What happens when a primordial city with its stake of myth, folklore and tradition confronts an aggressively expanding modernity? Varanasi is a place where antiquity holds a mirror to modern India to reveal its real essence and longstanding values that refuse to wither with changing time. Birdsongs of Love & Despair includes eleven short stories that delve deep into the ethos that has made Varanasi so unique. And here they speak in the voices of common people coming from different spheres of life–the gardener, the maid, the retired person, the dead grandmother or a toy seller. These are voices belonging to the margin, to the anxious souls, who with their love and tender thoughts, do not know how to resist the invasion of looming loss the modern times have brought in.
What happens when a primordial city with its stake of myth, folklore and tradition confronts an aggressively expanding modernity? Varanasi is a place where antiquity holds a mirror to modern India to reveal its real essence and longstanding values that refuse to wither with changing time. Birdsongs of Love & Despair includes eleven short stories that delve deep into the ethos that has made Varanasi so unique. And here they speak in the voices of common people coming from different spheres of life–the gardener, the maid, the retired person, the dead grandmother or a toy seller. These are voices belonging to the margin, to the anxious souls, who with their love and tender thoughts, do not know how to resist the invasion of looming loss the modern times have brought in.
This books documents the salient characters of the tectonic evolution of the Indian subcontinent. It showcases the well investigated subcontinent of Gondwana. The book is linked to an updated geological and tectonic map of this region on 1:12,000,000 in scale. The Indian subcontinent displays almost uninterrupted and unique the geological history since about Eo-Archean (~3800 Ma) to recent, with the development of many Proterozoic deformed and metamorphosed fold belts around Archean nuclei, and enormously thick undeformed platform deposits. After their stabilization during late Proterozoic, the subcontinent underwent Paleozoic rifting and deposition of coal-bearing thick sequences, followed by enormously-thick outpouring of Deccan volcanics as a consequence of huge mantle plume. The youngest event in its evolution is the Cenozoic Himalayan Orogenic Mountains, spanning the area between Nanga Parbat and Namcha Barwah; a part of which extends both in Pakistan and Myanmar.
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