The ancient watermill in the village of Befa is being brought back to life as a place that safeguards the deepest soul of this part of Tuscany, where nature still follows its original rhythm and everything invites us to rediscover the value of simplicity.
Woods, streams, paths, and rolling hills surround this corner of the Murlo countryside, shaping a landscape where history, silence, and beauty coexist, and where the relationship between people and nature still retains an authentic and profound presence. It is a land to be explored slowly, on foot, by bicycle, or on horseback, along trails and country roads that open onto landscapes which still tell, even today, of a centuries-old relationship between human labour and the power of nature.
Of Etruscan origin, Murlo lies just a few kilometres from Siena, in the countryside between the Val d’Arbia and the Val di Merse, at a natural crossroads between the Sienese hills and those of the Grosseto area. Its location makes it possible to reach some of Tuscany’s most iconic destinations in around thirty minutes by car, from the Val d’Orcia to Monte Amiata, and from Siena to Montalcino.
Yet it is above all the more intimate dimension of the landscape that reveals its true character: a countryside to be explored without haste, following the rhythm of the seasons and letting yourself be guided by the network of streams, woods, hills, and ancient routes that weave through it.
It is within this landscape that the location of La Befa takes on a particular significance, as reflected in the very toponym
The Molino della Befa
In the heart of the valley where the Crevole and Crevolone streams meet, surrounded by woods, waterways, and ancient paths, stands the Molino della Befa: a place rich in charm, history, and memory. Here, nature has been in dialogue with human ingenuity for centuries, among medieval remains, ancient hydraulic works, and landscapes that have preserved their authenticity intact.
The words of Luciano Scali vividly bring to life this special corner of the Murlo area, from which our agriristoro takes both its name and its spirit.
“It is not easy to describe this place, because it seems to contain within itself an extraordinary concentration of breathtaking natural beauty, traces left by people over many different periods, and historical and almost mystical sites that can still be read and understood today. The only dilemma is deciding where to begin. Yet the sight of the old mill building immediately dispels any doubt, inviting us to follow its history and explore the structures that still survive around it.
This intention, however, is easier to express than to carry out fully, because doing so would mean moving through such a remarkable setting with one’s eyes closed to everything else. On either side of the place where we now stand are two facing hills, both bearing the title of ‘mount’: Monte Pertuso and Monte Ambrogio, although the former reaches only 272 metres above sea level and the latter 231. Despite their modest elevation, they appear much higher than they really are because of the way they loom over the narrow valley where ‘the two Crevole’ — the Crevole of Murlo and the Crevole of Monte Specchio, now known as the Crevolone — meet.
In ancient times, buildings stood on the summits of both hills. While much is known about Monte Pertuso and its history, the same cannot be said of Monte Ambrogio.
Even historians are reluctant to draw conclusions, probably because the information that has reached us so far is insufficient to provide reliable answers. On Monte Pertuso there once stood a large settlement of Lombard origin, as attested by a church dedicated to Saint Michael the Archangel, as well as a castle that the Sienese destroyed in 1271 in order to drive out the Ghibelline exiles who had taken refuge there. The fortress, whose remains can still be seen, later fell into ruin. The place name itself may perhaps derive from a tunnel, still accessible until around half a century ago, which connected the fortress with the church.
Below, at the confluence of the two streams, where the flow of water was more abundant than elsewhere, a mill was built. The Leopoldine Land Register identifies it as the ‘Molino della Befa’. The presence of members of religious orders in the area was certainly not unusual, nor was their interest in bringing their grain to be milled there.
Returning, however, to the subject that concerns us, one cannot fail to notice the large basin behind the mill. Water arriving from a diversion weir some distance upstream collected here, forming the mill’s reserve reservoir — the bottaccio — which supplied the water required for its operation.
The various structures normally found in a watermill can be seen at Befa with unusual clarity and detail. The entire course followed by the water, from the intake at the weir to the reservoir beside the mill, reveals a succession of solutions specifically devised to overcome the natural obstacles along the way.
