The scientific study of the structure and processes that shape the earth's crust and surface features.
From Greek 'geo-' (earth) + 'tekton' (builder, carpenter) + '-logia' (study of). This term refers to the study of how earth-building forces work, emerging from 19th-century geology as scientists began understanding plate movements.
Geotectology explains why earthquakes happen and why mountain ranges form—it's about understanding the deep architecture of our planet. The discovery of plate tectonics revolutionized geotectology by showing that Earth's crust is like a giant puzzle made of moving pieces that continuously rearrange themselves.
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