Alpine Orogeny refers to the mountain-building processes that formed the Alps and other mountain ranges in Europe and Asia. This geological event began around 65 million years ago and continues today, primarily due to the collision of the African and Eurasian tectonic plates. The intense pressure and heat from this collision caused the Earth's crust to fold and uplift, creating high peaks and deep valleys. The Alpine Orogeny is part of a larger series of orogenies that have shaped the Earth's landscape over millions of years. It has also influenced the climate and ecosystems in the region, leading to diverse habitats and unique biodiversity. The ongoing geological activity continues to reshape the terrain, making it a dynamic area of study for geologists.