The platea, as the weir built across the Crevolone to divert part of its water towards the mill was known, was positioned where the stream forms a broad bend, precisely at the point where a steep path begins. Winding upwards through the woodland in wide curves, the path leads to a higher area known as the “accetinata”, from which the cork-oak woods begin.
The weir is a solid construction of brick and river pebbles, bound together with an exceptionally hard lime mortar that has allowed the structure to remain clearly recognisable to this day. Several walls still emerge from the mass of sediment and debris accumulated against the barrier. Although largely concealed by vegetation, gravel, and material carried downstream during floods, they still allow the curious observer to understand how this water-intake system once worked.
The stream reaches the barrier after tracing a broad curve. Here, the greater flow of water was channelled through a specially constructed passage towards an intake opening controlled by a guillotine-style sluice gate. The barrier across the stream determined the level of the impounded water, which would always remain higher than the intake opening leading to the mill.
Put simply, if the stream continued to flow over and beyond the weir, this meant that upstream there was a reserve of water capable of feeding the millpond. During periods of low water, when the stream pooled behind the barrier, the mill could continue to operate for as long as the level of the reserve remained above the threshold of the intake.
The opening in the wall was closed by a sluice gate which slid between two vertical guides built into the sides of the opening. It could be raised just enough to ensure a steady flow of water towards the millpond. The gate itself was lifted by means of a sturdy screw mechanism operated from above, allowing the opening to be regulated as required.
This was a delicate operation, because care had to be taken to prevent the water from gaining enough speed to erode the earthen sides of the gorello, the narrow mill leat through which it flowed. This helped prevent damage to the channel as well as excessive accumulation of silt on the bottom of the millpond.
This was one of the problems that affected the mill, particularly during the autumn rains, when large quantities of debris, leaves, and other organic material were washed down from the surrounding land.
Yet it is above all the course of the gorello that is remarkable, because of the ingenious solutions adopted along its route before it finally reached the mill. In order not to interfere with the road to Resi, part of the channel was covered over and carried through a masonry culvert beneath the road, which runs above it for a considerable distance.
Even the bridge of the old coal railway incorporated, alongside the passages for the road and the stream, a separate culvert to allow the water of the gorello to pass through.
It is indeed a fascinating work which, although partly lost today, says a great deal about the ingenuity of those who came before us: people accustomed to solving the practical problems of survival by sharpening their wits and rolling up their sleeves, finding ways to turn the natural conditions around them into productive resources.”
The railway trail
A truly distinctive itinerary, weaving together history and nature, follows the route of the railway that once connected the mines of Murlo with La Befa station, passing through the Basso Merse Nature Reserve.
Through enchanting landscapes such as the Crevole valley, among historic bridges, ancient mills, and remarkable examples of industrial archaeology, the route offers the chance to discover the botanical and geological features that make this area so unique. The trail crosses land that was once submerged beneath the ancient Ligurian-Piedmont Ocean, revealing volcanic and metamorphic rocks such as basalt, gabbro, and Murlo’s famous “green marble”, which was also used in the construction of Siena Cathedral.
The path continues through a landscape rich in Mediterranean scrub, growing over distinctive red rocks and creating a unique combination of vegetation and geology that gives this area its wild character. The “Murlo marl dunes” add an almost exotic quality to the experience, as the route passes through a remarkable variety of landscapes and reaches breathtaking viewpoints over the Crete Senesi and the Val d’Orcia. Geological and industrial history intertwine here in an authentic and unforgettable experience.
The itinerary begins in the former mining village of Miniere di Murlo, a hamlet of the municipality of Murlo located in the Crevole valley. Once equipped with its own thermoelectric power station, the settlement is a remarkable example of an industrial village created to meet the needs of both the local population and the mining industry.
From the second half of the nineteenth century and for around a hundred years, lignite was extracted here. An 1881 booklet preserved in Siena’s Biblioteca degli Intronati and published for the Milan Industrial Exhibition by the Compagnie Française des Charbonnage de Pienza, which managed the mine at the time, describes it as follows: “black in appearance, with little lustre, producing a chocolate-brown powder when freshly mined.”
