Gadag-Betageri | |
|---|---|
| Veeranarayana Temple | |
Interactive map of Gadag-Betageri | |
| Coordinates: 15°25′00″N75°37′00″E / 15.4167°N 75.6167°E | |
| Country | |
| State | Karnataka |
| District | Gadag |
| Government | |
| • Type | City Municipal Council (CMC) |
| • Body | Gadag-Betageri CMC |
| Area | |
| 54.01 km2 (20.85 sq mi) | |
| Elevation | 654 m (2,146 ft) |
| Population (2010) | |
| 172,813 | |
| • Density | 4,657/km2 (12,060/sq mi) |
| • Metro | 367,258 |
| Time zone | UTC+5:30 (IST) |
| PIN | 582 101-103 |
| Telephone code | 08372 |
| ISO 3166 code | IN-KA |
| Vehicle registration | KA-26 |
| Official language | Kannada [1] |
| Website | gadag-betagericity |
Gadag-Betageri is a city municipal council in Gadag district in the state of Karnataka, India. It is the administrative headquarters of Gadag District. The original city of Gadag and its sister city Betageri (or Betgeri) have a combined city administration. The municipality of Gadag-Betageri has a population of 172,813 and an area of 54.0956 km2 (20.8864 sq mi). Kanaginahal of Gadag is the birthplace of the first co-operative society in Asia. [2] [3] The temples of Veera Narayana and Trikuteshwara [4] are places of religious and historic importance.
The Gadag Schist Belt, also known geologically as the Gadag Greenstone Belt, forms a dramatic geological anomaly within the Dharwar Craton of North Karnataka. [5] Dating back 2.5 to 3.0 billion years to the Archean Era, the hills are among the oldest surviving landforms on Earth. Geologically, the region consists of the compressed, metamorphosed remnants of an ancient ocean floor and a submarine volcanic arc.
The foundational terrain is built on metavolcanic rock, originating from submarine volcanism when underwater fissures erupted across a primordial sea floor, cooling into sheets of lava (metabasalts). [6] As tectonic plates collided under extreme heat and pressure, these horizontal layers were buckled and squeezed into near-vertical, wave-like folds known as synclines and anticlines. During this process, superheated hydrothermal fluids were forced through fractures deep within the rock. This intense geological pressure drove quartz veins deep into the schist, leaving behind a heavily metalliferous greenstone bedrock containing massive iron ore deposits and auriferous (gold-bearing) lodes. [7]
The mineralization of the greenstone belt gave rise to the Gadag Gold Field, a historically and economically significant auriferous zone extending over 40 kilometers. Gold is primarily hosted in the structural shears and quartz-carbonate veins that cut through the metavolcanic rocks of the belt. [8] The region features extensive evidence of ancient indigenous gold panning and shallow mining. More intensive, deep-shaft extraction efforts were initiated during the British colonial period in the late 19th and early 20th centuries, with notable historic mining operations centered around villages such as Sangli, and Hosur. [9]
Unlike the tropical rainforests of Dakshina and Uttara Kannada, the hard metavolcanic bedrock of the Gadag Greenstone Belt prevents deep root systems from taking hold, resulting in a treeless, velvet-green high-altitude steppe. Volcanic weathering over millennia has created an exclusive soil chemistry that supports a dense concentration of rare, endemic medicinal plants. [10] The abrupt elevation of the Kappatagudda hill range traps passing moisture and creates a massive natural wind tunnel. These unblocked, high-velocity winds shape the undulating velvet-green grass, drive extensive wind turbine farms, and keep the ambient temperature distinctly cooler than the surrounding arid Deccan plateau.
