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Earth Science Week is celebrated the second full week of October throughout the nation as well as in other countries. The purpose is to increase public understanding and appreciation of the Earth sciences. Launched in 1998 by the American Geosciences Institute, efforts have grown on local, national, and international levels to highlight the vital role Earth sciences play in society’s use of resources and interaction with the environment.

Learn about the Earth and its processes with this self-guided experience into Earth science topics, created by the UGS for teachers, parents, students, and the public.

For the desktop-friendly version of this page, click here.

Scroll down for Earth Science Week activities or select a topic to jump to a specific section.

Rocks and Minerals Dinosaurs and Fossils Stream Erosion Earthquakes and Hazards

Rocks & Minerals

Geology is the study of Earth as it pertains to the composition, structure, and origin of its rocks. Rocks are classified based on how they formed and what minerals are in the rock. Minerals are classified by their chemical composition. 

In this Section:

Rocks and Minerals Videos and Photos

Rocks vs. Minerals Information

Teaching Materials and Publications

Interactive Maps

Rocks and Minerals Videos and Photos

Select a subject below to open the informational video.

Pyrope garnets gathered from harvester ant mounds. The roundish crystal habit of the garnets and their relatively high specific gravity lets them roll down to the perimeter of the nest cone for easy gathering. Garnets approach a carat in weight. Photo: Mouser Williams http://flickr.com/photos/mouser-nerdbot/. Used with permission.
MineralsRocks are made of minerals that come in thousands of varieties. Learn how we identify and classify minerals.
Igneous RocksVolcanoes, magma, and lava create some of the youngest rocks on Earth in many different forms and sizes.
Liquefaction features in Navajo Sandstone, Paria Plateau, Kane County. Paria Plateau, Kane County, Utah Photographer: Tyler Knudsen; © 2013
Sedimentary RocksFormed from weathering and erosion, deposition, and cementation, sedimentary rocks are the most common rocks on Earth’s surface.
Folded pegmatite vein in Farmington Canyon Complex gneiss, Pearsons Canyon, Box Elder County. Pearsons Canyon, Box Elder County, Utah Photographer: Adam McKean; © 2014
Metamorphic RocksHeat and pressure are the ingredients to create a metamorphic rock. Learn about some of the oldest rocks on Earth through metamorphism.
Glad You Asked - Utah Coal, Good, Bad, or Ugly
Glad You Asked - Utah Coal, Good, Bad, or Ugly
A close-up of quartzite ashlar blocks and a boulder; rock hammer for scale at West Mountain Community Pit.
A close-up of quartzite ashlar blocks and a boulder; rock hammer for scale at West Mountain Community Pit.
Banded white marble and quartz augen (eyeshaped crystals) in gray argillite, Notch Peak, Millard County. Photographer: Mark Milligan; © 2014
Banded white marble and quartz augen (eyeshaped crystals) in gray argillite, Notch Peak, Millard County. Photographer: Mark Milligan; © 2014

Rocks vs. Minerals

From the United States Geological Survey (USGS) the difference between rocks and minerals is defined as:

Rocks

Rock comes from the Latin rocca, meaning “rock” or “stone.”

Rocks are made of different kinds of minerals, or broken pieces of crystals, or broken pieces of rocks. Some rocks are made of the shells of once-living animals, or of compressed pieces of plants. A good way to think about it is if a chocolate chip cookie was a rock, then the flour, sugar, butter, and chocolate chips are the minerals that make up that rock! Rocks can be divided into three types. These categories are igneous, sedimentary, and metamorphic.

Read More

What are Igneous, Sedimentary, & Metamorphic Rocks?

Minerals

Mineral comes from the Latin mineralis, meaning “something mined.”

Minerals are naturally occurring inorganic elements or compounds having an orderly internal structure and characteristic chemical composition, crystal form, and physical properties. Minerals generally form crystals and have specific physical and chemical properties which can be used to identify them. Sometimes single minerals form rocks, as in quartz. Quartz is the most common form of crystalline silica and is the second most common mineral on the earth’s surface.

Read More

How Do Geologists Identify Minerals?

Teaching Materials & Publications

El Ciclo De Las Rocas (Spanish Version)

Contact the Natural Resources Map & Bookstore for print posters and publications.

