Divnogorye, Russia

Divnogorye

 

Description of Divnogorye

Divnogorye or Divnogorie is located in the Voronezh region, 130 km from the regional center and 12 km from Liski. Divnogorye - Cretaceous plateau, towering tens of meters above the surrounding forest-steppe. The name of the area received from the "divs" - chalk pillars and remnants of geologic formations that formed on the bottom of ancient seas that once covered this area. In 1991, the territory of the plateau received the status of a museum-reserve.

Unusual chalk formation, magnificent views of the Don and Silent Pine that flow down below, rare for Russia monasteries and churches make Divnogorye one of the most interesting sights of the region. The best time to visit is from May to September, in dry weather.

1 Reserve administration, Divnogorye farm. ☎ +7 (47391) 2-12-17, 5-91-11. Opening hours: 10: 00—18: 00 from April 25 to November 10, excursions every two hours from 10:00 to 16:00. Mondays and Tuesdays are weekends; the cave church and the entire infrastructure are closed.

 

Characteristic

The area of the museum-reserve is more than 11 km². From a geological point of view, the reserve is an outcrop of Cretaceous deposits on the surface of the earth. The maximum height of the plateau above sea level reaches 181 meters, relative - 103 meters (the mouth of the Quiet Pine River, which flows at the foot of the plateau, at the confluence with the Don is located at an altitude of 78 m above sea level). Due to a rather significant difference in height between the plateau and the floodplain of the Don and Tikhaya Sosna rivers, its microclimate differs significantly from the surrounding floodplain lowland. The elevated, dry surface of the plateau heats up quickly. Rising hot air streams drive away the emerging thunderclouds towards low floodplain lands. As a result, the already small average annual precipitation in the region (on average 480 mm per year) over the plateau is reduced by 1.5-2 times. The summer period is especially dry. This slows down the process of water erosion, and also reduces the likelihood of karst failures. There are voids inside the chalk layer and are detected in the following way: when passing over its surface, human steps emit a kind of rumble. The top layer consists of 15-20% chalk. Below 80 centimeters there is a layer of pure chalk. The top layer is exposed to wind erosion (weathering). Despite the rather steep slopes, the plateau has undergone anthropogenic changes: in 1860 part of it was blown up with dynamite to build a railway. In addition, the activity of sheep farms and vandalism caused great harm to the reserve.

 

Flora and fauna

The territory of the reserve is located on the outskirts of the northern steppe zone and differs from the forest-steppe region of Voronezh. For a long time, the plateau and its slopes were used by sheep farms, due to which a significant part of the steppe vegetation underwent severe degradation. In 2013, thanks to the cessation of grazing and the regulation of human presence, the steppe vegetation on most of the plateau has been restored to its original form. More than 250 species of xerophytic and petrophytic plants grow on the plateau, such as: feather grass, drooping sage, cretaceous thyme, multi-colored elm, oriental cornflower, two-spike ephedra, siverekia podolskaya, whole-leaved clematis, meadow lumbago, protozoan osma, dwarf iris and leafless iris, anemone forest, adonis spring. Almost 40% of the plant species of Divnogorye are classified by botanists as calcephytes (that is, "melolyubov"). Cretaceous outcrops in the south of the Russian Plain are endemic to the Kozo-Polyansky bulrush and some other species. On the surface of the plateau, there is also a peculiar gelatinous lichen from the genus collema, which dries up in dry weather and swells in wet weather. Occasionally on the territory of the reserve there are bustards and golden eagles listed in the Red Book. Bee-eaters and eagle owls are more widespread. Of the mammals, hares and foxes are common. Bats live in crevices. The entomological fauna is rich, among which the most common are: bumblebees, dragonflies, wasps, dybki, stag beetles, redheads, swallowtails. In 1956, on the initiative of I.V. Stalin, but after his death, a forest protection strip of maple and ash trees was created in the central part of the plateau. Due to the characteristics of the chalky soil and the lack of moisture, many trees still appear young even after almost six decades since planting.

