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What Kind Of Minerals and Crystals Can Be Found In Ohio?

Ohio Fluorite
Calcite celestite Pugh Quarry, Custar, Ohio

Calcite and celestite crystals from Ohio

If you live in Ohio and want to get rich finding Emeralds then forget it. Your best bet for that is to move to the Asheville, NC. Our state just doesn’t have the Geology necessary for that sort of gemstone to be present. It’s true people do find gold and diamonds (six of those have been found in Ohio, not including those found in jewelry stores) in Ohio, but those are travelers that arrived courtesy of glaciers and deposited in glacial sedimentary deposits.

But just because you can’t fill a jewelry shop from our geology doesn’t mean that Ohio isn’t rich in crystal treasure. Our state is blessed with minerals that are used industrially and helped turn the state into an Industrial powerhouse. It also is a source of beautiful minerals perfect for a collection or as a display piece (Celestite, I am looking at you!) And don’t get me started talking about fossils! Cincinnati is famous for its rich troves of Ordovician era fossils on the Cincinnati Arch. You know where to go if you want a Trilobite.

Since most locals aren’t aware of our state’s Geology, let alone that we have a geology, or if we have one, where somebody may have misplaced it, how much it’s worth and whether you can trade it to rent Top Gun: Maverick on Amazon, we are presenting a curated list of the crystals and minerals found in the Buckeye state.

Photo credit for image above: Photo By James St. John – https://www.flickr.com/photos/47445767@N05/33229612163/, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=96284794

Calcite

Calcite crystals Gibraltar Island Lake Erie Ohio

Sunlit Silurian calcite from Put-in-Bay in Ohio on Lake Erie.

Photo By James St. John – https://www.flickr.com/photos/47445767@N05/50588186197/, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=96284996

Calcite is found throughout Ohio in different forms as granular aggregates in black shale in eastern and central Ohio, and as crystal and granular aggregates in Western Ohio.

The name calcite comes from a Greek word meaning lime. This comes from its chemical component, Calcium Carbonate, which sometimes is mistakenly known as “lime.” Calcite is known in more than 300 forms of crystals. The scalenohedral crystals of Calcite, one of its most common varieties, ordinarily are known as “dogtooth spar” or “dogtooth calcite” because of their resemblance to a dog’s canine tooth. Another variety, transparent rhombohedral calcite, is used in optical equipment. Although they are not specific varieties of calcite, stalactites, stalagmites and other formations found in caverns are made of calcite.

Calcite is one of the most common minerals, making up about 4% by weight of the Earth’s crust. Calcite is common as vein fillings in many rocks in western and central Ohio. Silurian dolomites in northwestern Ohio yield clusters of large crystals ranging from clear to dark brown. Many have a golden color.

Crystals and granular aggregates in cavities and fractures of dolostones and limestones in western Ohio; granular aggregates commonly form veins in dolostone concretions and less commonly in ironstone concretions from black shales in central and eastern Ohio; more rare as an efflorescence.

Calcite (CaCO3) is a soft carbonate mineral that occurs in various colors, including white, yellow, brown, gray, black, and pink, and also can be colorless. Calcite is a common mineral that occurs primarily in limestone and dolostone, occasionally in concretions and rarely as an efflorescence.

The Romans made concrete by mixing lime and volcanic ash to create a pozzolanic reaction. If this was mixed with volcanic tuff and placed under seawater, the seawater hydrated the lime in an exothermic reaction that solidified the mixture.

Aragonite

vug with aragonite east central ohio

Vug with aragonite crystals in arenaceous, ferruginous, fossiliferous limestone from Ohio

Photo By James St. John – Vug with aragonite crystals in arenaceous, ferruginous, fossiliferous limestone (Vinton Member, Logan Formation, Lower Mississippian; Mt. Calvary Cemetery Outcrop – Rt. 13 roadcut, Heath, east-central Ohio, USA) 3, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=82971990

With a name that sounds like a heroic character in J.R.R. Tolkien’s The Lord of the Rings, but originates from the territory of Aragon in Spain, aragonite is one of the three most common forms of calcium carbonate. Its crystal lattice differs from calcite, one of the other common forms of calcium carbonate. It has a host of industrial uses. Aragonite has been found in Coshocton County.

