BE ADVISED: On Thursday, October 17 our museums will participate in a brief earthquake drill. Guests will hear an overhead announcement, but are not required to participate, nor will the building be evacuated. Please plan your visit accordingly or contact us at info@nhm.org or 213.763.DINO if you have any questions or would like to reschedule your visit.

Your Fossil Discovery

Man in plaid shirt standing over rock. Child and woman in background

Fossils provide a valuable record of the plants, animal life, and environmental conditions from millions or even billions of years ago! What should you do if you think you found a fossil in your neighborhood?

The guide below from our Museum staff will help move you through the fun and informative process of scientific discovery.

 I think I found a fossil; what should I do with it?

Woman sitting in desk holding fossils

Juliet Hook, Assistant Collections Manager, Invertebrate Paleontology, explains: 

If you think you found a fossil, the most important thing to do is to leave it exactly where you found it. 

When paleontologists study a fossil, it is very important to know precisely where it came from to learn more about it. The location can tell us how old the fossil is and what other fossils may be around it. Also, it is important to know that taking anything out of a national park or a publicly owned park is not allowed. Alert a park ranger or staff member from the park if you find something.

What exactly are fossils?

man sitting at desk with fossils

Jorge Velez-Jurabe, Associate Curator, Mammalogy (Marine Mammals) explains: 

A fossil is simply any evidence of life from the ancient past, which can include footprints, skin impressions, and fossilized feces called coprolites. Typically, the hard parts of an animal, such as its bones, are more likely to be preserved than soft tissues such as skin or hair.  Even fossils of bones are still relatively difficult to find. Among the most common fossils found around Los Angeles are the hard parts of marine animals, such as snail and clam shells. Take a look at the images below to see the variety of fossil types in the Museum’s collection.

fossil snails on rock

Natural History Museum of Los Angeles County

A slab of 50 million-year-old Turritella snail shells.

fossils on rock with hand showing size

Natural History Museum of Los Angeles County

A cut rock exposing two-three million-year-old snail and clam shells and impressions (molds).

Invert Paleo Fossil Shells

Natural History Museum of Los Angeles County

A drawer of mostly scallop and clam shells of varying age.

 A few of the six-million-year-old coprolites (fossilized feces) of extinct bone-crushing dogs; the one on the right has visible bits of bone sticking out. (Ouch.)

A few six-million-year-old coprolites (fossilized feces) of extinct bone-crushing dogs. The one on the right has visible bits of bone sticking out.

fossil bird footprints

Natural History Museum of Los Angeles County

Bird footprint impressions from the Eocene Green River Formation, Utah. These are body fossils, but rather trace- or ichno-fossils, a record of biological activity but not the preserved remains of a plant or animal itself.

Leaf Impression

Natural History Museum of Los Angeles County

Compressions of leaves from Paleocene age rocks of Wyoming. Compressions of leaves will be pressed flat in the sediment, and will often retain some evidence of organic material.

Shark Teeth Miocene

Natural History Museum of Los Angeles County - Invertebrate Paleontology

Shark teeth from Miocene age rocks from near Bakersfield, California.

Petrified wood

Natural History Museum of Los Angeles County

Examples of petrified wood from an unknown locality.

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A slab of 50 million-year-old Turritella snail shells.

Natural History Museum of Los Angeles County

A cut rock exposing two-three million-year-old snail and clam shells and impressions (molds).

Natural History Museum of Los Angeles County

A drawer of mostly scallop and clam shells of varying age.

Natural History Museum of Los Angeles County

A few six-million-year-old coprolites (fossilized feces) of extinct bone-crushing dogs. The one on the right has visible bits of bone sticking out.

Bird footprint impressions from the Eocene Green River Formation, Utah. These are body fossils, but rather trace- or ichno-fossils, a record of biological activity but not the preserved remains of a plant or animal itself.

Natural History Museum of Los Angeles County

Compressions of leaves from Paleocene age rocks of Wyoming. Compressions of leaves will be pressed flat in the sediment, and will often retain some evidence of organic material.

Natural History Museum of Los Angeles County

Shark teeth from Miocene age rocks from near Bakersfield, California.

Natural History Museum of Los Angeles County - Invertebrate Paleontology

Examples of petrified wood from an unknown locality.

Natural History Museum of Los Angeles County

Not all bones found underground are old enough to be fossils. Sometimes we find bones in the ground that have not yet turned to stone, such as this 100- year-old sheep bone dug up in Expo Park. This fossil can be seen in the L.A. Underwater: The Prehistoric Sea Beneath Us exhibition:

Fossil ID Sheep Bone

Sometimes we find objects that look similar to fossils but are actually called pseudofossils. Pseudofossils are made from inorganic (non-living) rocks that have been shaped by wind, water, and time to look like fossils. Below are examples of commonly found pseudofossils in Los Angeles. 

small round opals on rock

Natural History Museum of Los Angeles County

These hyalite opals found in San Pedro, California, are small and round in shape and can be mistaken as petrified fish eggs or the skin of a prehistoric animal. In reality, they are formed by silica and water introduced into rock formations when they are still hot and formed globular crusts as they cool.