 

Attractions and visit

Chalk pillars divas. Cretaceous remains, which gave the name of the area, are located in different parts of the reserve:
1  Big divas. located in the administration area and about. settlement Divnogorskaya, hanging over the valley of Quiet Pine;
2  Small divas. are located on the territory of the Divnogorsky monastery in the northern part of the reserve. The chalk plateau rises above the monastery: a steep path leads to the top, and from above there is a magnificent view of the mouth of the Silent Pine. More relics have been preserved here than in Bolshiye Divy, including the ring rock, and the chalk mountain as a whole looks more preserved.
3  Lonely diva. in the dry ravine, in the eastern part of the reserve. There is no road to it, not even a path, you have to go straight across the steppe. If you go strictly to the south from the archaeological park, you can pass by the diva and go to the dirt road to the village of Divnogorie.

It is forbidden to climb the Big Divas; A steep path leads to the Small Divas.
4 Church of the Sicilian Icon of the Mother of God (XVII century). adults - 250 rubles, schoolchildren and students - 125 rubles. (July 2017). A steep staircase leads up to the plateau from the train platform, ending at the entrance to the cave church - the main attraction of the reserve. Entrance to the church is allowed only as part of excursion groups departing from the foot of the stairs every two hours. The church belongs to the reserve, and divine services are held only twice a year. The two-story church and utility rooms were hollowed out in the chalk according to the traditions of Athos monks in the middle of the 17th century, approximately at the same time as the Divnogorsky monastery was founded. The temple was consecrated in honor of the Sicilian icon of the Mother of God, according to legend, belonged to Sophia Paleolog. In the temple there is a list made about 100 years ago from the original icon (it was restored in 2010), the location of the original is unknown. A feature of the cave temple is a narrow corridor of almost a hundred meters in length around the main hall, which was previously used for religious procession, and now is a habitat for butterflies. There is no artificial lighting in the temple, but you will be given a church candle. In front of the entrance there is an observation deck with an excellent view of Quiet Pine.
5  Mayatskoe settlement. From the church to the north stretches a small area of the recreated steppe, along which footpaths are laid. They lead to the remains of a settlement (VIII-X centuries), an outpost of the Khazar Khaganate in the north. The rectangular settlement was a chalk fortress surrounded by 6-meter ramparts. The fortress has not yet been excavated, but the ramparts are clearly visible around the perimeter. The archaeological culture of the settlement is called Mayatskaya, as it is believed that the white-stone fortress on the highest point of the plateau was an excellent landmark (beacon) for the entire region. If you carefully look under your feet, it is easy to find fragments of ceramics on the territory of the ancient settlement. Near the settlement there is one of the best viewing platforms overlooking the Pine, Don and Zadonye.
6 Chalk Canyon. From the Mayatsky settlement, past the forest plantation, the path leads to a deep chalk ravine of a bizarre shape. The picturesque canyon is a popular spot for photography, especially at sunset when the setting sun gives the chalk a pinkish tint. There are many nests of burrowing birds on the walls of the ravine.
7  Archaeological park "From camps to cities". Tourist groups do not lead to the central part of the protected area, and paved paths are replaced by unpaved ones. Behind the chalk canyon is a recreated settlement of the Mayak culture: dugouts and adobe huts resembling yurts.
8  Geological exposition. In a forest plantation next to the archaeological park, there are stone slabs illustrating different geological periods. There are no signs and pointers here, and in general, the exposition looks neglected.
9th Divnogorsky Holy Dormition Monastery (next to the Divnogorskaya platform). In the northern part of the reserve there is a monastery with another cave temple and a second group of remains - small Divas. The territory of the monastery is no less picturesque than Big Divas, and is included in the “obligatory program” of visiting the reserve.
From the administration of the reserve, you can walk to the monastery along the railway (about 3 km) - the shortest, but the most uninteresting path, or along the top, past the archaeological park (a dirt road starts from the park, connecting the Divnogorie farm and the monastery directly). The monastery can also be reached by car on an asphalt road around the chalk plateau.