Celestite

Celestite Crystals inside Crystal Cave on South Bass Island

Crystal Cave is a small cave in Put-in-Bay on Lake Erie in Ohio touted as the world’s largest geode. An abundance of large, well-formed crystals of celestite cover the walls. The cave was originally mined for its strontium content, but enough nice crystals still remain to keep the site open as a show cave.

Photo by James St. John – Celestite (Crystal Cave, South Bass Island, Lake Erie, Ohio, USA) 16, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=82969277

A soft sulfate mineral ore of strontium, in fact being the most common mineral that contains strontium. Celestite derived strontium is used industrially in fireworks, ceramic magnets, and toothpaste

Ohio is famous for having some of the best celestite deposits in the world. The mineral is found in 11 counties. The northwestern regions of Ohio amid the Findlay Arch produce celestite ranging in color from white to pale blue. The area of Serpent Mound southwestern Ohio also produces some celestite due to an unusual geological occurrence. South Bass Island is a huge vug filled with very large celestite crystals.

Quartz

Geode with sphalerite barite dolomite and quartz Monroe County Ohio

Close-up of a Monroe County, Ohio geode with sphalerite, barite, dolomite and quartz.

Photo by James St. John – Geode with sphalerite, barite, dolomite, and quartz (Monroe County, Ohio, USA) 2, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=84692026

What can’t you not say about quartz? It is a hard silicate in the form of silicon dioxide. It’s useful in glassmaking, watchmaking, ceramics, metal casting, electronics, and the petroleum industry. But the enduring love it receives is because of it’s beauty and variety: rose quartz, lavender quartz, blue quartz, rutilated quartz, citrine, amethyst, enhydro quartz, prasiolite, ametrine and a variety of shapes including points, needles, and clusters.

In Ohio, quartz is found in flint beds in Coshocton, Licking, and Muskingum Counties; in Adams and Highland Counties; in septarian limestone concretions in the central portion of the state; and loose in streambeds and creeks in the Southeast.

Fluorite

Ohio Fluorite

An example of Ohio Fluorite from Stoneco Auglaize quarry (Maumee Stone County quarry), Junction, Paulding County, Ohio.

A 1.2 cm colorless cube with well-centered, distinct, rich purple color “phantom” inside. The crystal has very sharp faces and excellent gemminess. It sits upon a small amount of Dolostone matrix

Photo by Rob Lavinsky, iRocks.com – CC-BY-SA-3.0, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=10148353

Fluorite is a another name for calcium fluoride, a halide ore mineral of fluorine. It’s has several industrials uses including as a flux for removing impurities in the manufacture of steel and in the production of fluorine gas which itself is used in the refining of uranium.

While fluorite is found across the world, the quality and largest quantities are mined out of Europe and North America. In Ohio fluorite is found in 19 counties. Typically cubic crystals found in dolostones in northwestern Ohio particularly along the edges of the Findlay Arch and occasionally in the Serpent Mound area.

Some fluorite is UV reactive, fluorescing under exposure. Because of this property, it and it’s compounds are used to manufacture synthetic crystals with applications in laser and special UV and infrared optics.

Dolomite

Put-in-Bay Dolomite South Bass Island, Lake Erie,Ohio

Ohio Dolostone. In the past Dolomite was used to refer to both the mineral and the rock. Dolomite is now used to refer to the mineral and dolostone refers to sedimentary rock whose primary content is dolomite.

