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The Earth Story

@earthstory / earthstory.tumblr.com

This is the blog homepage of the Facebook group "The Earth Story" (Click here to visit our Facebook group). “The Earth Story” are group of volunteers with backgrounds throughout the Earth Sciences. We cover all Earth sciences - oceanography, climatology, geology, geophysics and much, much more. Our articles combine the latest research, stunning photography, and basic knowledge of geosciences, and are written for everyone!
We hope you find us to be a unique home for learning about the Earth sciences, and we hope you enjoy!
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geoledgy

I bought a 365 nm UV light to unlock forbidden colors in my minerals. Top is my manganoan calcite I got last week at a rock show (most fluorescent specimen I have in my collection, it turns a pink-orange which is pretty cool) and on the bottom is my cassiterite (not fluorescent) but I found that uv light will shine on dust so it was kinda interesting.

The photo I have does not do the fluorescent property ANY justice, it is very bright IRL. Maybe I'll see if I can take a better photo in the future.

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New Locations

One of the most useful things I’ve learned as a rock hound is how to locate new mineral sources. There are plenty of books and internet sources that can show you the major dig sites. This is good for beginners, but these sites can be crowded, mostly depleted, and often times left in a mess of tailings that you have to dig through to reach new material.

To start this off, definitely use local resources. Local rockhounding clubs and mineral societies often have plenty of useful info to get you started and occasionally have their own sites. Although I stick to my self and do my best to find my own locations, I will still occasionally use local groups’ sites and buy maps or guides to support them.

Maps are key. There are a variety of maps that’ll be a major help for finding mineral sources. I have four go to maps that I use regularly. I will go through three of the maps and explain how I use them, and then how I add it all up. Google maps (or Earth) is going to be a big help in getting an idea of the terrain and location.

First is geological maps. Obviously each state is going to vary, but this is the USGS map showing Washington’s surface geology. Other good sources of geological maps are geology schools or schools that have geology departments. I would regularly check Montana Tech’s maps while in western Montana.

There are two ways I utilize these maps. 1: learn a little bit of geology to figure out what host rock different minerals form in. This is a little bit trickier than the second method but if your a curious person and like learning new things it’s not too bad.

2 (match the color): pull up a geological map and a regular map like google. Find some well know prospecting locations and try to locate them on the geological map. After locating, you can observe what the host in that site is and look for other areas with the same host rock. For example: A well know site near me for geodes and agate has a surface geology consisting of tertiary volcanic rock (Tv, brown). I can take that and simply look around for other brown areas on the map. I’ve used this method a few times and can even match it with other known dig sites. I also like to use google maps to see if there is exposed rock or Boulder fields in the area for easy access.

The Diggings have a very useful website that I utilize regularly. The black diamonds show documented mines, prospects, and placers. The blue boxes are current and expired mineral claims. I like to use this map to find where clusters of mineral claims are to find what can be in the general area. It’s also useful to make sure you aren’t on someone’s active claim. It’s always safe to check with the Bureau of Land Management, just to be sure.

Finally is OnX maps. I currently do not have their product downloaded so I can’t show a photo. This one isn’t involved with rockhounding but the hunting version is incredibly useful. OnX maps shows accurate land boundaries along with ownership. It does not show mineral claims but it is helpful in knowing where you are and making sure you are on lands where you can legally prospect. It also has multiple layers that you can customize, route tracking, and saving maps to use when offline. I believe the hunting version is $30 for a year of one state or $100 for the entire US, but don’t quote me on that. Also, I do not have a partnership with this brand. I am simply a very satisfied customer.

So that about sums up how I locate new deposits. There are plenty of other methods and resources you can use out there. Hoping this provides some help to anyone interested. I apologize for the long post.

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Thrissops This fish is a Thrissops, a genus of ray-finned, bony fish that swam in the seas during the Jurassic and the Cretaceous. This extremely well preserved sample was preserved in the Kimmeridge clay, a geologic unit made of fine-grained sediment that sank to the bottom of a Jurassic seaway. The unit is exposed on the Dorset coast of England and travels offshore where it is the major source of North Sea oil and natural gas. This sample is housed in the Etches Collection – a private museum in the area where this fossil was found. -JBB Image credit: Lebatihem https://flic.kr/p/2n2VpGj

Source: facebook.com
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Airglow over the Atacama One of the several rising steps that climbs to the main cordillera of the Andes through the driest desert on Earth resembles a beach abutting onto a sea of clouds below and provides the backdrop for this gorgeous photo of airglow above the southern skies with our galaxy in the sky above. The ripples are caused by atmospheric waves and produce a completely different pattern to those in the skies above the Tibetan Plateau I shared once before (see http://on.fb.me/1MC62j0).

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Norbergite These yellow crystals bear testament to the forces of metamorphism, which transformed the original sea bottom limestone into glistening white marble, concentrating the impurities in the rock into gems. This particular one was magnesium rich, since the marble is dotted with red spinel crystals (magnesium aluminium oxide) along with a larger yellow-brown chunk of normbergite (hydrated fluorated magnesium silicate).

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The simplest kind of fault When rocks tear and break they can do so in a variety of ways, depending on whether they are being pulled apart (aka extension to geologists), pushed together (compression) or slid alongside each other (strike slip, like the San Andreas) by the tectonic forces affecting the area. This example is a normal fault from Iran, produced by pull apart forces, at least on a local level. The layers pick out very well the block of rock that has dropped between two others, and the two fault lines bordering it. The tectonics in Iran are complex, the main forces are compressive as Arabia separates from Africa and is in a slow motion collision that is closing the Persian Gulf. As the rock is pushed out of the way and uplifted to form mountains such as the Zagros range some regions are twisting and buckling in a rotatory motion, leading to local extensive forces and normal faulting. Loz Image credit: https://twitter.com/HaakonFossen

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