How to pronounce “basalt” in English

This little bleb here-- well, it's not really a bleb-- this, I guess, an iridescence, a pocket of iridescence is weathering of the lava.So basaltic lava in particular contains a lot of iron and magnesium, and those materials can oxidize when they're in contact with air.So this lava in this picture is just a few months old, and that beauty, that up-close beauty, the whole iridescence

This is a giant wall of basically magma.It's basalt, so it would have been-- it's ancient magma that would have fed eruptions a little further west to create the Watch Tongue Mountains in northern New Jersey,if you've ever been out there.

Kīlauea is an example.Its lava flows harden into broad flanks of basalt that end up looking kind of like a shield.But if the lava is extra gassy or has slightly more silica, eruptions can get a little more explosive.

The abyssal plain is the flat-ish bottom of the ocean basin.It’s mostly made of a volcanic rock called basalt and covered in a layer of sediment.It tends to hover around 4-and-a-half kilometers deep.

But even the rock-mutts still fall into three basic types, classified by how they formed within the rock cycle: sedimentary, like this super sandstone,igneous, like this beautiful basalt, and metamorphic, like this nice, well, gneiss!All three of these rock types were involved in the formation of Los Cuernos.

Now, here's another up-close view, and this is a side of lava that many people may not get a chance to ever experience, unless you're lucky enoughto go to a place like Hawaii that produces basaltic lavas, or Iceland, also, is in the news these days for doing somethingvery similar. But this is basaltic lava.

It intruded, if you will.But some igneous rocks, like the basalt and this pumice here, form in a way that’s extrusive.They’re created when magma exits up to the earth’s surface, becoming lava, where it cools and hardens into rock.

And you see them in the middle here of the cleaning cycle and someone back off about 20 or 30 meters who is recording the dataThe old LITA drill was notoriously wimpy in some materials-- if you went into basalt or if he went into solid ice.

to go to a place like Hawaii that produces basaltic lavas, or Iceland, also, is in the news these days for doing somethingvery similar. But this is basaltic lava.And this middle section, I'm going to put the cursor on the mid-left portion of the screen and then slowly just drag it over to the right.

They never got sleepy.But they didn't talk very much, and they just sat there on the basalt boulders.And then all of a sudden-- so I thought that was magical.

This is a picture from Google Maps, actually.Basically, all the brown stuff you see on that map is basalt lava from these giant eruptions 252 million years ago.And they erupted through one of the world's biggest coal basins.

And he shows me a picture of the vineyards and this looks like the moon if the moon had vineyards with palm trees on it. That's what these vineyards would look like. The vinesare planted inside of craters and around the craters are little volcanic rocks, basalt rocks, that shelter the craters because it's very windy, it's very dry, and they need tocapture every molecule of moisture that lands anywhere in the vicinity and shelter the vines from the wind.

They’re generally composed of both continental lithosphere, which makes up the land we can see, and oceanic lithosphere, which makes up the seafloor.Continental lithosphere is made up of mostly thick, lightweight granite, while oceanic lithosphere is made of denser, heavier rocks like basalt and gabbro.Roughly 95 percent of Earth’s surface is made up of seven major plates, with the rest covered by much smaller ones.