Photo By James St. John – Put-in-Bay Dolomite over Tymochtee Dolomite (Upper Silurian; South Bass Island, Lake Erie, Ohio, USA) 6, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=82969360

What relationship does Ohio have with a nineteenth century french geologist? The answer in one word is Dolomite! Named after Déodat Gratet de Dolomieu, Dolomite is found in over 19 Ohio counties. Dolomite differs from limestone in that it contains both calcium and magnesium.

More well known as an Indiana mineral, especially the Corydon area, this calcium magnesium carbonate occurs in small crystals in western Ohio and along the Huron river among other areas.

Dolomite has industrial uses including as a source of magnesium salts like magnesia and by builders as structural and ornamental stone.

The term dolomite used to refer both to the mineral dolomite and dolostone (a sedimentary rock of which is made primarily of dolomite).

Barite

Fluorite and barite (quarry in Marblehead Peninsula, far-northern Ohio

Fluorite and barite from Marblehead Peninsula Ohio

Photo By James St. John – Fluorite and barite (quarry in Marblehead Peninsula, far-northern Ohio, USA), CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=40022633

Found in over 26 counties in Ohio, this Barium Sulfate mineral often associated with calcite and other minerals is often white or colorless but can also have light blues, greys, yellows or browns. In the central and eastern Ohio black shale formations barite is found in concretions such as limestone, ironstone and pyrite. In the northwestern and southwestern Ohio crystalline or granular barite can be found in fractures and cavitiesof dolostones (dolomite sedimentary rock).

Barite is the primary ore for barium, and has varied industrial uses including paper, paint and glass manufacture as well medical radiology (as a dye) and in oil drilling.

Barites crystals found in Ohio can sometimes be massive in size.

Malachite

Malachite,Zaire

Malachite – sadly from Zaire and not Ohio

Photo By JJ Harrison (https://www.jjharrison.com.au/) – Own work, CC BY-SA 3.0,https://commons.wikimedia.org/w/index.php?curid=7515677

Typically found in botryoidal, stalagmitic, or fibrous masses, beautiful green malachite is collectible, and displayable.

It was a little hard to believe that malachite is found in Ohio, but according to the state it actually is present. Since it’s a copper carbonate hydroxide mineral it obviously needs copper to be present to form, and I did find a reference to a copper mine in Cuyahoga county.

Pyrite

Pyrite snake concretion Ohio Shale Upper Devonian creek cut in Ross County, southern Ohio, USA

Pyrite

Photo By James St. John – Pyrite snake concretion (Ohio Shale, Upper Devonian; creek cut in Ross County, southern Ohio, USA) 8, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=84692435

Iron Pyrite, commonly known as “fool’s gold”, is metallic iron sulfide mineral found in over 88 Ohio counties, typically in Devonian or Pennsylvanian shales. Pyrite has been used as an ore for sulfur and a source of iron.

The most common sulfide mineral, pyrite can form form in extremely well-crystallized examples of cubes, pyritohedrons, and octahedrons.

Sphalerite

Sphalerite on dolostone Millersville Quarry, Sandusky County, Ohio

Sphalerite crystals atop sucrosic dolostone from Sandusky County, Ohio

Photo by James St. John – https://www.flickr.com/photos/jsjgeology/31282767801/, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=101721070

Sphalerite is a sulfide mineral that is an ore of zinc, cadmium, gallium, germanium, and indium. It has a wide variety of colors including light/dark brown, red-brown, yellow, red, green, light blue, black, and colorless. It occurs in the Findlay Arch area, near Serpent Mound, and in Eastern Ohio.

Smithsonite

example of smithsonite

Illustrative example of smithsonite – sadly, not from Ohio. This example is from the Kelley Mine in Soccorro County, New Mexico.

Photo by Bureau of Mines – http://libraryphoto.cr.usgs.gov/cgi-bin/show_picture.cgi?ID=ID.%20BOM%20Mineral%20Specimens%20016, Public Domain, https://commons.wikimedia.org/w/index.php?curid=1825549

Smithsonite is named after English geologist and chemist James Smithson. Also known as zinc spar, this form of mineral zinc carbonate is a variably colored trigonal mineral.

