Wednesday, October 11, 2017

Red River Gorge, Kentucky

In my other life, I am a professor of geology at Northern Kentucky University.  An important part of my teaching is taking students on field trips to expose them to geology first hand.  Last weekend I took my introductory class to Red River Gorge in Kentucky to study the formation of natural bridges and other associated rock formations.

Red River Gorge is near Slade, Kentucky, about an hour southeast of Lexington.  It is one of the largest collections of natural bridges in the country.  


Red River Gorge is on the edge of the Appalachian Plateau on what is known as the Pottsville escarpment.  In this area, sandstone from the Pennsylvanian Period, about 290 million years ago, is exposed.  This sandstone is relatively resistant to erosion, especially compared to the Mississippian Limestone that lies below it.  As a result, it holds up the edge of the plateau and creates the escarpment, where it drops down to lower elevations where the Mississippian limestone is exposed.  

From University of Kentucky department of Geography.  The blue-gray area on the east side of the state is Pennsylvanian sandstone and the lighter blue is Mississipian limestone.  

The region was uplifted along the edge of the Cincinnati arch during the formation of the Appalachian Mountains, which ended in the Permian Age, 245 million years ago.  The uplift warped the continent in this area and made the layers tilted, as shown in the geologic cross-section above.  This causes different rock units to be exposed in different parts of the state, with the oldest in the center of the Cincinnati arch, which is centered on Lexington, and younger rocks found in a bulls-eye pattern around it.  Where the Pennsylvanian sandstone and the Mississippian limestone are exposed together, we get the escarpment.  

The flat tops of the hills are the Appalachian Plateau.  The Red River cut down through the sandstone, exposing it and allowing the formation of the natural bridges.


The limestone was deposited in a shallow sea teeming with life of a coral reef in a shallow sea that formed in the Appalachian Basin, a low area that formed when the Appalachian Mountains pushed up and put weight on the continent, pushing it down.  From the Mississippian to the Pennsylvanian, this basin started to get more shallow and the sandstone was deposited in layers by large rivers flowing off the Appalachian Mountains and into the Appalachian Basin.  During the uplift of the Cincinnati arch, the sandstone was fractured in both a north-south and east-west direction.  

The combination of horizontal layers in the sandstone and the fractures are responsible for the formation of the natural bridges in this area.  Initially, the sandstone starts to weather by grains of sand and pebbles getting plucked out of the sand.  Small holes open up in the sand, and the grains get caught up in the holes with wind and rain and tumble around in the holes opening them larger.  This creates a "swiss cheese" texture in the rock.  
"Swis cheese" texture in the sandstone as little holes open

Eventually, these little holes grow to where they start combining together and open up recessed caves.  Recessed caves are shallow but long and follow the layers in the sandstone.  The layers are zones of weakness in the rock, so the rock weathers more quickly here.  

A recessed cave can be seen under this waterfall at Rock Bridge
The sandstone has horizontal layers that are more susceptible to weathering and open up recessed caves
Because the sandstone is fractured vertically, eventually, the recessed cave will cut through to the other side, where a fracture exposes it, opening a hole in the rock and creating an arch.  Initially this hole is small, but it eventually grows.  Early, the edges of the arch are sharp and blocky, like at Natural Bridge.  But, over time the edges of the bridge weather more smooth, and the arch becomes more rounded.  This is like what is seen at Delicate Arch at Arches National Monument in Utah.

Students under Natural Bridge.  Natural Bridge is sharp and blocky and is a young arch.
Delicate Arch in Utah is an old arch

Eventually, the top of the arch becomes too thin to support itself and it collapses forming pinnacles.  The pinnacles continue to weather along the layers, and form balanced rocks.  Eventually, the balanced rock will collapse, completely destroying the formations.  
Balanced Rock at Natural Bridge State Park

Sometimes, the bridges will form from a river running over the sandstone and cutting down into the fractures.  As the fracture opens, it separates a bridge from the rest of the rock, and forms a waterfall next to the bridge.  Over time, the waterfall will cut upstream, separating from the bridge.  This is the case at Rock Bridge.  The waterfall is now about 1/4 mile upstream from the bridge.
Waterfall formed by Rock Bridge

Rock Bridge with a river flowing under it

Weathering is a process of creation, but it is also a process of destruction.  The formation of the arches will continue to change until ultimately they are destroyed by the same processes that created them.