The route follows the course of the old railway built to transport the lignite extracted from the mines. The wagons were loaded and, once outside the tunnels, pulled by horses as far as La Befa station, from where the material continued its journey.
This stretch of railway, a fascinating example of industrial archaeology in Tuscany, bears witness to the technological innovation of the period and to the importance of lignite for the local economy.
Lignite can still be found along the route today. For much of the first section, the path is covered with squared, smooth brown stones that look almost like pieces of chocolate.
Continuing along the trail, the route crosses the Crevole valley, a natural landscape where the stream of the same name once powered numerous mills, used for grinding grain and even cement for the mining village. The valley is significant not only for its industrial history, but also for its remarkable natural features. The path runs across land that, millions of years ago, formed part of the seabed of the ancient Tethys Ocean, and along the way it is possible to observe sedimentary and igneous rocks that bear witness to a long and complex geological evolution.
Along the route, two historic bridges offer further evidence of the engineering skills of the period: the bridge over the Crevole, 22 metres long and restored in 2019, and the bridge over the Crevolone, a stone-and-brick structure measuring approximately 36 metres. These bridges did more than simply provide crossings over the streams: they were also an essential part of the hydraulic system that supplied water to the mill.
The trail then reaches the Molino della Befa, a historic watermill that already existed before the railway was built, as documented in the 1821 Leopoldine Land Register. Restored and now home to a small farm restaurant, the mill retains the charm of its past and offers another example of the ingenuity and industriousness of the local community.
A short distance away stand two old lime kilns, probably once fired with limestone quarried nearby. The stream is actually forded at the Molino della Befa, at the end of this approximately seven-kilometre section of the route.
A few metres further on, a sharp turn leads uphill towards Montepertuso along a steep path. Almost nothing remains of the castle that once stood at the summit. The parish church of San Michele Arcangelo and its rectory, however, still survive. Today, the latter is home to a centre run by the Comunità Mondo Nuovo for young people facing difficult circumstances. From the beautiful meadow in front of the church, there is a spectacular 360-degree view stretching from the Val di Merse to Monte Amiata.
Walking these paths today means stepping into the atmosphere of the past and experiencing the landscape in an authentic way.
Municipality of Murlo – The Murlo Mines Railway Trail
The Ritrécine Horizontal-Wheel Watermill
The Molino della Befa belongs to the category of horizontal-wheel watermills, known in Italian as ritrécine mills.
A Little History…
Mills are an ancient invention. Evidence of these machines already exists from the 1st century BC in the eastern Mediterranean. In his treatise De Architectura, the Roman architect Vitruvius described the watermill, although he did not explain how this technology had passed from the Greeks to the Romans.
At that time, the heavy hourglass-shaped millstones were still turned by muscular power, provided not only by animals, but also by slaves, poor citizens, and criminals sentenced to this form of labour.
The widespread use of the watermill came much later, during the Carolingian period and the early Middle Ages, and represented an important technological revolution. The economic development that took place throughout the medieval period encouraged the increasing spread of water-powered mills.
There were two main types of construction and operation: mills with a vertical wheel and mills with a horizontal wheel. Large vertical-wheel mills were generally found along Tuscany’s main waterways. Through more complex systems of gears and pulleys, they could power several millstones at once and therefore produce larger quantities of flour.
Horizontal-wheel mills, known as ritrécine mills, used smaller millstones and had a considerably lower flour output. Their great advantage, however, was their ability to operate with relatively small quantities of fast-flowing water, typical of the many streams found throughout the region.
These mills were almost always isolated buildings located beside a watercourse. Their production capacity was generally limited, sufficient only to meet local needs: those of a farm, a landowner, or at most a small village.