Special Mention: Fossils

While not minerals, it would be unforgivable to not mention Ohio’s rich treasure trove of minerals. The greater Cincinnati area (which includes parts of northern Kentucky and southeastern Indiana) sits atop what is known as the Cincinnati Arch, the eroded remains of a mountain range from Michigan to Alabama that was thrust up by collision of two ancient continents. The arch sank beneath a series of shallow inland seas filled with marine life ending up as deposits of fossils in what is known to geologists as the Cincinnatian Epoch.

The region is famous for a wide variety of marine fossils, but particularly Trilobites, a now extinct member of the arthropod family.

Phacops rana,Silica,Ohio

Example of Ohio Eldredgeops rana fossil

Photo by Daderot – Own work, CC0, https://commons.wikimedia.org/w/index.php?curid=83993913

Graftonoceras – limonite-stained external mold of nautiloid in dolostone

Photo By James St. John – Graftonoceras fossil nautiloid (Lockport Dolomite, Middle Silurian; Coldwater, southern Mercer County, western Ohio, USA), CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=36833417

Graftonoceras fossil nautiloid (Lockport Dolomite, Middle Silurian;Coldwater,southern Mercer County).
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The Petrified Forest National Park in Arizona

In northeastern Arizona lies a region named El Desierto Pintado or The Painted Desert by Spanish explorers. In its midst is a 346 square region that is the Petrified Forest National Park. Part of the late Triassic Chinle Formation (which is formed of mudstone, siltstone, sandstone, and conglomerate deposited into channels and floodplains of a large river system) the park is part of a broader area famous for petrified fallen trees from forests that date to the Late Triassic Epoch, about 225 million years ago. Pushed upwards starting around 60 million years ago the upper layers were eroded away by wind and rain exposing fossils. A humans in the area only began about 8000 years ago, when migrants entered the region eventually growing corn, and building pit houses and pueblos. Changing climate conditions eventually drove the descendants of these settlers out of the area and into the Hopi and Navajo regions.

Arizona Petrified Wood Forest

Early Tourist Guide for the Petrified National Forest

Ever since the early 20th century, scientists have been unearthing and examining the rich fossils deposit in the Painted Forest. Giant reptiles called phytosaurs, large amphibians, and others have been discovered here, but the most famous fossils are those of plants of the Late Triassic Mesozoic period including ferns, lycophytes, cycads, gingkoes and others. At the time these plants and creatures lived, the park was part of the super-continent Pangaea, and located much further south, near the equator in fact, and the climate of the region was humid and sub-tropical, far different from the barren and arid deserts of today.

A view at Petrified Forest National Park, a site managed by the National Park Service in Arizona.


A view at Petrified Forest National Park, a site managed by the National Park Service in Arizona.

By AndrewKPepper – Own work, CC BY-SA 4.0, https://commons.wikimedia.org/w/index.php?curid=83635779

The most famous of plant fossils and the namesake of the park is petrified wood. These fossils were created when downed trees accumulated in river channels flooded by tropical rainstorms became buried by sediment containing volcanic ash from nearby volcanic that erupted periodically. The quick burial of these plants in an ash mineral rich, low oxygen environment proved ideal for fossilization as low oxygen inhibits the decay of organic matter and deters the presence of many hungry critters (from bacteria on up). Over time silica (silicon dioxide) from the ash dissolved into the water began to form quartz crystals (also a form of silicon dioxide) on edge of the logs eventually replacing the organic matter as it slowly decayed. Iron oxide and other substances in the ash created different colors in quartz minerals creating over a very long period of time beautiful, (sometime brilliantly) colorful plant fossils. There are rare specimens of green petrified wood fossils that also stand out, the green coming from chromium. These tree fossils are sometimes monumental in size, feet in diameter and sometimes the length of (broken) tree logs.

