Iskitim is a city (since 1938) in the Novosibirsk region of Russia. It is part of the Novosibirsk agglomeration. It is the administrative center of the Iskitim district (not included in it). The city of regional significance, forms the municipal formation of the city of Iskitim with the status of an urban district as the only settlement in its composition. Population - 56,033 people. (2020).
Cultural institutions of Iskitim: houses of culture - Molodist
(Industrial microdistrict), Cementnik (Northern microdistrict),
Oktyabr (in Lozhok microdistrict), RDK im. Leninsky Komsomol
(Central microdistrict), as well as the palace of culture "Russia"
(Southern microdistrict).
Park of culture and recreation
named after I.V. Koroteev and a monument to I.V.Koroteev.
City History and Art Museum
The Iskitim City History and Art
Museum was opened to visitors on November 4, 1977. The museum was
originally formed in two directions and is complex, consists of two
sections: historical and artistic. The museum keeps 24 collections,
more than 19 thousand exhibits. The most ancient are the exhibits of
the paleontological and archaeological collections. The most modern
- materials testifying to the participation of Iskitim in the
Chechen wars.
Storage units: 19 839, of which items of the
main fund: 17 648, including: ethnographic collection - 1759 units,
icon collection - 200 units, numismatics collection - 3898 units,
natural history collection - 563 units, photos and documents from
the collection “V. M. Shukshin. Life and Creativity "- 250 units.
Museum of Memory of Victims of Political Repression
The
museum was opened on May 3, 2019 in the Lozhok microdistrict in the
basement of the church in honor of the New Martyrs and Confessors of
the Russian Church, built on the site where in the Soviet years,
from 1929 to 1956, the Special Camp No. 4 Siblag was located.
According to various estimates, about 30 thousand people were killed
in this camp, whose corpses were buried in common pits, burned in
industrial zone furnaces or simply thrown into the forest. In five
museum halls, documents and personal belongings of Siblag prisoners,
miraculously preserved photographs, prisoners' tools are displayed.
In one of the rooms of the museum, the isolation cell was
reconstructed.
According to one of the numerous etymological versions, the name "Iskitim" is considered to be derived from the ethnonym "Askishtim (Ashkitim, Azkeshtim)" - an ancient tribal group of Teleuts of the steppe Turks living in the area, and translated from Turkic means "pit" or "bowl". Indeed, the city is actually located in a basin. This nomadic people came to southern Siberia (and, in particular, to the Ob region) in the 15th-17th centuries. within the boundaries of the Oirat Khanate (Turkic-speaking peoples). At the same time, they ousted the Finno-Ugric peoples who previously lived here. The population density in Western Siberia in the Middle Ages was extremely small and the total number of Teleuts by the 17th century in the Upper Ob region and in the foothills of Altai was only a few thousand people. In the next two centuries, the Russian Cossacks and the Russian peasantry became the dominant population.
Pre-Russian Era and Early Russian Settlement (Pre-1717 to Late 19th
Century)
Before Russian arrival, the region had low population
density and was home to small groups of Teleuts. In the early 18th
century, following the construction of the Tomsk Ostrog in 1604, Russian
Cossacks built a chain of defensive outposts (ostrogs) and barricades
(zaseki) against Jungar and Kyrgyz threats. One such forward post was
near modern Berdsk.
The first documented Russian settlements on the
site of future Iskitim appeared in the 1717 census: the villages of
Koynovo (the largest, known for craftsmen), Shipunovo (a Cossack
military outpost for patrols and alerts), Chernodyrovo (later
Chernorechka/Black River, named after the local river later renamed in
Soviet times), and Vylkovo (documented around 1719). These were founded
by state peasants and free colonists engaged in farming, gardening,
hunting, fishing, and small crafts. Koynovo featured mills, an oil
press, tannery, felt-boot and rope workshops, shops, and a church (later
dismantled due to flooding). A staging prison for convicts en route to
Altai mines also existed there. Chernorechka had handicraft workshops
and a primary school; a small lime-burning factory was added by a
Barnaul merchant in 1911. Shipunovo served as a forward guard post.
Administratively, the area belonged to Koynovskaya Volost in Barnaul
Uyezd, Tomsk Governorate (later Altai Governorate). The 19th century saw
modest growth thanks to the Barnaul Trakt (a major road) and small-scale
limestone quarrying by local merchants starting in the late 1800s. The
villages remained rural and agricultural.
