yego.me
💡 Stop wasting time. Read Youtube instead of watch. Download Chrome Extension

Volcanoes 101 | National Geographic


2m read
·Nov 11, 2024

Our planet has a violent soul, majestic and often destructive. Volcanic explosions rattle our collective imagination: Krakatoa, Mount St. Helens, Etna. Yet, lay your eyes on the images; they simultaneously strike fear and awe in our hearts.

But how did these giant mountains form, and where does all that destructive force come from? At least 50 eruptions rock the earth each year, meaning our planet is literally bursting apart at the seams. The Earth's crust is made up of about 17 slabs of land called tectonic plates that float on the superheated magma that makes up most of the planet's interior.

Magma is the Earth's lifeblood, churning restlessly beneath the crust, and wherever it can, it’s trying to burst through. It’s at these spots that volcanoes form. Our planet is home to some 500 active volcanoes. While some volcanoes, like those in Hawaii, break through a thin point in the crust called a hotspot, the vast majority of volcanoes occur on active fault lines where tectonic plates meet.

The most volatile region is the Ring of Fire, a geological fault belt that rims the Pacific Ocean and holds roughly 75 percent of all the Earth's volcanoes. Typically, volcanoes take one of two forms: shield volcanoes, which are wide and broad with lava usually slowly oozing out of them, and composite or stratovolcanoes, which are steeper and more violent.

When hot liquid magma reaches the surface, whether in a slithering flow or a booming eruption, we call it lava. Though molten lava may seem threatening, it's not known to move quickly. A volcano's pyroclastic flow is far more deadly; this poisonous ash cloud can race down the slope of a volcano like a bullet train, obliterating everything in its path at speeds topping 100 miles per hour. It’s what stopped the residents of Pompeii dead in their tracks.

But despite the volcano's brutal destruction, it is also a force of beauty and rebirth for the planet. Lava creates new lands where life can flourish. Like it or not, volcanoes are part of the planet's life cycle. As the Earth continues to explode, gurgle, and slither its molten heart out, we must learn to live side by side with its awesome power.

More Articles

View All
Miranda v. Arizona | Civil liberties and civil rights | US government and civics | Khan Academy
[Kim] You have the right to remain silent. Anything you say can and will be used against you in a court of law. We’ve become familiar with the Miranda Warnings given to suspects in police custody through movies and TV shows, but who was Miranda and what d…
Learn to Love Your Mistakes
You mentioned in the book that you need to learn to love your mistakes. Even as I was telling you about my hopeless, uh—or not hopeless, but hapless, uh, tendencies, there’s a part of me I start to flush. I start to feel embarrassed. It’s like it’s a litt…
Noble’s Story | How Khan Academy helped me get into my dream college
That was one of the best days of my life. Honestly, like signing day, I just knew that all the hard work that I put into this dream finally paid off. I’m Noble; I’m a freshman at Brown University. I’m a receiver on the football team. It became apparent t…
How to Stop Procrastinating
The greatest hindrance to living is expectancy, which depends upon the morrow and wastes to-day. — Seneca When we procrastinate, we are immersed in future thinking and unable to do the work that we had planned to do in the present moment. The consequence…
15 Money Secrets from the World's Wealthiest People
What do you think would happen if someone decided tomorrow to take all the money in the world and divide it amongst the global population equally? Some say the world would be a better place and everyone would be happy and prosperous. Others say that money…
Scaling perimeter and area example 2 | Transformational geometry | Grade 8 (TX) | Khan Academy
We’re told quadrilateral A was dilated by a scale factor of 2⁄3 to create quadrilateral B. Complete the missing measurements in the table below. So like always, pause this video and then we will do this together. Try to do it yourself, and then we’ll do i…