Detail inside petrified wood, Petrified Forest National Park, Arizona, USA


Detail of colorful petrified woodPetrified Forest National Park, Arizona, USA

By Brian W. Schaller – Own work, FAL, https://commons.wikimedia.org/w/index.php?curid=29628344

Green Petrified Wood from Holbrook, Navajo County, Arizona, USA Size: 3.8 x 2.1 x 1.6 cm. The bark on both sides is very well preserved. This is a polished slice from petrified tree limb

By Rob Lavinsky, iRocks.com – CC-BY-SA-3.0, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=10175980

Green Petrified Wood from Holbrook, Navajo County, Arizona

Green Petrified Wood fromSize: 4.0 x 2.0 x 1.5 cm. The bark on both sides is very well preserved. You can see the distinct knots, where smaller limbs were once attached and the corrugated nature of the bark.

By Rob Lavinsky, iRocks.com – CC-BY-SA-3.0, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=10176074

This fossilization process typically preserves details of the external shape and structure of the woody material including sometimes the bark, but in a small number of specimens the fossilization process penetrated into and preserved the cellular structure of the plant or animal bone. Paleologists and Paleobotanists can sometimes study these special fossils under a microscope to understand their cellular structure and this has brought a wealth of knowledge about species with no known relatives alive on the surface of the earth today.

At least nine species of extinct tree have been identified among the park’s fossils some growing up to 9 feet in diameter and up to 200 feet high. Perhaps the most famous of all is a conifer tree named Araucarioxylon arizonicum that grew from the Early Permian period through the Late Triassic. It’s closest living relatives are the Monkey Puzzle Tree and the the Norfolk Island Pine tree both of which only live in the southern hemisphere.

Artistic reconstruction of the plant Araucarioxylon arizonicum according to the descriptions given for the species from its Triassic fossil remains. The maximum height estimated for the species is 60 meters and its diameter is 60 centimeters. The columnar trunk with monopodic branching is observed and the lateral branches grow at an angle of 90º with respect to the axis and present negative geotropism. The structure of the leaves is unknown.


Artistic reconstruction of the plant Araucarioxylon arizonicum according to the descriptions given for the species from its Triassic fossil remains. The maximum height estimated for the species is 60 meters and its diameter is 60 centimeters. The columnar trunk with monopodic branching is observed and the lateral branches grow at an angle of 90º with respect to the axis and present negative geotropism. The structure of the leaves is unknown.

By Falconaumanni – Own work, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=37304138

Fossil Araucarioxylon arizonicum (petrified wood) outside the National Museum of Natural History, USA, in Washington, DC, USA.


Fossil Araucarioxylon arizonicum (petrified wood) outside the National Museum of Natural History, USA, in Washington, DC, USA.

By Daderot – Own work, CC0, https://commons.wikimedia.org/w/index.php?curid=27276482

There are other fossils as well, preserved through what is known as compression fossilization, which been preserved by being flattened by the weight of sediment accumulated above it until only a thin film of fossil remains. These types of fossils have preserved leaves, seeds, pine-cone, spore, fish, insects, pollen grains and sometimes animal remains.

Recently scientists in the park retrieved a quarter mile deep core sample to understand the history of the earth better. One of the questions they trying to answer is whether three the impact of at least three mountain sized asteroids created a tectonic movement leading to the eruption of chains of volcanoes could have been the key cataclysmic event that ripped apart Pangaea – the earth’s single supercontinent at the time. It turns out the core provides evidence of two different potential story arcs: the change in the fossil record at the time could be connected to powerful asteroid impact in Canada which left behind a 62 mile wide impact crater, or that no single catastrophic event was responsible for the.

Incidentally, Petrified wood is not limited to Arizona. It occurs anywhere the conditions are right. For example, we’ve previously written about the petrified forest in the protected national monument on the Greek Island of Nesbos. Namibia too, has an exceptional petrified forest national park. Discovered by a pair of farmers in the 1950s, the enormous fossilized tree trunks in this case did not originate in the area where they were found, but instead were washed downstream of a river by a great flood. These trees date back to about 280 million years ago.