In the Middle Ages, building a watermill required very specific conditions. It was not enough simply to have access to a suitable site; it was also necessary to hold the legal rights to use it. Construction and maintenance involved considerable expense as well. For this reason, the building of a mill was largely the privilege of lords and religious institutions, who alone were usually in a position to exercise rights over a watercourse and bear the significant costs involved.
For the investment to be worthwhile, there had to be enough grain to grind to generate a profit, while the cost of constructing the mill needed to remain as low as possible. This encouraged the spread of ritrécine mills. Although their hourly and daily flour output was lower than that of vertical-wheel mills, they could operate effectively even along streams with seasonal flows and could be built at relatively modest cost. This made it possible for them to be widely distributed across the countryside.
In addition, rural inhabitants were often required to bring their grain to the mill belonging to the local lord, monastery, or municipality, paying a milling tax that further increased the profitability of the mill.
Location and Siting
Along a river or stream, sites with a natural waterfall or a sudden drop in elevation were preferred, as these conditions increased the force of the water striking the blades of the ritrécine. A minimum difference in height of around 3–4 metres was generally required between the water level in the millpond and the stream bed.
Where the terrain was relatively flat, it became necessary to increase the height of the weir, extend the mill leat, and enlarge the millpond, all of which significantly increased construction costs.
During the first decades of the nineteenth century, the agricultural policies promoted by the House of Lorraine led to a profound reorganisation of the Tuscan countryside, and rural areas began to become more densely populated. The growing demand for flour, essential to meet the increasing need for bread — the staple food of the time — encouraged the entrepreneurial classes of the period, still largely made up of landed nobility but increasingly joined by the emerging bourgeoisie, to invest in the construction of new milling facilities.
With the advent of the First Industrial Revolution and the introduction of electric power, the larger mills, whose production levels made conversion economically worthwhile, were gradually modernised. Smaller mills based on the ritrécine system, on the other hand, slowly fell into disuse as they became increasingly uneconomical.
The Ritrécine Grain Mill
The overall structure of a watermill consisted of four distinct sections:
- The building itself;
- The hydraulic system, including the structures used to divert the water, channel it through mill leats, and collect it in reservoirs or millponds;
- The drive system, made up of the mechanisms used to convert the energy of the water into rotary motion;
- The milling system, consisting of the millstones and all the equipment needed to turn grain into flour.
At the heart of the drive system was the waterwheel, which determined the type of mill. In mills equipped with a horizontal wheel, known as a ritrécine, the wheel consisted of a series of spoon-shaped wooden or iron blades arranged horizontally. It was housed in a lower chamber known as the carcerario, located beneath the main part of the building.
Upstream from the mill, water from the stream was diverted by means of a weir, or serra, and channelled into a reservoir known as the bottaccio or gora. From there, it descended through a channel and struck the blades of the ritrécine, causing the wheel to rotate. After powering the wheel, the water flowed out of the carcerario and was carried through another channel back into the stream downstream from the mill.
The ritrécine was directly connected by a vertical shaft to the millstone on the floor above. The upper millstone, known as the soprana, rotated at exactly the same speed as the waterwheel, with a 1:1 transmission ratio, while the lower stone, known as the sottana or dormiente, remained fixed.
Together, the pair of millstones formed what was known as the palmento. A very narrow gap had to be maintained between the two stones, allowing the grain to be crushed and transformed into flour and other products such as bran and semolina. The distance between the stones, which directly affected the quality of the milling, was adjusted by the miller using a lever mechanism.
The grain was fed through the central opening in the upper millstone, falling by gravity from the hopper above. Centrifugal force then pushed the flour outwards, where it was collected through a dedicated channel.
To make the grinding process more effective and help carry the flour towards the outside edge, the miller cut grooves into the horizontal surfaces of the millstones. These grooves, known as raggiature, were made with special chisels and hammers and had to be regularly sharpened and renewed.
A Short Glossary
Serra or platea: a weir or diversion barrier built across the watercourse to raise the water level and direct water towards the gora, or millpond.
Bocca di presa: the water intake, controlled by a sluice-gate system, through which water passed from the platea into the gorello.