Sandstone Concretion

Natural History Museum of Los Angeles County

Sandstone concretions, formed from sand grains cemented together by calcium carbonate. Concretions are commonly mistaken for fossil eggs, limb bones, or skulls according to their variable shape.

Rock with many holes

Natural History Museum of Los Angeles County

A modern colony of tube worms that have been eroded to resemble the spongy texture of a bone. These are commonly found on beaches and near tide pools.

rock with many fine cracks

Natural History Museum of Los Angeles County

Mudcracks, formed as muddy sediment dries, contracts, and cracks. Cracks can spread and join up forming a polygonal pattern. Mudcracks are sometimes mistaken for preserved skin.

Rock with eroded hole, lunar in shape

Natural History Museum of Los Angeles County

A geode is a hollow and often spherical rock, in which crystals have formed. Crystals are often precipitated from minerals in groundwater or hot fluids. In some cases, the geode might have originated from a fossil (e.g., a hollow clam or snail) but most often was not a fossil.

Layers of sediment formed by the growth of algae (stromatolite).

Natural History Museum of Los Angeles County

Layers of sediment formed by the growth of algae (stromatolite). While they were created by ancient organisms, geologists consider them to be biochemical structures rather than fossils.

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These hyalite opals found in San Pedro, California, are small and round in shape and can be mistaken as petrified fish eggs or the skin of a prehistoric animal. In reality, they are formed by silica and water introduced into rock formations when they are still hot and formed globular crusts as they cool.

Natural History Museum of Los Angeles County

Sandstone concretions, formed from sand grains cemented together by calcium carbonate. Concretions are commonly mistaken for fossil eggs, limb bones, or skulls according to their variable shape.

Natural History Museum of Los Angeles County

A modern colony of tube worms that have been eroded to resemble the spongy texture of a bone. These are commonly found on beaches and near tide pools.

Natural History Museum of Los Angeles County

Mudcracks, formed as muddy sediment dries, contracts, and cracks. Cracks can spread and join up forming a polygonal pattern. Mudcracks are sometimes mistaken for preserved skin.

Natural History Museum of Los Angeles County

A geode is a hollow and often spherical rock, in which crystals have formed. Crystals are often precipitated from minerals in groundwater or hot fluids. In some cases, the geode might have originated from a fossil (e.g., a hollow clam or snail) but most often was not a fossil.

Natural History Museum of Los Angeles County

Layers of sediment formed by the growth of algae (stromatolite). While they were created by ancient organisms, geologists consider them to be biochemical structures rather than fossils.

Natural History Museum of Los Angeles County

Documenting your discovery

Taking time to document your finding properly is a very important step. Follow the steps below to work through the process of science! 

We encourage you to download the DOING SCIENCE! Observations of My Discovery worksheet to help guide you. Note: Do not resize the document or scale to print. The scale bar on the margin is set to print on 8.5” x 11” paper.

To get started, gather your supplies. 

  1. Download and print DOING SCIENCE! Observations of My Discovery worksheet (Note: Do not resize the document or scale to print. The scale bar on the margin is set to print on 8.5” x 11” paper.) If you don’t have access to a printer, grab a notebook and a ruler with centimeters. 
  2. Grab a smartphone or camera and a map 

Step 1: Measuring your discovery 

Knowing the size of the object is essential. You can use a ruler or a scale bar to measure your discovery. In science, we use the metric scale to measure. 

A scale bar is a handy tool that can help you document what you found and is essential to someone helping you identify your discovery. A scale bar is included in this downloadable worksheet. 

Record the following measurements:

  • Length (cm)
  • Width (cm)
  • Depth (cm) 
Image showing how to measure objects
Measuring the length, width, and depth of your discovery allows you to capture the dimensions of your find and helps others to understand the form or shape of the object.

Step 2: Take photos of your discovery 

Place the printed scale bar next to the object. The photo below is an example of how to place your scale bar next to your object. If you don’t have a scale bar, you can use a ruler with centimeters (cm) instead. 

large shark tooth and scale bar
Prior to taking pictures of your object, place the scale bar next to your object so that the scale bar and your object are clearly visible. Pictured here is a megalodon shark (Carcharocles megalodon) tooth from the Museum collection. 
Natural History Museum of Los Angeles County

We suggest you take the following pictures of your object. Make sure to take pictures of the complete object before you zoom in on any interesting features you find.

  • Your discovery with a surrounding landmark
  • Your discovery and the scale bar from the top down
  • Your discovery and the scale bar from the right
  • Your discovery and the scale bar from the left
  • The underside of your discovery (only if you can safely turn it over)
  • Close up photos of any interesting parts of your discovery

Step 3: Describe where you found your discovery

The location where your object was found is very important. People who study fossils do detective work to determine how long ago rocks formed—it is hard to tell the age of a rock! The location of the rock can give you clues, so write down where the object was found. 