Typical Veld Landscape near Petrified forest in Namibia



Typical Veld Landscape near Petrified forest in Namibia

By Olga Ernst – Own work, CC BY-SA 4.0, https://commons.wikimedia.org/w/index.php?curid=72029500

Petrified wood in Namibia.


Petrified Wood in Namibia

By t_y_l – P9133880, CC BY-SA 2.0, https://commons.wikimedia.org/w/index.php?curid=76429571

Petrified Wood in Namibia


Petrified Wood in Namibia

CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=1274653

Closeup view of Namibian Petrified Wood



Closeup view of Namibian Petrified Wood

By Lidine Mia – Own work, CC BY-SA 4.0, https://commons.wikimedia.org/w/index.php?curid=99649068

Petrified wood is found all around the region in Arizona including outside the Petrified Wood National Park, but don’t forget when visiting the park itself that it is both illegal and unethical to take fossils from public land! Do the right thing and enjoy the fossils in their natural place in the park and go home with beautiful memories and photographs.


Originally built with agatized wood blocks and mud mortar, Agate House likely housed a single family sometime between 1050 and 1300, during the Late Pueblo II – Pueblo III Periods. The scarcity of artifacts suggests a relatively brief occupation. Due to its relatively large size, Agate House may have served as a central gathering place. Indeed, Agate House was a part of a much larger community. When first recorded by archeologists in the 1930s, the petrified wood construction of Agate House was thought to be unique. Since then, hundreds of similar petrified wood structure sites have been found in the park, indicating a history of humanity as colorful and diverse as the building blocks of Agate House. Agate House @ Petrified Forest National Park, Arizona

By daveynin – https://www.flickr.com/photos/44124370018@N01/49518910517/, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=88114729

We have our own petrified forest of sorts at Georarities! Visit our Petrified Wood category to find samples of Arizona, Indonesian, green chromium petrified wood, and other varieties that you can buy for your collection!

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New Miocene Fossil Find in Australia

Fossil Fern

A spectacular new fossil trove has been reported in New South Wales, Australia. Located in the Central Tablelands regions, about 25 miles from the 19th century gold rush town of Gulgong, and named McGraths Flat after the person who discovered the fossil cache, the site is a window into the wetter and forest dominated past of Australia.

The fossil cache includes thousands of beautifully preserved specimens of flowering plants, ferns, spiders, insects and fish dating to the Miocene (23.03 to 5.33 million years ago) era. Climactic upheaval during the Miocene dried the rainforests that once covered Australia. At the time of the fossil cache’s formation the rainforest that had once covered the site had changed into temperate forest around a small lake. A fine goethite (an iron hydroxide mineral) matrix acted to help preserve plants and insects in the water. A diverse array of flowers, ferns, arachnids, insects and other soft bodied animals have been found in the fossil cache.

Image is illustrative of fossilized fern Dennstaedtia americana. Image by James St. John – https://www.flickr.com/photos/47445767@N05/39373225554/, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=97215903

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Electrifying Petrified Wood Discovery on the Island of Lesbos, Greece

Petrified Wood Trunk on the Island of Lesbos

The Greek island of Lesbos is notable for it’s Petrifed Wood forest, a protected national monument. The forest is located on the western portion of the island and was formed from the Late Oligocene to Lower–Middle Miocene and consists of  silicified remnants of a sub-tropical forest that going back 20–15 million years ago.

Recent discoveries in the rich Petrified Forest have been electrifying. First was the rare discovery of a spectacular 19.5 meter long log , with accompanying roots, branches, and trees, the only found to date in over 25 years of excavations. Weeks later, the excavators uncovered over 150 more petrified wood logs and petrified wood stumps including conifers, fruit producing trees, sequoia trees, pine, palm, cinnamon and oak trees. The finds were all discovered in the same pit.