It is believed that the monastery was founded in 1640 by the monks Xenophon and Joasaph from the Kiev-Pechersk Lavra, who carved cells and a temple in chalk. The monastery has been closed several times and its artificial structures are of no interest, although it is possible that it was this lack of development that allowed the preservation of the chalk mountains surrounding the monastery.
10 Cave Church of John the Baptist (XVII-XIX centuries). In the chalk column at a height of about 80 meters is the entrance to the cave church. It is very similar to the Church of the Sicilian Icon, but is not a museum object, but part of a monastery, and therefore looks a bit run down. From the lowland, where the monastery buildings are located, a staircase leads to the entrance to the temple. Entrance is allowed only as part of organized groups: excursions can be arranged in the monastery, but there are no regular excursions with a fixed start time. Divine services in the church are also conducted irregularly.
11 Casemate and Ear Caves. In the extreme north-eastern corner of the protected area, between the monastery and the village of Selyavnoye, two narrow caves were carved in the chalk plateau: they gave an excellent overview of the Don valley and the opportunity to monitor the enemy. A hermit monk once lived here, carving niches for icons and lamps in the chalk walls.
12  Reconstruction of the Ukrainian courtyard. A stylized Ukrainian estate (many Ukrainians have always lived in the Voronezh region), which houses the ethnographic collection of the museum-reserve. The exposition is extremely meager - spinning wheels, towels, rural utensils - and only children may like it.
13  C the holy spring. The spring from which the ministers of the Church of the Sicilian Icon took water. The water is very hard, and its compliance with sanitary standards is unknown.

 

In fiction

In Vladimir Sorokin's story "The Day of the Oprichnik", the estate of Prince Urusov is located in Divnogorie.

 

How to get here

How to get there
Most ways to get to Divnogorye involve transit through the city of Liski, a major railway junction in the immediate vicinity of the M4 highway. Ostrogozhsk is also relatively close, the city is somewhat more interesting than Liski, but much less accessible by transport.

By train
Divnogorie is served by two train stations on the Liski-Ostrogozhsk-Valuiki line.

1  o. settlement Divnogorskaya. near the monastery.
2  o. n. 143 km. near the administration of the reserve.

From Liski, three electric trains a day (direction to Ostrogozhsk or Alekseevka) allow you to leave in the morning and return not late in the evening. The same electric trains run from Ostrogozhsk, but their schedule is not very convenient. Travel time from both Liski and Ostrogozhsk is about half an hour. On some summer weekends, direct express trains from Voronezh are scheduled in Divnogorye, the journey takes a little more than two hours.

Both stations are half-stations with no infrastructure other than a shelter the size of a bus stop. Tickets must be taken from the traveling cashier on the train (but in Liski or Ostrogozhsk, in turn, at the box office at the station).

The railway itself goes right at the foot of the chalk hills and is very picturesque, although the floodplain of the rivers is often blocked by trees.

By bus
There is a bus from Liski twice a day (in the middle of the day). It is not very convenient, as it takes 1 hour 15 minutes (in the opposite direction a little faster), and its stop is located about 2 km from the reserve. However, if the seven-hour interval between trains is inconvenient for you, you can come to Divnogorie by train and leave by bus, or vice versa.

By car
A dead-end local road leads to Divnogorye (however, of good quality): the distance from Liski is about 40 km, from Ostrogozhsk - about 50 km. From Liski, in the village of Pukhovo, without crossing the railway crossing, turn towards Kovalev; however, it is difficult to get lost, as there are signs to Divnogorye at all the forks. A little further from the administration of the reserve is free parking.

A separate road leads to the monastery (and the northern part of the reserve) through the village of Selyavnoe. The car will have to be left on the paved parking lot at the top of the hill, from which the monastery is still about 800 meters away.

From the direction of Voronezh and Ostrogozhsk, navigators often show a shorter route to Divnogorye, but roads of unclear quality, among which there are unpaved ones. It is better to choose the path described above, and if you are still attracted to others, you should find out in advance about their condition.