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Gneiss shows such banding. Alternating bands are known to Geologists as Gneissose Banding, and is used to instantly classify the metamorphic rock.

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Q: What is composed of alternating bands of light and dark silicate minerals?
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What is composed of alterning bands of light and dark silicate minerals?

Gneiss shows such banding. Alternating bands are known to Geologists as Gneissose Banding, and is used to instantly classify the metamorphic rock.


What are rocks called with alternating bands of light and dark silicate minerals?

They are probably gneiss, a banded metamorphic rock.


Is composed of alternating bands of light and dark silicated minerals?

Gneiss shows such banding. Alternating bands are known to Geologists as Gneissose Banding, and is used to instantly classify the metamorphic rock.


The metamorphic rock texture that has alternating bands of light and dark minerals is?

gneiss


If a rock has bands of light and dark layers it is what?

It could be a sedimentary rock or a foliated metamorphic rock exhibiting alternating bands of light and dark minerals.


If a rock has bands of light and dark layers its what?

It could be a sedimentary rock or a foliated metamorphic rock exhibiting alternating bands of light and dark minerals.


Do smooth muscle have alternating dark and and light bands on them?

Yes, smooth muscle has alternating dark and light bands known as the A and I bands, respectively.


What planet has alternating bands of white brown red and tan?

The planet Jupiter has alternating white, brown, red, and tan bands. There are also yellow and orange bands that appear with storms and winds in the atmosphere.


Skeletal muscle cells are striated that is they have alternating dark and light bands called repectively?

A and I bands


What makes cells look striated?

The alternating A and I bands on the miofibrils.


Is gneiss nonbanded?

No. Gneiss has alternating light and dark bands.


During metamorphism of granite into gneiss what happens to the minerals?

With the extreme heat and pressure causing the metamorphism into gneiss, the constituent minerals recrystallize into bands, usually alternating from light colored to dark, perpendicular to the direction of the pressure which is being applied. The exact cause of the banding is not fully understood at this time.