The excavation team has been working since 2013 excavating along a 20km stretch of highway and have made 15 major finds, but these all pale to this most recent discovery, which was actually the result of a lucky accident. One the excavators notices a leaf in a stretch of the highway about to get asphalted, and halted the road work.

The park has been designated a UNESCO Global GeoPark. There is an excellent museum well worth visiting. If you visit the park, remember that the removal and transfer of fossilized material is prohibited by law. The forest includes six parks. The fossilized trees include mainly huge sequoias and primitive pine trees in an ecosystem closest to the coniferous forests of North America.

While we haven’t been to Lesbos we do have some of our own spectacular Petrified Wood finds available for sale in our catalog.

Top image is of Petrified Forest on the Island of Lesbos, Greece, by C messier – Own work, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=8926168

Petrified Wood near Sigri, Island of Lesbos, Greece. Photo By Rutger2 at nl.wikipedia, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=3222318

Petrified Wood, Island of Lesbos, Greece. Photo by Signy – Own work, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=11642494

Unstable temperature and relative humidity, different rates of expansion and contraction, salt movement, living plant roots and other factors cause cracking in fossil wood. In order to prevent dirt and contemporary vegetation from accumulating into the cracks, and prevent breakages, solutions of especially prepared consolidants are injected in surface cracks. [Kyriazi, E. and Zouros, N. (2008) ‘Conserving the Lesvos Petrified Forest’, Studies in Conservation 53 (Supplement-1 – Conservation and Access: Contributions to the 2008 IIC Congress), London, p. 141-145] The beautiful rose colours of the silicified fossil wood in this picture are due to the presence of manganese ions. Photo by E.Kyriazi – Own work, CC BY-SA 4.0, https://commons.wikimedia.org/w/index.php?curid=44800562

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Short Crystal: Quartz and the Fossilized Bird

Photograph of the holotype of Zhouornis hani, a type of Enantiornithes

A recent study in Frontiers in Earth Science reveals that researchers discovered quartz crystals in the stomach of a bird that lived alongside the dinosaurs. The bird, a member of the Enantiornithes clade of fossil birds, appeared to be a sensational discovery, as previously there had never been a find which preserved any traces of food in the fossils stomach which would clue researchers in to the diet of the animal. Many modern birds have what’s called a gizzard, a thick and muscular portion of the stomach used to help digest food. Often birds swallow small stones know as gizzard stones, which make their way to the gizzard itself where it helps to crush tough or difficult to digest food. These stones are know as gastroliths and have been found in some dino and bird fossils providing hints as to the diet of those animals. The presense of stones in the stomach, though isn’t defiinitive as to the purpose of the stones. There are some modern birtds of prey that swallow rocks to help move material through their digestive tract, cleaning it out, and it’s hard to differentiate between a gastrolith and a gastrolith that is a gizzard stone without knowing anything about the diet and habits of the animal using the stone. In the end, the reesearchers determined that the quart material found where the birds stomach would have been probably was a gastrolight at all. After exposing the supposed gastroliths to X-rays and a scanning electron microscope it was determined that the rocks were actually chalcedony crystals, quartz that grew in sedimentary rocks. There is evidence of chalcedony crystals forming with a clamshell, or replacing minerals in fossil bones. Furthermore, the crystals in this case were all connected in a thin sheet rather than separate rocks. The rocks were also much larger than would be expected of rocks swallowed by a bird that size. In the end there just wasn’t enough evidence, and some negative evidence against the idea that the rocks were in the birds stomach. Just goes to show, never count your gastroliths before they’s been swallowed.

We don’t have any examples of Enantiornithes, but you can check our our collection of fossils for sale here.

Top image is a photograph of the holotype of Zhouornis hani, a type of Enantiornithes,
By Yuguang Zhang, Jingmai O’Connor, Liu Di, Meng Qingjin, Trond Sigurdsen, Luis M. Chiappe​ – https://peerj.com/articles/407/, CC BY 4.0, https://commons.wikimedia.org/w/index.php?curid=33060650