Saturday, September 9, 2017

Opals and Onyx

Tomorrow, I am releasing the limited edition

opals and onyx collection

showstopping gemstones for every occasion



Opals and onyx are two of the most popular ever-lasting gemstones in the jewelry market.  But what are they ... really?  In a previous post on August 20, I talked about flint and chert.  Today, you will discover that opal, onyx, chert, flint, chalcedony ... they are all essentially variations on the same thing - microcrystalline grains of silica.

Onyx is a banded variety of chalcedony.  The bands are created by alternating layers of microcrystalline quartz and moganite, which is essentially quartz with a different crystal structure.  Sardonyx is a variety of onyx with bands of quartz and sard, another variety of chalcedony.  (Gemstone manufactures seem to try to make their products stand out by giving different names to essentially the same minerals).  Utah blue and orange sardonyx are examples.
Utah Sardonyx collected near Nephi, Utah

Calcite onyx is actually not onyx at all.  Calcite onyx, or cave onyx, is banded layers of calcite that form from cave formations such as stalagtites and stalagmites.  It forms much the same way, with one little layer at a time slowly precipitated.  But it is calcite instead of quartz.  Honey onyx and the most popular flowering tube onyx are examples.
Flowering Tube Onyx collected near Nephi, Utah

Cave Formations at Ruby Falls, Tennesee
Opal is the least like all the other minerals - onyx, chert, flint, and chalcedony.  It is still silica, but in opal, the silica does not form crystals of quartz.  It is a hydrated, amorphous silica "ooze".  Most often, opal is associated with volcanic activity.  Silica-rich fluids from magma flow into the surrounding rock, where the opal is precipitated in pockets and layers in the rock.  The internal structure of the silica ooze makes it refract light, which gives opals their most-sought after feature - sparkle.

There are two types of opal - common opal and precious opal.  I personally feel these names do not do them justice because "common" opal is just as amazing as precious opal.  Precious opal tends to show a play of colors and multi-color sparkle and shimmer that dances in the light.  Common opal tends to be translucent and often a single solid color, or bands of colors.

Examples of common opal include Utah bacon opal and Peruvian pink and blue opal.
Utah Bacon Opal collected near Milford, Utah

Examples of precious opal include the Honduran black matrix opal and koroit boulder opal.

Honduran Black Matrix Opal

All of these stones make beautiful cabs and stunning jewelry perfect for that special occasion or to make every day feel special.

Cabochon from Bacon Opal
Cabochon from Koroit Boulder Opal














Find the Opal and Onyx Collection at www.rubymountain5rocks.com.  Don't forget, join Club Ruby for an instant 20% discount!

Dr. Janet Bertog, owner Ruby Mountain5 Rocks




Monday, September 4, 2017

Hurricane Harvey

Most people are fully aware of the impact that hurricane Harvey has had on Houston and the surrounding areas.  This was the first hurricane to make landfall in the United States since 2005, and it is easy to forget about the devastation these things can cause, especially after 12 years of feeling "safe".  When it made landfall, it was a category 4 hurricane, with sustained winds of 130 mph.  This was the beginning of days of torment.  Hurricane Harvey was in no hurry to leave Texas, and stalled for two days just inland, with continued heavy rainfall.

In reality, although the devastation is enoromous, the people were "lucky".  There were 60 confirmed deaths, in comparison to approximately 1500 (as many as 1800) deaths from Hurricane Katrina in 2005.  Nevertheless, Hurricane Harvey was catastrophic.

And now, only days after the remnants of Hurricane Harvey made its way across the eastern United States, we are poised for another hurricane, Hurricane Irma is headed toward the Carribean and is expected to impact the east coast next week.

While people are picking up the pieces from this hurricane and trying to put their lives back together, some people lost very important members of their families.  While rescuers were able to evacuate many people, they could not take pets with them.  Pets all over the region are abandoned, lost, confused and scared.  Rescue agencies all over the country have mobilized to help get these pets back to their families.

In Ohio, where I live, Silver Linings of Ohio is teaming up with other rescue agencies in Ohio to bring pets that were in rescues and shelters in Houston to Ohio for foster and adoption.  Meanwhile, Best Friends Animal Society is working to house the lost pets and help them find their families again.  I am sure there are agencies in your state doing the same things.

During this time, I will be donating 15% of my sales to Silver Linings of Ohio to help them bring the animals to Ohio, house, feed, and medicate them, and help them find loving homes.


