Researchers may have finally cracked why the Indus Valley civilisation collapsed | Current Affairs | Vision IAS

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    Researchers may have finally cracked why the Indus Valley civilisation collapsed

    2 min read

    Indus Valley Civilisation: Urban Planning and Decline

    The Indus Valley Civilisation, at its peak, covered modern-day Pakistan and northwest India. It featured advanced urban planning with gridded streets, multi-storey brick homes, and sophisticated sanitation systems, including flush toilets.

    Causes of Decline

    • Contrary to the belief that a single catastrophic event led to its downfall, recent studies suggest a series of prolonged droughts over centuries as the primary cause.
    • A study published in Communications Earth & Environment used paleoclimate data and computer modeling to analyze climate from 3000 to 1000 BCE.
    • The findings indicate that the downfall of Harappa was due to recurring droughts leading to river and soil desiccation.
    • These droughts, compounded by diminished food supply and fragile governance, pushed the society towards decline.

    Adaptation Strategies

    • The civilisation showed resilience by changing agricultural practices, diversifying trade, and relocating settlements closer to reliable water sources like the Indus River.
    • This adaptability offers lessons on proactive planning and sustainable systems relevant to today's climate change challenges.

    Scientific Analysis

    • The study integrated model outputs with environmental indicators such as stalactites, stalagmites, and lake water levels to understand the factors influencing the civilisation’s decline.
    • Between 3000 and 2475 BCE, a vigorous monsoon facilitated settlement near rain-abundant areas due to cooler tropical Pacific conditions.
    • Warming of the tropical Pacific in subsequent centuries resulted in drier conditions, reduced rainfall, and drought periods.

    Key Drought Events

    • Four major drought events identified between 2425 and 1400 BCE, each lasting over 85 years.
    • The third severe drought around 1733 BCE lasted 164 years, impacting the entire region.
    • Overall temperature increased by 0.5°C, and rainfall decreased by 10%-20%, leading to significant hydrological changes.

    Research Contributions

    • This study advances the understanding of hydroclimate dynamics and their impact on ancient civilisations.
    • The methodology offers insights applicable to other river-dependent cultures like Mesopotamia, Egypt, and China.
    • Understanding tropical Pacific Ocean temperature fluctuations is crucial for future regional rainfall pattern research.
    • Tags :
    • Indus Valley Civilisation
    • Urban Planning
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