Gorello or aldio: the mill leat or feeder channel connecting the platea to the gora.
Gora: also known in some areas as the bottaccio, the reservoir or millpond located beside the mill building and used to supply water to the mill wheel.
Condotto di carico: also known as the tromba di carico, the inclined penstock connecting the gora to the carcerario. Controlled by a sluice gate and narrowing towards its lower end, it allowed the water to build up pressure and energy before striking the blades of the ritrécine. The penstock ended in a small opening, only a few tens of centimetres in diameter, designed to maximise the force of the water reaching the horizontal wheel.
Carcerario: the chamber on the lower level of the mill where the ritrécine, the horizontal wheel that powered the mill, was housed.
Ritrécine: a horizontal waterwheel fitted with spoon-shaped wooden blades. Water falling from the penstock struck the blades and set the wheel in motion, driving a vertical shaft directly connected to the upper millstone of the palmento.
Palmento: the pair of millstones located on the upper floor of the mill.
Soprana: the rotating upper millstone of the palmento, directly connected to the ritrécine with a 1:1 transmission ratio.
Sottana or dormiente: the lower millstone, usually fixed, upon which the soprana rotated.
Scarico: the tailrace or outlet channel leading from the carcerario, which collected the water after it had passed through the wheel and channelled it back towards the stream.
Murlo and the etruscans
The importance of the Etruscans in Murlo probably began in the 7th century BC, with the emergence of an aristocratic class that initially exploited the area’s local resources — copper mining was particularly important here — and later benefited from the growth of trade, encouraged by the presence of waterways connecting the territory with the sea.
Trade involved both raw materials used in metalworking and objects produced by the skilled craftsmen working at Poggio Civitate. The period of greatest prosperity undoubtedly extended from the 7th to the 5th century BC, during the so-called Orientalising and Archaic periods. Important traces from these centuries have survived and today provide valuable evidence for the study of Etruscan civilisation, attracting scholars from around the world.
The presence of the Etruscans is still clearly visible in Murlo, both across the landscape and, according to a number of genetic studies, among the local population. The rich archaeological discoveries at Poggio Aguzzo, the site of the Etruscan necropolis, and at Poggio Civitate, where the famous princely residence once stood, contributed to the creation of the Antiquarium di Poggio Civitate, Murlo’s Archaeological Museum.
The possible genetic continuity between the ancient Etruscans and the native population of the area has also been the subject of scientific research. Studies carried out from the 1980s onwards, including research published in The American Journal of Human Genetics in 2007, investigated the genetic heritage of populations from Murlo and other historically Etruscan areas.
Geology of the railway trail
The old railway line serving the mine cuts through rock formations that, for around 100 million years, formed the seabed of part of the ancient ocean known as the Tethys.
This ocean began to form approximately 200 million years ago, during the Triassic period, when intense volcanic activity broke apart the existing landmasses, gradually separating the continental blocks that would later become present-day Europe and Africa. Lava rising through long fractures in the Earth’s crust — the oceanic ridges — solidified to form new ocean floor, upon which large quantities of deep-sea sediments were deposited.
The process of oceanic expansion came to an end around 140 million years ago, when compressional movements began, eventually leading to the formation of the Alps and the Apennines. During these events, the Tethys Ocean disappeared and fragments of its seabed were uplifted and displaced onto dry land, folded and disrupted in the process.
The entire municipality of Murlo offers a remarkable opportunity to study and observe this ancient ocean floor and the geological processes that transformed it. Between Casciano and Vallerano, for example, serpentinites, gabbros, and basalts can be found at the surface — rocks formed through the solidification of magma produced along oceanic ridges.
At the Crevole bridge, directly beside the road, it is possible to observe “pillow basalts”, rounded rock formations created when magma cooled rapidly upon contact with seawater.
Along the Mining Trail, sedimentary rocks deposited above the newly formed oceanic crust are more prevalent. These include radiolarites, the Murlo Marls, Calcare Balzano, and the Argille con Calcari Palombini formation. In this area, the magmatic component of the ancient ocean floor is represented only by gabbro.