Helping shelter pets in the wake of Hurricane Harvey


Janet Bertog,


My assistants ... Reddie and Angus (my senior rescue dogs)






Monday, August 28, 2017

Thomas Mountains of Utah - Volcanic Fields for Hundreds of Miles

Thomas Mountains, Utah

This summer when I did my dinosaur expedition to Utah, we took some time to go to the Thomas Mountains in eastern Utah.  We actually went there last year as well.  This place is amazing!  The geology of the region is very complex, with multiple events occurring in the same place over a span of hundreds of millions of years.  The Thomas Mountains are a volcanic mountain range that formed about 50 million years ago to as recently as 1 million years ago, near the time of the end of the formation of the Rocky Mountains.  Numerous volcanoes litter the region and most of them are calderas, giant volcanoes that erupted very violently.  Because of the volcanic activity in this area, gemstones are very common throughout the region. 

Probably the best known caldera is Topaz Mountain, appropriately named because natural amber-colored topaz is found here, along with red beryl, amethyst, garnet, bixbyite, opal and hematite.  The minerals are found in cavities in the rhyolite ash that was deposited when the volcano erupted.  It can be a lot of work to break open the rhyolite to find the cavities with the precious minerals inside.    In the picture, you can see the crater of the caldera.  The area of Eureka is also famous for many metal deposits, including gold and silver.
Topaz Mountain near Eureka, Utah

To the southeast of Topaz Mountain, near the town of Nephi, precious calcite onyx can be found.  The popular flowering tube onyx is from this area as well as yellow, red and white banded sardonyx, which will be available on Ruby Mountain5 Rocks soon.  The onyx forms when geothermal fluids from the volcanoes flowed through calcium-rich rocks in the mountains, depositing bands of colorful silica.

Flowering Tube Onyx
 
Sardonyx
Available at Clidastes Stones

To the west of Eureka is the town of Birdseye, where birdseye rhyolite is found (Utah Birdseye Rhyolite will soon be available at Ruby Mountain5 Rocks, currently you can find Mexican Birds Eye Rhyolite)
Birdseye Rhyolite, Utah
Available at Clidastes Stones



South of Delta is another kind of volcano, Sunstone Knoll is a locality that is andesite lava.  In the cavities in the andesite, you can find small yellow sunstone crystals.  Sunstone is a gem variety of the mineral feldspar, the same class of minerals that includes moonstone and labradorite.

Sunstone knoll is a cinder cone.  Cinder cones are smaller volcanoes that are less explosive and produce more lava than ash.

Sunstone Knoll.  Image from millardcounty.com

Sunstones collected from Sunstone Knoll


My most favorite gemstone from this area is the bacon opal.  Bacon opal is formed when geothermal fluids flow through rhyolite layers and deposit colorful bands of silica rich in iron minerals.  Every piece of this material is unique.  You can find specimens of bacon opal at Ruby Mountain5 Rocks, Bacon Opal.
 



One of the most famous and sought after gemstones from Thomas Mountains is Tiffany Stone.  Tiffany stone is becoming very rare because the locality has not been open to collecting for quite a long time and the only stock available was collected over 30 years ago.  Tiffany stone is opalized beryllium-rich fluorite and bertrandite.  This stone has a cracked marbling of creamy white and purple.  You can get your own Tiffany Stone at Ruby Mountain5 Rocks.

 



Utah is riddled with collecting localities for rock hounds of all types.  Some localities can be found here and here.

By Dr. Janet Bertog, Professor of Geology
Owner of Ruby Mountain5Rocks
Owner of Clidastes Stones



Sunday, August 20, 2017

Chert, Flint, Jasper, Agate, Opal .... all so popular, and yet, what's the difference??

Chert, flint, jasper, agate - these are all common semi-precious and precious gemstones found in the lapidary world.  They are all different, they all look different, and yet, they are all the same.  All of these gemstones are made of micro-crystalline or non-crystalline silica grains, similar to quartz.  So, why so many different names for essentially the same material?  Well, it gets even more complicated than that because there are many types of jasper, many types of agate... you get the idea.  

So, to start, what makes them all similar?  Rocks are generally made up of minerals.  Minerals are crystals with an orderly arrangement of atoms.  Some rocks are not made up of minerals.  For example, coal is made up of plant material, which is not a mineral.  No minerals are organic.  Chert, flint, jasper and agate are all made up of micro-crystalline, poly-crystalline quartz, a mineral composed of silica and oxygen.

