Where can i get petrified wood

It forms when plant material is buried by sediment and protected from decay due to oxygen and organisms. Then, groundwater rich in dissolved solids flows through the sediment, replacing the original plant material with silica , calcite , pyrite , or another inorganic material such as opal. The result is a fossil of the original woody material that often exhibits preserved details of the bark, wood, and cellular structures. Some specimens of petrified wood are such accurate preservations that people do not realize they are fossils until they pick them up and are shocked by their weight.

These specimens with near-perfect preservation are unusual; however, specimens that exhibit clearly recognizable bark and woody structures are very common. At the top of the gulley, a "pedestal log" is suspended on a column of Chinle Formation. When the Chinle weathers away, the log will be lowered to the ground surface.

Image by Petrified Forest National Park. Petrified wood: A nice piece of petrified wood representing a limb cross section. This specimen shows the growth rings, cellular structure, and external bark. Specimen is about six inches across. The most famous locality for observing petrified wood is Petrified Forest National Park near the community of Holbrook in northeastern Arizona. About million years ago, this area was a lowland with a tropical climate and covered by a dense forest.

Rivers flooded by tropical rain storms washed mud and other sediments into the lowlands. Enormous coniferous trees up to 9 feet in diameter and feet tall lived and died in these lowlands. Fallen trees and broken branches were often buried by the river sediments. Nearby volcanoes erupted numerous times. These eruptions blanketed the area in volcanic ash with a high silica content.

Rapid burial allowed the plant debris to escape destruction by oxygen and insects. The soluble ash was dissolved by groundwater flowing through the sediments. The dissolved ash served as a source of silica that replaced the plant debris, creating petrified wood. Trace amounts of iron, manganese and other minerals were included in the silica and gave the petrified wood a variety of colors. These sediments, plant debris, and volcanic ash became part of a rock unit known today as the Chinle Formation.

In the millions of years after the Chinle Formation was deposited, the area was uplifted and the rocks deposited above the Chinle were eroded away. The petrified wood is much harder and resistant to weathering than the mud rocks and ash deposits of the Chinle. Instead of eroding away, the wood accumulated on the ground surface as the surrounding mud rocks and ash layers were eroded away.

That is why areas of the Park are covered with a litter of petrified wood trunks, branches and fragments. Today, visitors to the park can observe the petrified wood and photograph it; however, collecting petrified wood in the park is prohibited.

Peanut wood: A close-up of a slice of petrified wood from Australia known as "peanut wood" because of its white markings the size and shape of peanuts.

The "peanuts" are actually boreholes made in the wood by a shipworm which is a tiny species of clam. If you look closely you can see a spiral-shaped boring that traverses the width of this image second row from the bottom. Learn more about peanut wood. Petrified wood is not rare. It is found in volcanic deposits and sedimentary rocks at many of locations worldwide. Different minerals impart different colors to the resulting stone. For example, iron oxides create red, brown, or yellow hues, while carbon turns the stone black.

Satyamani Natural petrified Wood Fossil Showpiece is a powerful protective stone that helps one feel connected to Nature. It is a grounding stone, which is calming and good for meditation. It teaches patience, and is useful for removing obstacles and achieving goals. Petrified Wood is said to be an excellent stone for business success.

When you buy through links on our site, we may earn an affiliate commission at no additional cost to you. Have you ever looked down on the ground and a rock caught your eye? But when you pick it up you notice somethings different about it.

Or is it? It looks just like a piece of wood. It has wood grain just like a piece of wood would have. But its hard like a stone, and solid as a rock. But over millions of years, that piece of wood became a fossil. Petrified wood forms when trees that die millions of years ago fell and became covered in mud, sand and water. Over time, minerals seeped into the wood of the trees depositing minerals. Eventually, the wood rotted away and the only the minerals remained.

This entire process is called petrification. Unlike other types of fossils which are typically impressions or compressions, petrified wood is a three-dimensional representation of the original organic material.

So why do so many people like to collect petrified wood? One of the most popular reasons is because petrified wood is considered a gemstone. Just like other gemstones , you can polish petrified wood and create things like jewelry and even furniture. In some instances, petrified wood is even considered very valuable and can be sold for quite a profit. There are many places you can find petrified wood. As a matter of fact, there are entire petrified forests. Below I list some of the more popular locations in some of the more popular states in the US to find petrified wood.

You can hunt for and find fossilized wood in your own back yard! The best place to look for fossilized wood in my opinion is in or near water.