To better understand the origin of these rocks, the trail can be followed starting from Miniere di Murlo. This easy and scenic 7-kilometre educational route, including the return journey, follows the former track of the mine railway, one of Italy’s earliest privately operated railway lines, built in 1871.
The railway transported lignite to the nearest railway station, following the Crevole gorge along an almost level route made possible by rock cuttings, embankments, and the daring Ponte Nero bridge.
The route has been proposed as a Geosite of Local Interest (GIL 37) because of the variety of geological formations found along it, most notably the impressive layers of radiolarite in different colours: red radiolarites, known as diaspri, coloured by iron oxides; green radiolarites, known as ftaniti, associated with the presence of pyrite; and black radiolarites, or liditi, coloured by graphite.
These rocks are formed from the siliceous skeletons of marine organisms deposited at depths of more than 4,000 metres on the floor of the ancient Jurassic ocean, locally enriched by layers of manganese oxides produced by submarine volcanic activity.
In the radiolarites found along the route, coatings of manganese oxides can be observed, only rarely occurring in microcrystalline form. In the altered gabbros at Fondo Bello, approximately 1 km from the beginning of the trail, minerals include analcime (also known as analcite), laumontite, prehnite, large crystals of diallage and, with a little luck, diopside, chabazite, epidote, and natrolite.
In the gabbros along the nearby Crevolone stream, feldspathic veins contain albite and, more rarely, diopside, laumontite, natrolite, hornblende, prehnite, talc, and zoisite. A small talc mine was also historically reported on Monte Pertuso above.
The Radiolarites (Diaspri) form the main outcrop along the first section of the trail. They are easily recognised by their distinctive liver-red colour and by their division into thin layers only a few centimetres thick.
These sedimentary rocks consist mainly of the remains of radiolarians, marine microorganisms with siliceous skeletons that lived suspended in the water column. Smaller quantities of iron oxides are also present, giving the rocks their characteristic red colour, together with manganese oxides, visible as shiny black coatings and formerly exploited through small-scale mining.
The identification of the radiolarian species preserved within the rock has made it possible to date its formation to between 160 and 140 million years ago, during the Late Jurassic.
The presence of these radiolarites provides evidence of both the great depth of the ocean and the intense submarine volcanic activity taking place within the Tethys at that time. The pressure exerted by the water — at an estimated depth of at least 2,000–3,000 metres — together with the enormous quantities of carbon dioxide released from submarine ridges caused calcareous material settling on the seabed to dissolve. Only the siliceous skeletons of radiolarians were able to accumulate, eventually giving rise to the radiolarites.
Along the trail, it is also possible to observe evidence of the immense forces to which these rocks were subjected during the closing of the Tethys Ocean and their displacement to their present-day position. Fractures and folds, sometimes spectacular, are relatively common and add further geological interest to the route.
A little further along the trail, gabbro appears: a dark rock of igneous origin. Unlike basalt, which cooled rapidly at the surface, gabbro formed through the slow cooling of magma within the oceanic crust and is therefore classified as an intrusive igneous rock.
The way in which it solidified is clearly reflected in its appearance. Slow cooling at depth allowed relatively large crystals to develop. Crystals of pyroxene — mainly dark green diallage — and milky-white plagioclase, the principal minerals that make up gabbro, can be clearly seen.
On a fresh fracture surface, the rock is dark green and its individual minerals are easily distinguishable. In several places along the trail, however, particularly near faults or other areas where the rock has been subjected to stress, it breaks down into a yellowish brecciated material in which the pyroxene crystals remain visible as dark, shiny flakes.
Continuing along the trail, we encounter the Murlo Marls, which appear weathered and broken down into thin grey flakes composed mainly of clay. These are interspersed with more compact outcrops of a white rock known as Calcare Balzano, a marly limestone containing, in addition to calcium carbonate, a certain proportion of clay.