Chert and flint are the most similar.  They really are essentially the same thing.  Chert is the variety that most often forms in nodules in limestone.  The formation of chert in limestone is thought to be a result of sponges (the marine animals).  Sponges make their shells out of tiny spicules of silica.  When they die, this silica absorbs into the water.  Most other animals in the shallow marine environment, including corals and clams, use calcite to make their shells.  The calcite gets recrystallized into limestone.  The silica from the sponges globs together and forms nodules in the limestone.  If you work in limestone, or in caves, this is often called "trash rock" because it is not the main rock that makes the limestone.  Chert is also found in banded iron formations, which are layers of the iron mineral hematite and chert.  Banded iron formations formed during the Precambrian, more than 500 million years ago.  It is thought that the alternating bands of hematite and chert represent seasonal changes.  During the dry season, chert crystallized out of the water and precipitated to the bottom of the oceans.  Sponges are some of the oldest animals on Earth and it is possible that this chert is remnants of these sponges, which were living in the ocean when no calcite-forming animals were around.  Up on land, things were much different.  There were no plants or animals on land during this time, the land was barren and weathering.  During rainy seasons, iron-rich weathered rock would get washed into the ocean as hematite-rich sands, depositing a layer.  This would alternate each season, with a layer of chert then a layer of hematite.  After the Precambrian, with the onset of the Cambrian, there was an explosion of new life, particularly, this was the first occurrence of animals with hard parts, shells made of calcite.  This put an end to banded iron formations.

So, long story short, chert is generally made from tiny pieces of sponge.  So what about flint?  Well, flint is exactly the same thing as chert, but it is usually restricted to the variety found in chalk or marl (marl is chalk with mud in it, chalk is very fine grained limestone - so many subtle variations!).  Some famous flint includes the Flint Hills in Kansas and the Ohio Flint Ridge.

So, what about jasper and agate?  These are also varieties of micro-crystalline,crypto-crystalline quartz, but they form by the replacement of other minerals with the quartz.  The main difference between jasper and agate is that agate is banded and jasper is not.  Jasper will replace grains of minerals in rock very slowly over time.  Petrified wood is a variety of jasper where the wood grains have been completely replaced with silica, or petrified.   There are many other types of jasper as well.  One of the neat things about jasper is that the replacement process usually creates great color patterns in the rock, such as seen in Owyhee Picture Jasper.  You will find that many of these jaspers are very similar!  That is a topic for another post.  Some rocks are mistakenly called jasper.  One example of this is Rainforest Jasper, which is really rhyolite, a type of volcanic ash.


Picture jasper with antiqued copper tree of life
Owyhee Picture Jasper
Owyhee Picture Jasper Slab
Brecciated Rhyolite (Jasper)
 
Birdseye Rhyolite (Jasper) Cab














Agate is generally banded and forms as the grains of quartz crystallize out around a rim or precipitate out in cavities.  Crazy lace agate is an example of an agate that forms in cavities and creates nodules that have to be cut open to reveal their beauty.  Moss agate forms from the crystallization of minerals in a mossy pattern within a background mineral.  Again, some rocks are misnamed, like Turitella Agate, which is actually not Turitella and is really a jasper.



Moss Agate Pendant at Clidastes Stones
Montana Agate
Montana Moss Agate

















Turitella Agate

Some examples of jasper include Bigg's Picture JasperDeschutes Picture JasperFantasy JasperKambaba JasperLeopardskin JasperMary Ellen JasperOcean JasperOwyhee Picture Jasper.

Some examples of agate include Black Plume/Medicine Bow Agate, Montana Moss Agate, and many more!

