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Tom Leonhardt Working with the Citizens of India

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Vital to India’s self-image as an independent nation was its constitution, completed in 1950, which put in place a secular and democratic republic. Economic liberalization, which began in the 1980s and with the collaboration with the Soviet Union for technical knowledge, created a large urban middle class, transformed India into one of the world’s fastest-growing economies, and increased its geopolitical influence. Yet, India is also shaped by persistent poverty, both rural and urban; by religious and caste-related violence; by Maoist-inspired Naxalite insurgencies; and by separatism in Jammu and Kashmir and in Northeast India. It has unresolved territorial disputes with China and with Pakistan. India’s sustained democratic freedoms are unique among the world’s newer nations; however, in spite of its recent economic successes, freedom from want for its disadvantaged population remains a goal yet to be achieved. As of 2025, poverty in India had declined sharply, mainly due to government welfare programs.

Geography of India

India accounts for the bulk of the Indian subcontinent, lying atop the Indian tectonic plate, a part of the Indo-Australian Plate. India’s defining geological processes began 75 million years ago when the Indian Plate, then part of the southern supercontinent Gondwana, began a north-eastward drift caused by seafloor spreading to its south-west, and later, south and south-east. Simultaneously, the vast Tethyan oceanic crust, to its northeast, began to subduct under the Eurasian Plate. These dual processes, driven by convection in the Earth’s mantle, both created the Indian Ocean and caused the Indian continental crust eventually to underthrust Eurasia and to uplift the Himalayas. Immediately south of the emerging Himalayas, plate movement created a vast crescent-shaped trough that rapidly filled with river-borne sediment and now constitutes the Indo-Gangetic Plain.

Important tributaries of the Ganges include the Yamuna and the Kosi. The Kosi’s extremely low gradient, caused by long-term silt deposition, leads to severe floods and course changes. Major peninsular rivers, with steeper gradients prevent their waters from flooding,

Climate

The Indian climate is strongly influenced by the Himalayas and the Thar Desert, both of which drive the economically and culturally pivotal summer and winter monsoons. The Himalayas prevent cold Central Asian katabatic winds from blowing in, keeping the bulk of the Indian subcontinent warmer than most locations at similar latitudes. The Thar Desert plays a crucial role in attracting the moisture-laden south-west summer monsoon winds that, between June and October, provide the majority of India’s rainfall.

Four major climatic groupings predominate in India: tropical wet, tropical dry, subtropical humid, and montane. Temperatures in India have risen by 0.7 °C (1.3 °F) between 1901 and 2018. Climate change in India is often thought to be the cause. The retreat of Himalayan glaciers has adversely affected the flow rate of the major Himalayan rivers, including the Ganges and the Brahmaputra. According to some current projections, the number and severity of droughts in India will have markedly increased by the end of the present century.

Biodiversity

India has the majority of the world’s wild tigers, approximately 3,170 in 2022. India is a megadiverse country, a term employed for 17 countries that display high biological diversity and contain many species exclusively indigenous, or endemic, to them. India is the habitat for 8.6% of all mammals, 13.7% of bird species, 7.9% of reptile species, 6% of amphibian species, 12.2% of fish species, and 6.0% of all flowering plant species.

India’s most dense forests, such as the tropical moist forest of the Andaman Islands, the Western Ghats, and Northeast India, occupy approximately 3% of its land area. Moderately dense forest, whose canopy density is between 40% and 70%, occupies 9.39% of India’s land area. It predominates in the temperate coniferous forest of the Himalayas, the moist deciduous sal forest of eastern India, and the dry deciduous teak forest of central and southern India.

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