Deccan Traps - Wikipedia
The Deccan Traps are a large igneous province of west-central India (17–24°N, 73–74°E). They are one of the largest volcanic features on Earth, taking the form of a large shield volcano. [2] .
Deccan Volcanism caused the mass extinction 66 million years ago
Multiple evidence reveals the killing mechanism for the mass extinction 66 m.y. ago began 25,000 years earlier with the onset of cataclysmic Deccan volcanic eruptions in India that caused hyperthermal warming, mercury toxicity, ocean acidification and acid rain on land.
The Story of Deccan Plateau - Shaping Minds
Apr 25, 2023 · The Deccan Plateau is one of the oldest land masses on earth and is composed primarily of igneous rocks, known as the Deccan Traps. It was formed by volcanic activity during the Cretaceous period, around 60 million years ago.
Deccan Plateau - Wikipedia
The Deccan is a plateau extending over an area of 422,000 km 2 (163,000 sq mi) and occupies the majority of the Indian peninsula. It stretches from the Satpura and Vindhya Ranges in the north to the northern fringes of Tamil Nadu in the south.
Deccan Traps: Volcanic Climate Change & Dinosaur Die-Offs
Evidence: Western India is home to the Deccan Traps–a huge, rugged plateau that formed when molten lava solidified and turned to rock. The Deccan Traps date back to around 66 million years ago, when magma from deep inside Earth erupted to the surface.
What are the characteristics of Deccan Traps? - NCESC
Jun 22, 2024 · The Deccan Traps lava flow is a flood basalt province located on the Deccan Plateau in west-central India. It consists of more than 2000 m-thick succession of flat-lying basalt lava flows and covers an area of nearly 500,000 square kilometers.
Deccan Traps | Volcano World | Oregon State University
Sep 29, 2010 · The Deccan Traps are one of the largest volcanic provinces in the world. It consists of a composite thickness of more than 6,500 feet (>2,000 m) of flat-lying basalt lava flows and covers an area of nearly 200,000 square miles (500,000 square km) (roughly the size of the states of Washington and Oregon combined) in west-central India.
Deccan Traps - an overview | ScienceDirect Topics
The Deccan Traps flow basalt (65 Ma) is one of the largest volcanic features on Earth, and crops out over 500,000 sq. km of the west-central Indian subcontinent. The trap complex is predominantly composed of multiple layers of tholeiitic flood basalt.
Deccan Volcanism | Gerta Keller, Professor of Geosciences, Emeritus
This section provides critically important information on the effects of Deccan volcanism at 1000 km distance from the volcanic province. The information gained from this locality shows that the Deccan catastrophe was severe and caused near total devastation long before the final phase at the KTB mass extinction.
The Deccan Plateau: A Geological Journey Across Southern India
The Deccan Plateau, primarily composed of basaltic rock, is a testament to the volcanic activity that unfolded millions of years ago. The formation of the Deccan Traps, a vast region of basaltic lava flows, is attributed to a series of volcanic eruptions during the Cretaceous period.
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