Seafloor spreading is a dynamic geological process where new oceanic crust forms at mid-ocean ridges. Here, tectonic plates diverge, allowing magma from the Earth's mantle to rise and solidify as it meets seawater, creating fresh crust. This ongoing activity not only reshapes the Earth's surface but also facilitates the movement of continents, supporting the theory of plate tectonics. By generating new crust and redistributing heat across the planet, seafloor spreading plays a pivotal role in Earth's geological and oceanic systems. It exemplifies the constant renewal and transformation of our planet's outer shell, impacting everything from ocean currents to the distribution of geological resources.
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