By Dr. Janet Bertog, Professor of Geology, Northern Kentucky University
Owner of Ruby Mountain5 Rocks lapidary material
Owner of Clidastes Stones, specializing in unique and rare gemstone jewelry and home decor


Utah Dinosaur Expedition and Mineral Collecting

I have returned from another successful trip to my Utah dinosaur excavation.  I have been working at this site for 13 years, studying the animals that are buried there and how they got there.  Every year a group of students from Northern Kentucky University and Marietta College and volunteers from all over join us at this dig.  The site is called the Aaron Scott Quarry and is near Ferron, Utah.  Our main dinosaur at the quarry is the majority of a skeleton of a Barosaurus. The site is in the Jurassic Period.  In addition to the Barosuarus, we have a juvenile Apatosaurus, lots of teeth and some other bones of an Allosaurus, and isolated remains of DryosaurusCamptosaurusCoelurus, and turtles, crocodiles, a small lizard called a sphenodont (related to a tuatara), and a few mammals.For an account of our adventures, you can see my posts on the facebook group Ruby Moutain5Rocks.  Here are some of the highlights.
Sites from the quarry:
excavation1
Students and volunteers excavating the quarry
Small bones from the quarry
Bones are wrapped in plaster to protect them
excavation2
Students and volunteers excavating the quarry
We camp at the site and it is such a beautiful place.  Here is the sunrise to the east and the reflection off the hill to our west.
 
We also take in some of the geological and cultural history of the area.
San Rafael
Students and volunteers at the Little Grand Canyon of the San Rafael
Spanish Trail
The Spanish Trail passes very close to our site. These monuments mark one of the places they passed through
The Fremont Culture carved these petroglyphs about 1000 years ago
Barrier Canyon
The Barrier Canyon Culture painted these pictographs about 2000 years ago
In the Thomas Mountain Range, volcanic activity was prevelent about 50 million years ago.  This deposited a lot of volcanic ash and lava flows and a great deal of mineralization is present as a result.   Some well known gemstones come from this mountain range including Tiffany StoneFlowering Tube Onyx, Calcite Onyx (coming soon), Birds Eye Rhyolite (coming soon), and this trip we collected sunstones and hyalite bacon opal, which will soon be available.
sunstones
Sunstones from near Delta, Utah
bacon opal
Hyalite bacon opal from near Milford, Utah
On the way home, we stopped at the Last Chance Mine in Colorado.  This area of the San Juan Mountains is again a giant volcanic field with several calderas. A lot of mineralization has taken place in this area including gold, silver, copper and zinc and it has been heavily mined.  The Last Chance Mine was a silver mine and the “waste rock” is sowbelly agate, or banded lace agate.  I collected a bunch of this material to make available soon as well!
Banded lace agate
Sowbelly agate
Volcanic ash from calderas in the San Juans
Overall, a very successful trip and I look forward to making all this new material available to you soon!
Visit http://www.rubymountain5rocks.com for lapidary slabs from these and other locations and http://ClidastesStones.etsy.com for cabochons and jewelry made from this material.

Ruby Mountain5 Rocks Under New Ownership

Welcome to Ruby Mountain5 Rocks Rock Shop.

Hello!  I have recently taken over new ownership of Ruby Mountain5 Rocks.  I promise to maintain the same quality products at reasonable prices.  I have recently implemented a new, lower pricing scheme, and free shipping still applies in the US, and now Canada!  Free shipping on orders over 5 items internationally.

So, a little about me.  I am a professor of Geology at Northern Kentucky University.  My specialty is vertebrate paleontology,  but I teach classes in introductory geology, field paleontology, stratigraphy and sedimenation (the study of rock units deposited in different environments and what they tell us about the environments), mineralogy and petrology (the study of the identification, characterization and interpretation of all rock types).  I have been teaching at NKU for 14 years and recently received full professorship.

In January 2016 I started an Etsy business, Clidastes Stones, selling stone crafted wire wrap jewelry and home decor.  I began to brach out within this business and started selling mineral specimens, rock slabs and cabochons.  I really enjoyed finding unique stones for people and sharing them.  I have done most of my business on Facebook through this company.  I have made hundreds of sales this way and have many repeat customers.

About a month ago, I saw Sharon's post about selling this business so they could retire.  I decided this fit perfectly with the direction I was taking my business and so  I offered to buy it.  Now, here I am, surrounded my thousands of rocks that I love and am excited to share them with you.

As you peruse the website, please keep in my mind that I have thousands of slabs of inventory to post, and I am working on this as quickly as possible.  In the meantime, if there is anything you are interested in that is not posted, please check the bulk spreadsheet lists for available items and contact me to see some of what I have available.

I know there will be some bumps in the road as I adjust the website to my settings, but I try to keep these to a minimum and will be happy to assist with anything that might come up.

I look forward to working with you to provide you with quality materials for your jewelry making or personal collections.

Please visit my websites Ruby Mountain5 Rocks and Clidastes Stones!