Early 20th Century:
Railway and Revolutionary Period (1900s–1920s)
The Altai Railway
(connecting Barnaul and Novo-Nikolaevsk/Novosibirsk) was built between
1912 and 1916, with a small halt (later Iskitim station) appearing near
the future town site. This improved connectivity but did not transform
the villages dramatically. Administrative shifts occurred amid
revolution and Civil War: the territory moved between various uyezds,
governorates, and districts (e.g., briefly abolished and restored
volosts under Kolchak and Soviet authorities). A local Bolshevik figure,
Afanasy Skorokhodov (a wounded Baltic Fleet sailor), briefly led the
volost soviet before and after the Civil War.
Soviet
Industrialization and the Birth of the Modern City (1929–1930s)
Iskitim’s “second birth” as an industrial town came with Soviet forced
industrialization. In 1929, geologists discovered major deposits of
limestone and clayey shale (ideal for cement). Construction of the
Chernorechensky Cement Plant (later Iskitimtsement, Siberia’s largest at
the time) began around 1930–1931 and became operational by 1934.
The
plant’s construction relied heavily on forced labor from the Gulag
system. The Iskitimsky Lagernyy Punkt (OLP-4), part of Siblag (Siberian
Camp Administration under OGPU/NKVD), was established in the early 1930s
in the Lozhok (Lozhki) microdistrict on the town’s outskirts. This
notorious “penal” or “katorzhnyy” (hard-labor) camp—often called one of
the harshest in the USSR or a “camp of death”—operated until 1955–1956.
Prisoners (politicals including clergy, pre-revolutionary officials,
Trotskyists, and common criminals) endured brutal conditions in
quarries: manual stone drilling (1,600 strikes per meter, daily norms of
5 meters per team), lime burning in massive bonfire furnaces, loading
5-ton quotas by hand, and work in extreme cold (down to -43°C in the
deep quarry). Mortality was high from silicosis (lime dust destroying
lungs), exhaustion, starvation, pellagra, and disease; rations were
withheld from those failing norms. Escapes were punished by execution.
The camp had separate zones for politicals, criminals, and women. It
supplied lime and stone for the cement plant and other industries (e.g.,
Kemerovo fertilizer plant). Estimates suggest tens of thousands passed
through, with high death rates. The camp was razed after closure to
erase traces.
On April 10, 1933, a workers’ settlement named Iskitim
was officially formed by merging the four old villages (Koynovo,
Chernorechka, Shipunovo, Vylkovo) with the adjacent Gulag territory.
Iskitimsky District was created in 1935, with the settlement as its
center. In 1938, Iskitim received city status (initially district
subordination). Population grew rapidly from the villages’ modest size
to around 14,000 by 1939 as workers (free and forced) arrived.
World War II and Post-War Growth (1940s–1980s)
During the Great
Patriotic War (1941–1945), over 16,000 Iskitim residents went to the
front; many did not return. Women replaced men in factories and farms.
The district overfulfilled grain and meat quotas, collected funds for
defense (e.g., for aircraft named “Iskitimsky Promkooperator”), and
hosted evacuated hospitals and equipment from occupied regions. New
enterprises like an oil-pressing plant emerged. Post-war, Iskitim gained
oblast subordination status in 1951. Industrial expansion continued in
construction materials (cement, lime, gravel, reinforced concrete).
Population reached ~34,000 by 1959.
Infrastructure grew: schools,
hospitals, a city garden (1930s), and cultural facilities. City Day was
established in 1987 on Builder’s Day (August), reflecting the town’s
industrial identity. Population peaked above 69,000 in the late Soviet
period. The economy centered on building materials, with some
diversification (e.g., later defense-related plants).
Post-Soviet
Era and Modern Times (1990s–Present)
The 1990s brought economic
challenges and population decline as industries restructured. In 1994, a
section of the city cemetery was designated for victims of Soviet
political repression, with a commemorative cross installed. The former
Gulag site in Lozhok has become a site of memory and faith: the Holy
Spring (Svyatoi Klyuch) is revered as sacred, linked to legends of
executions of around 40 monks and priests by camp guards (though exact
details blend with broader repressions). A memorial park and Church of
the Russian New Martyrs and Confessors were built and consecrated in
2006. It is now a regional pilgrimage site for healing and remembrance
of Gulag victims.