The topography of the Gadag region features a distinct transition in soil types. While the broader plains of Northern Karnataka are dominated by deep black cotton soils (Vertisols), the elevated areas surrounding the Gadag Schist Belt are heavily characterized by red sandy and loamy soils (Alfisols). [11]
The elevated hills and ridges of the Gadag Schist Belt are covered by red sandy and loamy soils (Alfisols). This red soil is primarily a residual product derived from the extensive weathering of the underlying Archean granites, gneisses, and metalliferous schist. Its prominent reddish hue is a direct result of high concentrations of iron oxides—particularly hematite and limonite—leached into the surface layers. [12] Characterized by a porous, well-drained texture, the soil is structurally aerated but naturally low in organic humus, nitrogen, and phosphorus. Agriculturally, these red soil tracts are optimized for rainfed dryland farming, predominantly supporting crops such as groundnut, sunflower, sorghum (jowar), and various pulses.
In sharp contrast, The broader, flat plains of the district are dominated by deep black cotton soils (Vertisols). Originating from the weathering of ancient basaltic rock, this clay-rich soil is characterized by its high moisture-retention capacity and its tendency to develop deep fissures during dry seasons—a "self-ploughing" trait that naturally aerates the earth. [13] These fertile plains are extensively cultivated for cotton, which thrives in the soil's deep moisture reserves. This geographical advantage historically established Gadag as one of the primary cotton trading sub-hub
The name Gadag is notable for being a palindrome in both the Latin and Kannada scripts. Spelled as G-A-D-A-G in English and ಗದಗ in Kannada, the word reads identically both forwards and backwards. This symmetry extends to the town's major transport hub, Gadag Junction railway station, where its official Indian Railways station code (GDG) forms palindrome. List of palindromic places
The name Gadag is historically derived from ancient Kannada designations found in Chalukya-era inscriptions, where the settlement was variously recorded as Kratuka, Kratapura, Galadugu, and Gadugu.
The Gadag style of Architecture, [14] marked by Ornate pillars with intricate sculpture, [15] originated during the period of the Western Chalukya (or Kalyani Chalukyas) king Someswara I, and it flourished for a period of 150 years (During 1050 CE to 1200 CE) during which period some 50 temples were built; some examples being: The Trikuteshwara temple complex at Gadag, The Kasivisvesvara temple, Lakkundi, The Doddabasappa Temple at Dambal, The Amriteshwara temple at Annigeri, etc.
As of 2011 [update] India census, [18] Gadag-Betageri had a population of 172,813. Males constitute 86,165 of the population and females 86,648. Gadag-Betageri has an average literacy rate of 85.56%. The Sex ratio is about 1006 females per 1000 males to females. 18,419 of the population is under 6 years of age. Kannada is the main and widely spoken language, while English and Hindi are spoken and understood by few people. [17]
Gadag Junction (station code: GDG) is a major railway junction operating under the Hubballidivision of the South Western Railway (SWR) zone. [19] The station falls under NSG-4 Category under Non-Suburban Grade (NSG) classification system and serves as a crucial intersection for three primary lines: routing west towards Hubballi Junction, east towards Hosapete, and north towards Solapur via Vijayapura. [20]
Guntakal-Ballari-Hosapete-Gadag-Hubballi-Vasco da Gama line is freight heavy and connectsSteel plants of Ballari to Marmagao Port [21]
Significant infrastructure upgrades have been completed across the region. This includes 25 kV AC route electrification and extensive track doubling along the Hubballi–Gadag–Hosapetesection and the Gadag–Hotgi line. [22] The junction serves as a scheduled commercial halt for numerous daily express trains and intercity trains. It also has direct train connectivity to majorcities of India like Vasco da Gama, Mangaluru, Bengaluru, Mumbai, Hyderabad, Tirupati, Visakhapatnam, Chennai, Surat, Ahmedabad, Jodhpur, Jaipur, Barmer, Ajmer, New Delhi, Bhubaneswar and Kolkata.
Gadag Bypass Railway Station (station code: GDGB) [23] is a halt station built primarily to allow some of the freight and passenger trains to bypass the main station
Gadag is well-connected to the state and national road networks. National Highway 67 (NH 67) facilitates transit between Hubballi and Hosapete. State Highway 57 (SH 57) and National Highway 48 (NH 48) facilitate transit towards Ranebennur and Bengaluru. [24] National Highway 52 (NH 52) facilitates transit towards Bagalkote and Vijayapura. Public road transport is managed by the North Western Karnataka Road Transport Corporation (NWKRTC), which operates an old and a new central bus stand in the city providing regular inter-city and inter-state bus services.