Or check out a UGS Teaching Kit, available for use in the classroom.

Interactive Maps

All 2 /rocks and minerals 2
GeoSights Tour

GeoSights

Explore Utah’s lesser-known geologic wonders.
Miocene-age granite in the Mineral Mountains glows as the sun sets over the distant San Francisco Mountains near Milford.Christian Hardwick

Utah Rockhounder

Collect rocks, minerals, fossils, and landscape rocks.
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Dinosaurs & Fossils

There are a wide variety of fossils native to Utah. Some of the most common fossils are of marine life like shells, coral, and trilobites. Plant and other land-based fossils are also native to Utah and include dinosaurs, Ice Age animals, and leaves.

Visitor Information Guide to Fossils in Utah

In this Section:

Fossils in Utah Interactive Map

Digging Dinosaurs Video

Utah in the Age of Dinosaurs Information

Tracks and Tracksites Information

Dinosaur and Fossil Photos

Digging Dinosaurs Video

Video: Digging Dinos at Doelling’s Bowl

Utah in the Age of Dinosaurs

Survey Notes 47-3 Megablock

Dinosaurs lived only during the Mesozoic Era, which is often called the “Age of Dinosaurs.” Utah has perhaps the best Mesozoic rock record in the world.

The Mesozoic Era (252 to 66 million years ago) is divided into three time periods:

Triassic Period – 252 to 201 million years ago

The first dinosaurs lived near the end of the Triassic. Eoraptor, a bipedal carnivore recently discovered in South America, is the earliest known dinosaur.

Triassic dinosaurs have not yet been found in Utah. Late Triassic rocks known as the Chinle Formation are exposed throughout southern and eastern Utah as well as Arizona and New Mexico. This rock unit has yielded abundant remains of the carnivorous (meat-eating) dinosaur Coelophysis in Arizona and New Mexico. Although no Triassic dinosaurs have been discovered in Utah, the state hosts a plethora of dinosaur fossils, so it is only a matter of time before Triassic-age fossils are found.

Jurassic Period – 201 to 145 million years ago

During the Early and Middle Jurassic, Utah was mostly desert, although periodically sea level would rise and the sea would invade this sand dune-covered landscape. The great sandstone cliffs of Zion and Arches National Park are basically fossil sand dunes. Although dinosaur footprints are known from many sites in Utah, no dinosaur skeletons have yet been found in these desert rocks. Marine reptiles have been found in marine rocks near Dinosaur National Monument.

Most of Utah’s well-known dinosaur fossils are Late Jurassic dinosaurs. They are found mainly in a rock unit known as the Morrison Formation which dates to approximately 150 million years ago.

Dinosaurs are divided into two major groups, the saurischian, or “lizard-hipped,” dinosaurs and the ornithischian, or “bird-hipped,” dinosaurs.

  • The saurischian dinosaurs include the herbivorous (plant eaters), quadrupedal sauropods, and the carnivorous, bipedal theropods.
  • The ornithischian dinosaurs are all herbivorous and are composed of many groups, including stegosaurs, ornithopods, and ceratopsians.

Birds evolved from a group of thesaurischian theropods known as coelurosaurs.

Dinosaur fossils from the Morrison Formation can be found in Utah at the Dinosaur National Monument quarry in northeastern Utah and at the Cleveland-Lloyd Dinosaur Quarry in east-central Utah. Allosaurus is Utah’s State Fossil. Allosaurus is a carnivorous theropod found in abundance at the Cleveland-Lloyd Dinosaur Quarry.

Jurassic Dinosaurs of Utah

Cretaceous Period – 145 to 66 million years ago

Early Cretaceous dinosaur fossils are found in Utah in the Cedar Mountain Formation, which dates to about 125 to 98 million years ago. This rock unit overlies the Morrison Formation, but represents more time and contains several entirely different faunas or groups of dinosaurs. These rocks represent a time when North America was connected to Europe before flowering plants, a period when rising sea levels led to the isolation of North America from the rest of the world, and finally a time when the first land connections with Asia were established and flowering plants had come into their own. The Cedar Mountain Formation is the basis of considerable research by UGS paleontologists.

