Visit Your Local PBS Station PBS Home PBS Home Programs A-Z TV Schedules Watch Video Donate Shop PBS Search PBS

NOVA Online: Hot Lava
photo: Mike
Rhodes Excerpted Interview with Mike Rhodes, Geologist with the University of Massachusetts:

NOVA: What's it like to be right next to an active volcano?

RHODES: It's really impressive. The sound and the vibration of the eruption take over your body and it's a very moving experience. There's the intense heat, particularly if the wind's blowing the heat off a lava flow. It's very difficult to get close. There's all the sounds. There's the smell of the gases that tend to make you choke, make your eyes water, your nose run, things like that. And there's always this sort of sense of excitement, bordering on fear or at least certainly awareness and concern for one's safety and what one is doing.

NOVA: Do you ever get used to it?

RHODES: I don't. Maybe some people do but I certainly don't. I'm always conscious of what I'm doing and somewhat nervous about what I'm doing too.

NOVA Online: Hot Lava

NOVA: What is lava?

RHODES: Lava is a molten rock. It's rock which has been heated above its melting point such that it can flow and be ejected into the air.

NOVA: And is it the same thing as magma?

RHODES: It's essentially the same. Geologists tend to use the term magma for molten rock that hasn't yet arrived at the surface. When it erupts the same material is referred to as lava.

NOVA: Is it moving?

NOVA Online: Hot Lava

RHODES: Yes, it's sort of like a plastic in that it is actually flowing. It is actually moving in the same way as a stream flows or a glacier flows. But we wouldn't recognize it as flowing.

NOVA: What does mantle look like?

RHODES: The mantle is solid. It's flowing at very slow speeds, maybe a few centimeters a year. It's crystalline. It's got identifiable minerals in it, and as this is slowly moving upwards from the depth within the mantle, the pressure gradually decreases and at some point it will begin to melt and would in fact then produce a magma, or lava.

NOVA: How hot is that mantle material?

RHODES: It's probably in the order of about 1400, 1500 degrees centigrade (2500 degrees Fahrenheit).

NOVA: Why are these (Hawaiian) islands here?

RHODES: Well, there are a number of islands in different parts of the world where volcanos are forming and gradually building up the land masses and producing islands. In addition to Hawaii, good examples include Réunion in the Indian Ocean, Iceland, the Galapagos Islands, Tristan da Cunha in the South Atlantic. All of these are examples of volcanic activity that's creating new land masses in the oceans.

(continue)




Support provided by

For new content
visit the redesigned
NOVA site

return to the Hawaii homepage


NOVA Home | WGBH Home | PBS Home
Search | Feedback | Shop
© 1996 WGBH