Don't Miss Out These 5 Ultimate Wildlife Safari Experience Close To Hyderabad
1. Nehru Zoological Park
The Nehru Zoological Park functions as an exceptional wildlife starting point because it occupies a position 15 kilometers outside Hyderabad city amongst India's biggest zoological institutions. The park features 380 acres of land where visitors can see all the more than 100 species of animals and birds and reptiles. People can observe the natural nighttime activities of civets and owls along with bats under nocturnal lighting at this location. The park provides visitors with two ways to experience its abundant wildlife through open-air enclosures for a semi-natural encounter with lions and tigers as well as deer and bears while the nocturnal animal house gives visitors unique daytime viewing of owls and bats and civets.
2. Mahavir Harina Vanasthali National Park
At 15 kilometers from Hyderabad Mahavir Harina Vanasthali National Park takes its name from Lord Mahavira who served as the 24th Tirthankara of Jainism. The 14 square kilometer sanctuary exists for blackbuck protection being an endangered Indian antelope species. Wild boars together with porcupines and monitor lizards share this habitat with several bird species in addition to other mammals. Jeep safari excursions enable tourists to observe wildlife within dry deciduous forests and grasslands while providing them with an exciting spotting opportunity.
3. Mrugavani National Park
Mrugavani National Park rests approximately 25 kilometers south of Hyderabad and includes a total 3.5 square kilometer space that attracts nature enthusiasts and birdwatchers. The small park encompasses more than 250 bird species and over 600 plant species within its grounds. The park supports the natural habitats of spotted deer and jackals together with junglefowl and partridges and peacocks. Visitors can access various pathways and jeep journeys that let them easily discover the peaceful beauty of this underrated park.
4. KBR National Park
Near the center of Hyderabad stands the Kasu Brahmananda Reddy (KBR) National Park as an exceptional urban conservation area. A haven of 1.6 square kilometers sets itself as a peaceful sanctuary when surrounded by urban noise. Multiple bird species together with butterflies and small forest mammals inhabit this area because of its dense vegetation and water resources and walking options. KBR Park provides visitors the chance to see wildlife while strolling through the park because you can capture photos and observe park inhabitants without leaving central Hyderabad.
5. Shamirpet Deer Park
Shamirpet Deer Park provides an entertaining wildlife encounter suitable for family vacationers who want rested yet active times. The park, maintained approximately 27 kilometers north of Hyderabad, protects Indian spotted deer among other herbivores in a guarded natural space. The pathways accessible to visitors allow them to walk while observing deer as they feed peacefully and jeep rides provide an additional viewing option. The beauty of Shamirpet Lake complements this place by providing both boating services and peaceful sites for picnics while visitors enjoy scenic views.
Conclusion
Visitors seeking relief from busy urban environments should visit the wildlife areas and parks around Hyderabad. All nature enthusiasts will find satisfying explorations because the parks offer magnificent large-cat observation together with rare bird watching experiences and peaceful natural exploration activities. The wildlife sanctuary series in Nehru Zoological Park serves visitors while Pocharam Wildlife Sanctuary maintains its untouched state to present unique encounters to nature lovers. Experience the unmatched wildlife safari getaway close to Hyderabad while you bring your field glasses and camera equipment. The visits to these amazing locations provide you with the chance to observe India's diverse natural habitats as you join in preserving those essential ecosystems for the benefit of generations to come.
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The quake occurred along the boundary where the Indian and Eurasian Plates collided, near the eastern terminus of the Himalayas, at a depth of 15 km. The rupture extended from the Mishmi thrust of the Eastern Himalayas to the Himalayan Frontal Thrust of Arunachal Pradesh, completing a curvilinear motion around the mountainous bend (see image above). As it happened, the shaking also occurred at a time when seismographic networks were expanding worldwide, providing great impetus to earthquake monitoring and the subsequent development of the theory of plate tectonics. It was also the time instrumental monitoring of earthquakes had started in India, with the India Meteorological Department (IMD) setting up its first seismological observatory at Alipore in Kolkata district in 1898. Today, we understand the Great Assam Earthquake happened on a plate boundary formed by the collision of continental plates, like those along other parts of the Himalayan plate boundary. However, it is differentiated by the fact that its source was in the Eastern Himalaya, which is tectonically very complex. GPS data indicate that while Indian and Eurasian continental plates are converging at about 20 mm/year on average across the Himalayas, in the Eastern Himalayas it ranges from 10 mm to 38 mm/year. This variation could very well be due to difficulties in capturing tectonic complexity and differences in data quality. While the main arcuate Himalaya plate boundary resulted from the collision of the Indian and Eurasian plates, the Sunda plate is also involved in the northeastern Himalaya, creating a complex structure. Due to plate rotation, major structural elements also take sharp turns and the regional strike shifts from the general NE-SW direction to the NW-SE direction post-collision, forming what geologists call the Eastern Himalayan Syntaxis (EHS). This is where the Great Assam Earthquake likely occurred. Unlike other Himalayan earthquakes, which have exhibited a thrusting mechanism — where one block of the fault thrusts over the other — the Assam earthquake displayed a component of strike-slip motion, with both blocks sliding past each other along the fault. This suggested it was connected with the EHS trending in the NW-SE direction. Models also indicate a thrusting component, likely resulting from the propagation of earthquake faulting towards the west, where thrust tectonics are predominant. The possibility of multiple faults being linked to the Assam earthquake is also supported by the distribution of revised aftershock locations, spread over a wide zone east of the main shock epicentre. Indeed, most researchers believe the earthquake may have started off on the Syntaxial bend while also activating Himalayan thrust faults to the west. Historical documents from the Ahom period (1228-1826) reveal the Northeast India region experienced earthquakes in 1548, 1596, and 1697 AD, all of uncertain magnitudes. Geological studies have also revealed a major medieval earthquake between 1262 and 1635 AD. Quakes of the future Looking back, the Great Assam Earthquake delivered to scientists a significant lesson on the destructive potential of major earthquakes in the Himalayas. Can a similar earthquake strike Northeast India again? As the Indian plate continues to move forward, earthquakes are an integral part of its future. Yet our current knowledge doesn't allow us to predict when, where or how strong the next quake will be. For now, we only know the Central Himalayas are the most potentially active segment and could generate a 1950-type earthquake in future. The seismic event also highlighted that we are more vulnerable today, primarily due to the exponential growth of the built environment and urban areas, leaving the landscape to look very different from the way it did 75 years ago. As we plan for more developmental activities and undertake heavy infrastructural projects, including large dams, in this tectonically fragile area, we must reflect on the images from the 1950 quake. Finally, the event also proved the Himalayan tectonic segments along the 2500-km-long stretch are fully capable of producing earthquakes of magnitude 8.6 or higher. As both China and India prepare to build large hydroelectric projects in the Eastern Himalayan bend, one of the most seismically vulnerable parts of the majestic range, it's clear the road ahead will be long and challenging. Kusala Rajendran is a former professor at the Centre for Earth Sciences, Indian Institute of Science, Bengaluru. C.P. Rajendran is an adjunct professor at the National Institute of Advanced Sciences, Bengaluru.
