a path and then a dirt road through patches of woods and cool xerophilous woods on the north side of Monte Rosso. The return via Sadurano offers panoramic views of the sandstone cliffs above. Duration: 4 hours. The memory of the last war 378 395 1 From Badolo, following the directions along the “Via degli Dei”, you reach the summit of Monte Adone by way of Monte del Frate. The path, sometimes very scenic, provides a chance to appreciate the main geological features and vegetation of Contrafforte. Duration: 5 hours (round trip). A long excursion itinerary sponsored by CAI of Bologna, the “Crossing of the five valleys”, connects Monteveglio to Ozzano Emilia by the roads and paths in the hills, covering a large part of Contrafforte (the track has accurate markings and “rest stops”). The route crosses the “Via degli Dei”, a hiking trail that follows much of the historical route between Bologna and Florence. Continuing along the CAI paths, it is possible to take shorter loop trails in different areas of the Reserve. Rock climbing is now permitted only in the area of Badolo. Ri o M 525 oli ne tto 493 12 Monte Rosso 599 591 453 or 2 Sassi R io 263 dei Cani nte T 248 13 Sadurano Ri vi o dei Co r The Reserve, established in 2006, is the largest in Emilia-Romagna and extends for 757 hectares in the municipalities of Pianoro, Monzuno and Sasso Marconi. The management of the protected area is the responsibility of the Provincia di Bologna (Servizio Pianificazione Paesistica - via San Felice, 25 - 40122 Bologna - tel. +39 051 6598645 from www.provincia.Bologna.it/ ambiente, it is possible to have access to the Reserve’s website, which offers a wealth of information about the nature, history and management). There are plans for the creation of information facilities in the villages of the Reserve. In Brento is the Monte Adone Centre for Conservation and Research of Exotic and Wild Fauna, which provides shelter to stray, injured or confiscated animals (Via Brento, 9 - tel. +39 051 847600 - www.centrotutelafauna.org). Near Badolo, an interesting botanical garden dedicated to local flora, open for visiting from March to October, is located near the B&B Nova Arbora (via di Badolo, 35 - tel. +39 051 847581 www.novarbora.com). In one of the rock houses in Livergnano is the small private museum “The Winter Line”, dedicated to the events of the Second World War (via della Chiesa, 4 - tel. +39 051 778834). Among the publications concerning the territory, the most recent are Marconi G., Mongardi D. C’era una volta il mare… Natura e storia tra il “Sasso” e il Monte delle Formiche, Provincia di Bologna, Fondazione Cassa di Risparmio in Bologna, Gruppo Studi Savena Setta Sambro, 2005, and Paticchia V. (a cura), Percorsi della memoria. 1940-1945: la storia, i luoghi, IBC EmiliaRomagna, Clueb, 2005. More information on Contrafforte is available online at the Regione Emilia-Romagna websites www.ermesambiente.it/parchi and www.regione.emiliaromagna.it/natura2000/. Via dello Stale or Via degli Dei The Reserve’s territory is characterized by the presence of an ancient road that led from Bologna to Florence, passing Brento, Monzuno, Madonna dei Fornelli and then the Passo dello Stale (near Barberino). In Roman times the road commenced at low altitude, to reach then the ridge between Savena and Setta, while in the Middle Ages, the road left the city at San Procolo (now San Mamolo) and led immediately to the higher altitudes via Paderno, Pieve del Pino and Brento. Over the centuries the old mule track, which was also a route for pilgrims to Rome (“Romei”), was called various things (Romea, via dei muli, via di Barberino), but today is known as Via dello Stale or Via degli Dei (Way of the Gods) because of the site names along the way that may refer to pagan gods: Monte Venere, Monte Adone, Monzuno (from Mons Juno). Along the way, there were various fortified centres, including the castles of Brento, Badolo and Livergnano. na Sasso Marconi Useful background Ze 13 The stream Zena skirts the eastern boundary of the Reserve, flowing through deeply recessed land. The area, which is made up Recommended Itineraries re uphill from Contrafforte). The sunny rocks that overlook the old centre of Sadurano are dotted with holm oaks, shrubs and rockdwelling grasses. On the northern side, however, there are cooler wooded stretches, with patches of old chestnut groves. Pubblication promoted by the Emilia-Romagna Region Department of Agriculture, Environment and Sustainable Development © Regione Emilia-Romagna, 2008. Coordination: Parks Services and Forestry Resources (Monica Palazzini, Maria Vittoria Biondi). Edited by Fondazione Villa Ghigi. Text: Ivan Bisetti, Maria Angela Cazzoli, Teresa Guerra, Emanuela Rondoni. Editor: Mino Petazzini. Graphics: Tiziana Gironi. Photography: Fabio Ballanti, Ivan Bisetti, Maria Angela Cazzoli, William Vivarelli. Maps: Elvezio Tiboni. Graphic design: Sandri Carlotti Adv. Acknowledgments: Laura Biagi, Ornella De Curtis, Marina Terranova, Carlo Sarti. Translation promoted by the Province of Bologna’s Landscape Planning Service © Provincia di Bologna, 2010. Edited by Fondazione Villa Ghigi. English translation: Simmetrie & Partners. Editor: Mino Petazzini. Acknowledgments: Paolo Pupillo. Printing: Grafiche Zanini, Anzola Emilia (BO). Cover: tree heath and holm oak.