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The Siberian Traps (Russian: Сибирские траппы, romanized: Sibirskiye trappy) are a large region of volcanic rock, known as a large igneous province, in Siberia, Russia. The massive eruptive event that formed the traps is one of the largest known volcanic events in the last 500 million years.
The Siberian Trap is a chess opening trap. After a series of natural moves in the Smith–Morra Gambit of the Sicilian Defence , White can lose a queen . The name appears to result from Boris Schipkov of Novosibirsk in southwestern Siberia .
Trap rock, also known as either trapp or trap, is any dark-colored, fine-grained, non-granitic intrusive or extrusive igneous rock. Types of trap rock include basalt, peridotite, diabase, and gabbro. [1] Trap is also used to refer to flood (plateau) basalts, such as the Deccan Traps and Siberian Traps. [2]
A sample of Siberian Traps basalt (dark) containing native iron (from Siberian Traps) Image 12 Nenets child (from Indigenous peoples of Siberia ) Image 13 Laminar armour from hardened leather reinforced by wood and bones such as this was worn by native Siberians.
In chess, the Smith–Morra Gambit (or simply Morra Gambit) is an opening gambit against the Sicilian Defence distinguished by the moves: . 1. e4 c5 2. d4 cxd4 3. c3. White sacrifices a pawn to develop quickly and create attacking chances.
Siberian Traps (252.6) [z] Permian–Triassic extinction event: Paleozoic: Permian: Lopingian: Changhsingian: ... This page was last edited on 2 April 2024, at 12:45 ...
Much of the Siberian Traps Large Igneous Province is inside. [1]The area is of about 400,000 square miles (1,000,000 km 2) in Krasnoyarsk Territory and Sakha Republic, between the Yenisei and Lena rivers.
Pages in category "Chess traps" ... Siberian Trap; V. Vienna Game, Würzburger Trap This page was last edited on 28 March 2013, at 03:03 (UTC). ...