crust, lithosphere, mantle, and asthenosphere |
Asta chose a question that could have been answered in far fewer than the 528 words she needed to meet that all-holy minimum word count. In fact, she (more or less) answered it completely within the first two sentences when she said,
"The lithosphere is not an individual layer, but rather a zone made up of two of the layers of the Earth, which includes the crust."In fact, the lithosphere comprises the crust and the uppermost, brittle portion of the mantle. Easy-peezy, lemon-squeezy, right? And if Jean had stopped there, she would have been... well, OK – not necessarily "right," but OK. Asta, however, had to keep writing; which is where she came up with the scientifically illiterate rubbish that so often afflicts eHow's stable of English Lit graduates. Some (although not all) of her dumbassery follows (with corrections):
- "The core, the innermost layer, is rich in iron and very dense." – "Rich" in iron? It's a nickel-iron alloy.
- "The mantle is made up of molten rock called magma." – No, it isn't. Magma is melted lithosphere. Why can't those liberal arts graduates ever figure that out? That's not to mention that the word "magma" appears in none of Asta's references...
- "[The crust] is the thinnest layer of the Earth at only 60 to 70 kilometers thick..." – No, Jean, oceanic crust is generally 5-10 km thick while continental crust is 30-50 km thick.
- "The crust surface is shaped by characteristics of the lithosphere that cause formations like mountains and fault lines." – No only is that rubbish ambiguous, but that's not what "formation" means to a geologist.
- "Volcanic activity occurs at subduction zones and forms continental landmasses..." – Not to put too fine a point on it, but volcanic activity occurs at just about any plate boundary and quite a few other places as well.
¹ now known as Leaf Group
copyright © 2018-2021 scmrak
SI - TECTONICS
No comments:
Post a Comment