Late Cretaceous dinosaurs such as Tyrannosaurus and Torosaurus lived about 65 million years ago at the end of the age of dinosaurs. Cretaceous dinosaur sites are found in great abundance in Montana and Alberta, Canada, and are also found in the North Horn Formation of central Utah. Further south in the Grand Staircase – Escalante National Monument the most continuous record of Cretaceous dinosaurs in the world has now been recognized and research is just beginning to bring these many undescribed Utah dinosaurs to light.

Early Cretaceous Dinosaurs of Utah

Late Cretaceous Dinosaurs of Utah

Tracks & Tracksites

Tracks and tracksites are types of trace fossils, also called ichnofossils, which are imprints left behind by an animal.

Artist conception of the plants and animals living in the Jurassic Navajo erg (sand sea). Note the two Tritylodons and their Brasilichnium trackways. Illustration by Russell Hawley.

A Glimpse into the past

Artist conception of the plants and animals living in the Jurassic Navajo erg (sand sea). Note the two Tritylodons and their Brasilichnium trackways. Illustration by Russell Hawley.

Dinosaur tracks on a block of fallen Jurassic-age Navajo Sandstone. North of the confluence of the San Juan and Colorado Rivers, Glen Canyon National Recreation Area, San Juan County. Photographer: Don DeBlieux; © 2011
Dinosaur tracks on a block of fallen Jurassic-age Navajo Sandstone. North of the confluence of the San Juan and Colorado Rivers, Glen Canyon National Recreation Area, San Juan County. Photographer: Don DeBlieux; © 2011
Visitor Information Guide to Fossils in Utah Where to see Utah's fossils and dinosaurs
Visitor Information Guide to Fossils in Utah Where to see Utah's fossils and dinosaurs
Glad You Asked - Sidewalk Tracks
Glad You Asked - Sidewalk Tracks
St. George Dinosaur Discovery Site at Johnson Farm
St. George Dinosaur Discovery Site at Johnson Farm

Tracks and Tracksites

Examples of tracks include claw marks, dewclaws, footpads, skin impressions, and tail drags. Tracks and other trace fossils can be good evidence for the size and identity of the animals that made them. Behaviors like eating habits, migration paths, and walking mechanics can also be inferred from some tracks if they are preserved well.

How are Tracks Formed and Preserved?

During times when the water levels dropped on shallow lake shores, swamps, coastal areas, and rivers, the animals walked in the mud along the shore, leaving footprints that then filled in with silt and sand – all of which later hardened into stone. Thus, many of the tracks are preserved as bumps (natural casts) instead of impressions. The track casts are mostly found on the underside of a sandstone layer that overlies the mudstone in which the tracks were formed.

Where are Tracks and Tracksites Located in Utah

In Utah, tracks can be found in many places like the St. George Dinosaur Discovery Site at Johnson Farm and at Flaming Gorge Reservoir, among other places. Visit our interactive map to locate and visit some tracksites for yourself!

Dinosaur and Fossil Photos

Click on the photos below to view them full-screen with descriptions.