Incidents like mass arson of Roma (Gypsy) homes
occurred in 2004–2005. Today, Iskitim remains an industrial town within
the Novosibirsk agglomeration, with cement production as its economic
backbone alongside other manufacturing. It has a local history and art
museum highlighting regional history, WWII heroes (12 Heroes of the
Soviet Union from the Iskitim area), and cultural life. The town faces
typical Siberian challenges like depopulation but maintains its identity
as a “city born twice”—once in 1717 as villages, and again in the 1930s
through Soviet industrialization.
Regional Setting and Broader Context
Iskitim lies in the
southeastern portion of the vast West Siberian Plain, one of the world’s
largest continuous flatlands. This plain stretches between the Ural
Mountains to the west and the Yenisei River to the east, covering
roughly 2.6–2.7 million km² of extremely flat, low-lying terrain formed
primarily by Cenozoic alluvial deposits. Most of the plain sits below
100 m elevation, with poor drainage leading to extensive swamps, lakes,
and seasonal flooding in northern areas.
Novosibirsk Oblast itself
occupies the southern part of this plain, at the foothills of the low
Salair Ridge (a northwestern extension of the Altai Mountains). The
oblast features a transition from taiga and wetlands in the north to
forest-steppe and steppe in the south, drained mainly by the Ob River
and its tributaries (including the Berd). Iskitim is positioned in the
forest-steppe zone, roughly 50–65 km south of Novosibirsk, near the
southern edge of the Novosibirsk agglomeration.
The town serves as
the administrative center of Iskitimsky District (area 4,384 km²),
though it is incorporated separately as the Town of Iskitim (an urban
okrug). The district lies in the eastern part of Novosibirsk Oblast.
Local Topography and Terrain
Iskitim occupies a relatively
low-lying, amphitheater- or basin-like setting along the Berd River
valley. The immediate area consists of:
A low alluvial plain along
the river (elevations around 113–120 m).
Surrounding higher,
dissected plains and low hills that rise to 175–179 m.
This
creates a gentle “bowl” effect. The eastern side features the
Bugotakskaya hilly plain with pine forests, while the west and south
transition into the flatter Cherepanovskaya plain. The terrain reflects
transitional tectonics near the Kolyvan-Tomsk fold zone, with some
gentle relief from glacial and alluvial processes rather than dramatic
mountains. Pleistocene loess-soil sections are notable in the area.
Overall, the landscape remains characteristically flat and open, typical
of the West Siberian Plain, with subtle riverine features, occasional
low ridges, and patches of forest.
Hydrology: The Berd River and
Novosibirsk Reservoir
The defining geographic feature is the Berd
River, a right tributary of the Ob River (length ~363 km, originating in
the Salair Ridge). Iskitim developed directly on its banks. The lower
course of the Berd was significantly altered by the construction of the
Novosibirsk Hydroelectric Dam on the Ob River, which created the large
Novosibirsk Reservoir. This reservoir submerged about 40 km of the
original lower Berd channel. The Berd now empties into the reservoir,
and the town lies near this confluence zone.
The river provides water
resources and historically influenced settlement and industry. Smaller
tributaries like the Koyon River are also present in the district.
Low-lying areas along the rivers include some bogs and flood-prone zones
typical of the plain’s poor drainage.
Climate
Iskitim has a
moderately continental climate (Köppen Dfb or similar), shaped by its
inland position on the West Siberian Plain. Key characteristics include:
Long, cold winters: January average around –19°C, with daily highs often
near –12°C (10°F) and frequent overcast conditions. Extreme lows can
reach –50°C.
Short, warm-to-hot summers: July average around
+18.5–19°C, with highs reaching the low 20s°C (and occasional extremes
up to +40°C).
Large annual temperature amplitude due to the
continental interior.
Precipitation: Around 450 mm annually, with a
pronounced summer maximum (rainy period roughly April–November). Winters
are drier, with snow cover.
Other factors: Prevailing southwest
winds; the basin-like topography can limit airflow and contribute to
temperature inversions or stagnant air in summer.
The climate
supports agriculture in the forest-steppe but brings challenges like
heavy snowfall and spring flooding.
Vegetation and Natural
Environment
The surrounding region belongs to the forest-steppe zone:
a mosaic of open grasslands, birch groves, and patches of coniferous
(especially pine) forest, particularly to the east on the Bugotakskaya
hills. Northern parts of the oblast have more taiga and marshes, while
southern areas trend toward true steppe. The plain’s flatness and
variable drainage create wetlands, meadows, and wooded areas. Local
mineral deposits (limestone, shale) have shaped human activity more than
the vegetation itself.