The nearest commercial aviation facility is Hubballi Airport (IATA: HBX), located approximately 60 kilometers west of Gadag. The airport provides scheduled domestic flight connectivity to major metropolitan cities: Delhi, Bengaluru, Pune, Hyderabad, Mumbai, Chennai and Navi Mumbai. [25]
The closest international airport is Dabolim Goa International Airport (IATA: GOI), located approximately 240 kilometers away.
Kempegowda International Airport (IATA: BLR) is the primary international gateway, located approximately 426 kilometers away.
| Climate data for Gadag (1991–2020, extremes 1932–2020) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °C (°F) | 34.5 (94.1) | 37.7 (99.9) | 40.0 (104.0) | 41.1 (106.0) | 41.7 (107.1) | 40.6 (105.1) | 34.9 (94.8) | 35.4 (95.7) | 37.8 (100.0) | 35.6 (96.1) | 37.2 (99.0) | 34.1 (93.4) | 41.7 (107.1) |
| Mean daily maximum °C (°F) | 30.2 (86.4) | 32.7 (90.9) | 35.7 (96.3) | 37.1 (98.8) | 36.3 (97.3) | 31.0 (87.8) | 28.9 (84.0) | 28.8 (83.8) | 29.8 (85.6) | 30.3 (86.5) | 29.8 (85.6) | 29.2 (84.6) | 31.7 (89.1) |
| Daily mean °C (°F) | 23.2 (73.8) | 25.5 (77.9) | 28.4 (83.1) | 29.6 (85.3) | 28.9 (84.0) | 25.7 (78.3) | 24.6 (76.3) | 24.3 (75.7) | 24.8 (76.6) | 25.2 (77.4) | 24.1 (75.4) | 22.5 (72.5) | 25.6 (78.0) |
| Mean daily minimum °C (°F) | 16.0 (60.8) | 17.9 (64.2) | 20.9 (69.6) | 22.4 (72.3) | 22.4 (72.3) | 21.7 (71.1) | 21.3 (70.3) | 20.9 (69.6) | 20.7 (69.3) | 20.4 (68.7) | 18.2 (64.8) | 15.8 (60.4) | 19.9 (67.8) |
| Record low °C (°F) | 9.6 (49.3) | 11.1 (52.0) | 13.8 (56.8) | 17.2 (63.0) | 17.3 (63.1) | 16.6 (61.9) | 18.5 (65.3) | 18.3 (64.9) | 15.5 (59.9) | 14.2 (57.6) | 10.2 (50.4) | 9.8 (49.6) | 9.6 (49.3) |
| Average rainfall mm (inches) | 0.3 (0.01) | 1.9 (0.07) | 7.3 (0.29) | 39.5 (1.56) | 71.5 (2.81) | 99.6 (3.92) | 77.5 (3.05) | 93.6 (3.69) | 112.9 (4.44) | 123.7 (4.87) | 38.7 (1.52) | 7.2 (0.28) | 673.8 (26.53) |
| Average rainy days | 0.1 | 0.2 | 0.8 | 2.6 | 4.7 | 6.5 | 6.6 | 8.0 | 7.9 | 6.3 | 1.7 | 0.4 | 45.8 |
| Average relative humidity (%) (at 17:30 IST) | 31 | 26 | 22 | 27 | 36 | 63 | 71 | 70 | 63 | 54 | 45 | 38 | 45 |
| Source 1: India Meteorological Department [26] [27] | |||||||||||||
| Source 2: Tokyo Climate Center (mean temperatures 1991–2020) [28] | |||||||||||||
Shri Aluru Venkataraya from Holealur is revered as Karnataka Kulapurohita (High priest of the Kannada family) in the Karnataka region for his contribution towards the cause of a separate Karnataka state. He became famous for undertaking a Karnataka Ekikarana movement in support of the formation of a state for the Kannada-speaking population of Mysore, Bombay Presidency and the Nizam's Hyderabad.
{{cite web}}: Missing or empty |title= (help)