Earth Lithosphere
The lithosphere, Earth's outermost shell, encompasses the crust and the uppermost mantle, extending about 100 kilometers deep. It is rigid and segmented into tectonic plates, whose movements drive geological phenomena such as earthquakes, volcanic activity, and mountain formation. The lithosphere's composition varies, with continental lithosphere being thicker and less dense compared to the thinner, denser oceanic lithosphere. Interactions at plate boundaries, including divergent, convergent, and transform boundaries, shape Earth's surface over geological time scales. The study of the lithosphere provides crucial insights into Earth's dynamic processes, influencing our understanding of natural hazards, resource distribution, and environmental changes.
Myint Win Bo
Toronto Metropolitan University , Canada
Leonid Anisimov
Volgograd State University, Russian Federation
Shozo Yanagida
Osaka University, Japan
Martina Gaglioti
LIPU, Italy
Maria Vicenta Esteller Alberich
Universidad Autónoma del Estado de México, Mexico
Oscar Andres Cuanalo Campos
Universidad Popular Autónoma del Estado de Puebla, Mexico
Arun K Shandilya
Dr HSG University Sagar, India
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
Title : Linking between color and element concentration for Fluorite: An optical spectroscopic approach
Ali Almohammed, Pandit Deendayal Energy University, India