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History of Goa

  • 39 min read
  • 7 chapters
Ellora is a UNESCO World Heritage Site located in the Aurangabad district of Maharashtra, India. It is one of the largest rock-cut monastery-temple cave complexes in the world, featuring Hindu, Buddhi
Shivajidesai29 · CC BY-SA 4.0

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Through History of India, Colonial India and Mesolithic

The Usgalimal rock engravings, belonging to the Upper Paleolithic or Mesolithic periods, exhibit some of the earliest traces of human settlement in India. The Mauryan and Satavahana Empires ruled modern-day Goa during the Iron Age. It was ruled by the Kadambha dynasty from the 2nd century CE to 1312 and by the Deccan from 1312 to 1367. The city was then annexed by the Kingdom of Vijayanagara and was later conquered by the Bahmanī sultanate, which founded Old Goa on the island in 1440.

The Portuguese invaded Goa in 1510, defeated the Bijapur Sultanate. The Portuguese rule lasted for about 450 years, and heavily influenced Goan culture, cuisine, and architecture. In 1961, India took control over Goa after a 36-hour battle and integrated it into India. The area of Goa was incorporated into Goa, Daman and Diu, which included the Damaon territory in the north of the Konkan region. In 1987, following the Konkani language agitation Goa was granted statehood. Goa has one of the highest GDP per capita and Human Development Index among Indian states.

Earliest history

There is evidence of the tectonic origins of Goa dating back to 10,000 BC. Further, evidence of human occupation of Goa dates back at least to the Lower Paleolithic Age, indicated by the archaeological findings of Acheulean bifaces in the Mandovi-Zuari basin. However, evidence suggesting the region's ancient foundation is obscured by the legend of Goa's creation by the Hindu sage Parashurama.

Geological origins

Some parts of present-day Goa appear to have been uplifted from the sea due to geological tectonic plate movement. There is evidence to support this theory as indicated by the presence of marine fossils, buried seashells, and other features of reclaimed topography in the coastal belt. fossilized branches have been found later in many villages on the foothills of the Sahyadri dating back more than 10,000 BC. Thus the geologists concluded that Goa has risen from the seabed as a result of violent tectonic movements. At the decline of the intensity of population in the last Pleistocene age around 10000 BC, the bottom of Deccan Plateau was lifted up and out of sea-waters by the tectonic movements, formed the West-coast of India, Goa being a part thereof.

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