The presence of limestone marks the beginning of the closing of the Tethys Ocean, as it indicates that both the depth of the ocean and its magmatic activity had decreased, allowing calcium carbonate to begin accumulating on the seabed.
Calcare Balzano is formed from the accumulation of calcium-carbonate skeletons and shells belonging to various species of microscopic marine organisms, particularly coccolithophores and calpionellids. By studying these microfossil species, geologists have been able to date the formation of the rock to around 140 million years ago, during the Early Cretaceous.
In the past, Calcare Balzano was widely used to produce quicklime for construction. For this reason, throughout the local area — including on the hills overlooking the old railway trail — it is still relatively easy to come across the remains of lime kilns beside long-abandoned quarries.
Approaching La Befa, near the Molino, the trail reaches the Argille con Calcari Palombini, or Palombini Clay and Limestone Formation. These rocks closely resemble the Murlo Marls and can be seen near the confluence of the Crevole and Crevolone streams, where they form striking bare hills made up of thin flakes of claystone interlayered with beds of grey limestone.
The unusual name of this formation derives from the colour of the limestone, caused by its high silica content: the Latin words palumbus or columbus refer to a grey or dove-grey colour.
Like the Murlo Marls, this rock formation also reflects the gradual closing of the Tethys Ocean, as suggested by the alternation of limestone beds and clay-rich layers. It is thought that, at intervals, submarine currents carrying calcareous sediments from shallower waters reached the deeper ocean floor where the clays were being deposited. These sediments were probably remobilised by the tectonic movements associated with the closing of the Tethys.
The small number of microfossils preserved within the limestone beds has made it possible to date the formation of the Argille con Calcari Palombini to around 130 million years ago, during the Early Cretaceous.
TOPONYM LA BEFA
The very name of the place appears to reflect its historical role as a landmark and a territorial boundary. Its etymological roots can be traced to medieval Germanic languages and to Lombard and Gothic dialects, in particular to the root wifa or wibja, meaning “post”, “branch”, or “boundary marker”.
The term referred to a post decorated with branches, or to another conventional marker placed in the ground to define private property, estates, or jurisdictions. From this root, through medieval Latin forms such as wifa, guifa, or guiffa — with the meaning signum quod propter defensionem ponitur, a sign placed for protection or demarcation — a number of place names developed in northern and central Italy in association with boundary locations, including Ghiffa in Piedmont and Befa in Tuscany.
Even today, La Befa lies in an area marked by clear natural and territorial boundaries: to the west by the Crevole stream and to the east by the Rigagliano stream. This particular geography historically defined the limits between different territories and communities, corresponding today to the municipalities of Murlo, Buonconvento, and Montalcino.
Water, therefore, is not only one of the defining elements of the landscape of La Befa, but also a presence that, over the centuries, has helped organise and distinguish the inhabited territory.
From the Early Middle Ages, and already during the Lombard period, places bearing names derived from this same linguistic root served a practical function as territorial markers. They were visible points of reference used to define reserved lands, properties, and boundaries controlled by Lombard kinship groups, known as fare, or by rural estates and administrative centres.
Over time, these markers became established reference points within local jurisdictions, often located near waterways, mountain passes, and important routes of communication.
In this sense, the name La Befa still seems to reflect the very nature of the place: a territory lying along a natural line of separation, where water, land, and ancient routes have helped define boundaries, relationships, and a sense of belonging for centuries.
It is precisely this layering of landscape and history that makes La Befa such a distinctive place: not simply a small village set in the Sienese countryside, but a point where geography has shaped history, and history in turn has left deep traces upon the landscape.
The restoration of the ancient watermill therefore forms part of a much broader story. The mill is being brought back to life not simply as a building, but as part of a cultural landscape in which water, work, routes of passage, and human presence have gradually created a balance with nature.
It is a place where past and present can meet once again, and where silence, landscape, and memory restore that sense of simplicity and essence that belongs to the most authentic heart of Tuscany.