Take note of the following: 

  • The city where your discovery is located. 
  • Nearby landmarks— Permanent landmarks can be a street name, park name, or buildings— anything that is likely to be there if someone returns to the location in the future. 
  • GPS coordinates— Use a smartphone or ask an adult to help you get the GPS coordinates of your location. Below are steps to get your GPS coordinates from Google Maps on a smartphone. 
Fossil ID GPS 1

On your smartphone, open the Google Maps app.

Fossil ID GPS 2

Touch and hold down on the exact spot on the map where you found your discovery. A dropped pin will appear on the map.

Fossil ID GPS 3

Scroll up on the dropped pin to view more information.

Fossil ID GPS4

You will see a series of numbers separated by a comma—these are your coordinates! Be sure to note down this important information.

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On your smartphone, open the Google Maps app.

Touch and hold down on the exact spot on the map where you found your discovery. A dropped pin will appear on the map.

Scroll up on the dropped pin to view more information.

You will see a series of numbers separated by a comma—these are your coordinates! Be sure to note down this important information.

You can also find the location of your object on a geological map. The USGS Geological Map Viewer is particularly helpful for determining the geological rock unit that your fossil was derived from and in determining the age of that fossil.

Step 4: Describe your discovery 

Fossils come in a variety of shapes, sizes, and textures. These features help paleontologists recognize different species and understand relationships between species. To document your object, describe the following: 

  • Describe the shape of your discovery.
  • Draw a picture of what your discovery looks like. 
  • What does it feel like? (Is it smooth or bumpy? Does it have ribs or spines?)
  • What color is your discovery? (What colors do you see? Is it shiny or dull? How is it different from the rock around it?)
  • Has your discovery left an impression that is concave or convex? (Concave means that it curves inward or is hollowed out, like a cave. Convex is the opposite of concave and is rounded outward. This is hard to see in a picture, so be sure to describe it! 

Below are images showing the difference between concave and convex.

Illustration showing difference between concave and convex

Concave means that it curves inward or is hollowed out, like a cave. Convex is the opposite of concave and is rounded outward.

Camel Footprint Fossil

Natural History Museum of Los Angeles County

Fossil footprints of a medium-sized camel preserved in sandstone from Red Rock Canyon State Park. These footprints are concave because they go into the rock.

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Concave means that it curves inward or is hollowed out, like a cave. Convex is the opposite of concave and is rounded outward.

Fossil footprints of a medium-sized camel preserved in sandstone from Red Rock Canyon State Park. These footprints are concave because they go into the rock.

Natural History Museum of Los Angeles County

Step 5: Share what you found! 

One of the best parts of doing science is sharing what you found with others! Show pictures of your discovery to your friends, family, and teachers and tell them where you found it.

 


 

 I think I may have found a fossil.  How can I find out more about it? 

Laura Tewksbury Fossil ID

Laura Tewksbury, Preparator of Rancho La Brea, explains:

This is one of the most engaging parts of your scientific journey!  You may be able to get clues from other people who may have found objects similar to your discovery, so documenting what you found is important. From there, you can talk to park rangers or park educators (if your discovery was made in a park), teachers, or conduct online research to help you understand more about your discovery.   Here are some suggestions:  

Can the Museum help me identify my discovery? 

man at drawer with fossils

Austin Hendy, Assistant Curator of Invertebrate Paleontology, explains:

If you have gone through all the steps above and conducted your online research and are still stumped, we are happy to help you! Here is what you need to do:

Follow all of the steps listed above and save your information and photos—you will need them to complete the form below. The DOING SCIENCE! Observations of My Discovery worksheet helps guide you to gather the information you need to complete the form.  If you are under 18, ask for help and/or obtain parent/guardian permission to complete the form.  

 

Once you have completed the form, a Museum staff member will reach out to you within 4 to 6 weeks. It takes us a bit of time to process these requests for identification, so thank you in advance for your patience. 

Can I donate my discovery to the museum? 

Man in hat holding fossil

Tony Turner, Museum Educator, explains: 

The exciting part of finding a fossil is that YOU found one! Your curiosity about the natural world is a big part of doing science, and paleontologists follow the same steps when they find a fossil! 

The Natural History Museum and La Brea Tar Pits staff care for and study nearly 10 million fossils in the collection. So, we have to be very intentional about taking in fossils offered to us. Storage space is limited at our museums, so we only consider taking in fossils that help us fill in gaps of knowledge. More importantly, the objects must have documentation of being acquired legally and have precise information on where they were found. Without this information, we cannot conduct any scientific research. 

If your fossil is relevant to the Museums' collection, we may consider the donation after you complete the Fossil Identification Request Form. If we cannot take your fossil to the collection, we encourage you to keep it to enjoy and share your knowledge with others.