The seismic counters began climbing at a pace that left even seasoned monitors pausing over their screens. Thousands of tiny tremors, each too small to be felt on land, stacked up hour after hour beneath the Pacific Ocean. By the time a full day had passed, the tally had crossed a threshold that demanded attention: more than ten thousand earthquakes recorded in just twenty four hours. The location was not random, nor was it unfamiliar to those who track the restless geology of the ocean floor. The activity was concentrated at Axial Seamount, an underwater volcano rising from the Juan de Fuca Ridge roughly three hundred miles, or about four hundred eighty kilometers, west of the Oregon coastline. How does a volcano hidden nearly a mile beneath the ocean surface generate such intense seismic unrest? What does it mean when the Earth fractures so persistently in such a short span of time? And why does this particular seamount repeatedly draw concern whenever its internal systems awaken? _ Join this channel to get access to perks: https://www.youtube.com/channel/UCHcADZQJjR5YE_47FaUo_tA/join _ Hope you guys enjoy this! 👉 If you enjoy this video, please like it and share it. 👉 Don't forget to subscribe to this channel for more updates.
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