Lava flow, a fundamental geological phenomenon, involves the effusion of molten rock from a volcano or fissure, spreading over the Earth's surface. Originating from the mantle, lava typically emerges at temperatures between 700°C and 1,200°C. Upon reaching the surface, it can travel several kilometers, influenced by factors like viscosity, slope gradient, and eruption rate. As lava cools, it solidifies into various forms such as pahoehoe, with smooth, ropy surfaces, and 'a'a, characterized by rough, clinkery textures. Lava flows contribute to the formation of volcanic landscapes, create new land, and influence local ecosystems. Over geological timescales, these flows can build extensive lava plateaus and shield volcanoes, shaping the Earth's surface and providing insights into the planet's internal processes.
Title : Geotechnical ground investigation
Myint Win Bo, Toronto Metropolitan University , Canada
Title : Simultaneous Global Climate Change "Heat Waves" and microwave and radio-wave from Solar Flares
Shozo Yanagida, Osaka University, Japan
Title : How subsurface waters record the earth’s history
Leonid Anisimov, Volgograd State University, Russian Federation
Title : Landslides.Rainfall one of the main triggering factors in the mountainous regions of Puebla, Mexico.
Oscar Andres Cuanalo Campos, Universidad Popular Autónoma del Estado de Puebla, Mexico
Title : Geo Education exploratory learning sessions on field and underwater
Martina Gaglioti, LIPU, Italy
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Ali Almohammed, Pandit Deendayal Energy University, India