Has the earth’s crust split into two halves? Here’s what the research team says | ANSWERS

A team of leading geologists from China and the US has made a stunning discovery that raises questions about geological stability. Earth’s crust. Has the earth’s crust split into two halves? In the next article we will tell you what experts say on this topic, which has attracted the attention of more than one.

IS THE EARTH’S CRUST OPENED INTO TWO HALVES? THIS IS THE RESEARCH TEAM SPEAKING

A team of geologists from China and the United States has discovered a surprising phenomenon in the heart of Tibet, where the Indian plate is splitting in two beneath the region.

Unlike normal vertical ruptures, this rift is horizontal: the shallow part supports the Tibetan Plateau, while the deeper part plunges into the Earth’s mantle.

The discovery challenges previous ideas about plate tectonics and raises questions about the risk of earthquakes in the region.

Although the Kona-Sangri fissure may indicate faulting in the Indian Plate, a direct link to seismic activity still requires further study, challenging current knowledge of Earth’s geology.

WHAT IS THE EARTH’S CRUST

The crust is the outermost and thinnest layer of the Earth, forming the solid surface of the planet. This layer is mainly composed of rocks and minerals and is essential for life on Earth as it is where most geological and geophysical processes occur.

The Earth’s crust is divided into two main types: continental crust, which makes up the continents and land masses, and oceanic crust, which makes up the sea floor. Both regions have differences in their composition and density. The crust is also the layer in which various geological features are found, such as mountains, valleys, oceans and other geographical features that have evolved over millions of years as a result of geodynamic processes.

The Earth’s crust is essential to understanding the geology and evolution of the planet because it provides critical information about the Earth’s geological history and is fundamental to understanding natural phenomena, the formation of natural resources, and the location of terrestrial habitats.

HOW MANY PARTS IS THE EARTH’S CRUST?

The Earth’s crust is made up of two main parts: the continental crust and the oceanic crust. The continental crust is the upper and thickest part of the earth’s crust, covering the protruding land masses, i.e., continents and continental shelves. On the other hand, the oceanic crust lies beneath the oceans and seas and is thinner and denser than the continental crust.

These two sections of the earth’s crust have significant differences in composition and thickness. Continental crust is thicker and reaches a depth of approximately 70 kilometers, while the average thickness of oceanic crust is about 5 kilometers. Both parts interact dynamically on the Earth’s surface, influencing the topography, geology and geophysical processes that characterize our planet.