Indo-Gangetic Plain
The Indo-Gangetic Plain is a vast low-lying region in South Asia that stretches over 2,400 kilometers from the Sutlej River in the west to the Ganges delta in the east, encompassing parts of northern India, Pakistan, and Bangladesh. Situated at the southern foothills of the Himalayas, the plains are characterized by extensive floodplains formed by the confluence of major rivers, including the Indus, Ganges, and Brahmaputra. This area's fertile alluvial soil, enriched by regular flooding, supports a rich agricultural tradition, making it one of the most densely populated and agriculturally productive regions in the world.
Farmers in the Indo-Gangetic Plain primarily cultivate wheat, utilizing the region's advantageous geography and seasonal rainfall patterns. However, the reliance on inorganic fertilizers and limited tillage practices can lead to soil depletion over time. Culturally and geographically diverse, the plains also feature contrasts between fertile areas and arid desert regions, particularly in the Punjab area, which can impact agricultural practices. Overall, the Indo-Gangetic Plain remains vital for the livelihoods of millions, showcasing a complex interplay of geography, agriculture, and human settlement.
Indo-Gangetic Plain
The Indo-Gangetic Plains lie in South Asia at the southern foot of the Himalayan Mountains. They extend more than 2,400 kilometers from the Sutlej River in the west, near the Pakistan-India border, to the Ganges delta in the east, within the territories of India's West Bengal and Bangladesh. The numerous rivers that run through this large, flat expanse of land has made much of the Indo-Gangetic Plains a floodplain. This low-lying area is often subjected to flooding from nearby sources of water. Nevertheless, the Indo-Gangetic Plains' proximity to these rivers has allowed the region to thrive as a successful center of agricultural productivity.
Geography of the Plains
The geographic location of the Indo-Gangetic Plains is the main reason they have become a floodplain. The plains are an extensive stretch of flat land that lies at the foot of the Himalayan mountain range, with the Indian subcontinent to the south. Three main rivers course through the plains: the Indus, Ganges, and Brahmaputra, all of which begin high in the Himalayas. This means that the annual transition from winter to spring causes the mountain snow to melt rapidly and swell all three rivers at the same time. When the engorged rivers reach the Indo-Gangetic Plains, they merge with numerous tributaries that only add to the inevitable flooding of the flatlands.
But aside from being a quintessential floodplain, the Indo-Gangetic Plains are also classified as alluvial plains, part of an alluvial system. These plains are created when rivers that descend steep mountainsides level off onto flatlands and spread out their alluvium sediment, which consists of gravel, silt, sand, and clay. Because of this regular flooding and the continual buildup of alluvial soil, the Indo-Gangetic Plains have a rich agricultural tradition.
Farming on the Plains
At 2,400 kilometers long and ranging from 240 to 320 kilometers wide, the Indo-Gangetic Plains are one of the most heavily populated regions in the world. From their western limit in the Sind region of Pakistan, across the northern Indian states of Uttar Pradesh, Bihar, and West Bengal to their eastern boundary in Bangladesh, the plains are home to millions of farmers who utilize the region's advantageous geography to engage in heavy wheat cropping. The plains' soil is strong and fertile, and the waters from the flooding rivers drain extremely slowly due to the almost complete flatness of the area—the land elevation drops by only two hundred meters until the waters empty into the Ganges delta. The moisture in the soil assists in the irrigation of the crops.
The Indo-Gangetic Plains are divided into three main zones of wheat cropping: the Indus Plains in eastern Pakistan and northwestern India, the Trans-Gangetic Plains in north-central India, and the Upper-Gangetic Plains in northeastern India near the Ganges delta. While the Ganges River valley in Uttar Pradesh is India's most populous region, the upper Indus River valley is among the most agriculturally fruitful areas on the entire Asian continent. Wheat farmers in all these regions follow a seasonal schedule, so their efforts yield the best results.
They usually plant wheat in the early winter month of November. The moisture stored in the soil from the previous season keeps the seeds alive until the rains come or the rivers flood. The rainy season in these northern regions of India lasts until about April. But during this time, only two hundred to three hundred millimeters of rain might fall on these crops, which require about six hundred millimeters of water to grow. This is especially troublesome if the next river flooding is not due for some time.
To combat this water deficiency, farmers rely on inorganic fertilizers to enrich their soil since they practice only limited forms of tillage and nutrient assimilation procedures. In spite of this, farmers can only plant in one region of the plains for so long. This is because the richness of even the fertile alluvial soil declines slightly after each season until the ground becomes barren.
Geographic Diversity
While most of the Indo-Gangetic Plains is composed of this wet and bountiful farmland, the plains' western limits, which cover parts of India and Pakistan, are a mix of fertile floodplain and arid desert. This area is known as the Punjab region. The Pakistani Punjab region includes the heavily irrigated upper Sind Plain as well as the 260,000-square-kilometer Thar Desert, created from a combination of the region's naturally arid climate and the relentless sand deposits carried by the wind.
These adjacent yet differing environments can also be found across the Pakistani border in northwestern India's portion of the Indo-Gangetic Plains. The northern part of the Indian state of Gujarat, for example, is home to the standard type of Indo-Gangetic alluvial floodplain. However, the peninsula of southern Gujarat is made up mostly of rolling hills. These were created millions of years ago by the movement of tectonic plates, large pieces of rock in Earth's crust that, over a long period, grind together and can force flat land up into mountains. While the desert parts of the Indo-Gangetic Plains are sparsely populated and infertile, the expansive floodplains continue to provide homes and livelihoods for millions of Pakistani, Indian, and Bengali farmers.
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