# Tag Info

4

We don't know for sure because A. the evidence has almost all been erased by the continued crustal shortening of the area where the volcanic arc(s) would have been. B. the region is huge and volcanism will have varied in duration greatly across the range as a whole. The "core range" of the Himalaya has lost on the order of 6000km (~2500 miles) of ...

2

I don't know if anyone is still interested in this question, but I am doing research on Uluru (a.k.a Ayers Rock), Australia, and the Mitten Ridge Sinkhole in Sedona, AZ (A very interesting combination of locations.). I have a photo just outside the sinkhole showing the sidewall of the Supai Sandstone. The sandstone is pitted just like honey-comb tafoni. ...

2

I know a young geologist using his smartphone as a compass. When we were in the field doing structural measurements together, I would: Record a waypoint using my hiking GPS Take the measurement with my compass Write it all down in my field notebook Given the time to take all the things out, and put them away afterwards, it was at least 2$-$3 minutes per ...

2

Part of the answer lies in where the geologist will be working and if there will be coverage by cellular/mobile telephone networks. It is my experience that a number of geologists, particularly exploration geologists, may work in remote regions where there is are no cellular/mobile telephone networks - parts of Africa, central Asia, Australia, South America, ...

1

To begin with, the formation of the Himalayas was never volcanic which is why you don't find volcanic rocks in the Himalayas. As for the subducting Indian oceanic plate (which contained Indian continental crust) that volcanism can be found in Tibet and the eastern Himalayas, in far northern Myanmar. This would suggest an oblique component to the subduction ...

1

For dating old geological material, zircon dating is sometimes used. Also see Uranium-lead dating. There is also data from Antarctic and Greenland ice cores. Other things you could look are Earth formation theories - the core accretion model & the disk instability model as well as plate tectonics and continental drift. There are also the theories about ...

1

From the readme.doc file, it looks that 1, 2 and 3 following AF and the other soil symbols in the excel files you mention are about this: Texture classes reflect the relative proportions of clay (fraction less than 0.002mm), silt (0.002 - 0.05mm) and sand (0.05 - 2mm) in the soil. Three textural classes are recognized: coarse (1): sands, loamy sands and ...

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