A double track of hadrosaur (plant-eating duck-billed dinosaur) footprints preserved as natural casts in an Iron Springs Formation boulder along the trail at the Parowan Gap Dinosaur Track Site. Scale bar on left is 6.5 inches long. Photographer: James Kirkland
A double track of hadrosaur (plant-eating duck-billed dinosaur) footprints preserved as natural casts in an Iron Springs Formation boulder along the trail at the Parowan Gap Dinosaur Track Site. Scale bar on left is 6.5 inches long. Photographer: James Kirkland
A volunteer excavates the limb bones of sauropod dinosaurs at the Hanksville-Burpee Dinosaur Quarry. Deposited in flowing water, these bones came to rest against one another forming a logjam of bones.
A volunteer excavates the limb bones of sauropod dinosaurs at the Hanksville-Burpee Dinosaur Quarry. Deposited in flowing water, these bones came to rest against one another forming a logjam of bones.
A rock with the texture of preserved dinosaur skin.
A rock with the texture of preserved dinosaur skin.
Earth Science Week 2014
Earth Science Week 2014
UGS fossil preparator Don DeBlieux removes iguanodont bones from a plaster field jacket.
UGS fossil preparator Don DeBlieux removes iguanodont bones from a plaster field jacket.
Cephalopod fossil in the Mississippian-age Great Blue Limestone along the crest of the Wellsville Mountains, Cache County. Photographer: Stefan Kirby
Cephalopod fossil in the Mississippian-age Great Blue Limestone along the crest of the Wellsville Mountains, Cache County. Photographer: Stefan Kirby
A collection of trilobite fossils on a rock of varying sizes.
A collection of trilobite fossils on a rock of varying sizes.
Gar fish fossil found in a well core sample.
Gar fish fossil found in a well core sample.
Visitor Information Guide to Fossils in Utah Where to see Utah's fossils and dinosaurs
Visitor Information Guide to Fossils in Utah Where to see Utah's fossils and dinosaurs
Detail of late Pleistocene life in central Utah from a mural painted by Joe Venus at the College of Eastern Utah Prehistoric Museum.
Detail of late Pleistocene life in central Utah from a mural painted by Joe Venus at the College of Eastern Utah Prehistoric Museum.
Survey Notes 47-3 Megablock
Survey Notes 47-3 Megablock
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Stream Erosion

Rivers or streams behave as systems. If one part of the stream channel is disturbed, changes will occur in the upstream and downstream direction. Stream tables are used in experiments where geologists can learn more about how rivers form, change, and affect surrounding rock and sediments. Geologists also use satellite imagery to piece together a stream channel’s history and infer its future.

In this Section

Stream Table Timelapse Video

Helpful Definitions

Stream Table Demo Videos

Ucayali River Videos

Stream Erosion Photos

Stream Table Timelapse Video

Video: Stream Table Time-lapse – BYU’s College of Physical and Mathematical Sciences

In this video, make observations on what shapes form and change in this river in different environments. What recurring shapes do you see? The different colored “sediments” represent more- or less-heavy material. Where do the different colors get deposited compared to each other?

Helpful Definitions:

  • EROSION – The process by which soil and rock are removed from one area of the Earth through natural causes such as wind, water, and ice and transported elsewhere.
  • DEPOSITION – The geological process where material is added to a landform.
  • DELTA – A piece of land in the shape of a triangle or fan made by sediment deposited at the mouth of a river.
  • FLOODPLAIN – Low, flat land along a stream that is flooded when the stream overflows.
  • MEANDER – A curve in a river. Meanders form a snake-like pattern as the rivers flow across fairly flat valley floors.
  • BRAIDED RIVER – A river that has lots of small channels that continually split and join. Braided rivers are usually wide but shallow.
  • OXBOW LAKE – A U-shaped lake created when a meander of a river is cut off as the river erodes a new path.

Stream Table Demos

Video: Delta Formation – Little River Research and Design

A river channel goes through many changes as it forms a delta.

Key concepts to take note of this video:

  • Meandering and braided streams change form dependent on stream slope, and water and sediment supply.
  • Deltas are landforms built of sediments near a stream’s mouth when the stream enters slow or still water. In this example, still water allows for a fan-shaped delta.

Video: Vegetation Experiments – Little River Research and Design

Vegetation makes a big difference in the amount of erosion that occurs in a river system.

Key concepts to take note of this video:

  • Vegetation hinders erosion—in these examples, from a cutbank along the stream and from wave action along the shoreline.
  • Flooding and high waves can accelerate erosion, vegetation protects stream banks and beaches.

Real-World Changing River System – Ucayali River, Peru

Video: Ucayali River – Satellite timelapse

The Ucayali River has a long history of changing river channels.

Key concepts to take note of this video:

  • Meandering streams migrate over time as erosion and deposition alter the easiest route for water to flow.
  • Older, abandoned stream channels can be seen as swirly shapes and lakes on the landscape surrounding the current stream channel.

Video: Watch an Oxbow Lake Form – Geography Realm

An oxbow lake forms in a meander of the Ucayali River.

Key concepts to take note of this video:

  • Oxbow lakes form when stream channels alter course and cut off river meanders.

Stream Erosion Photos

Click on the photos below to view them full-screen with descriptions.

A bird-foot delta forms as Lee Creek sinuously winds through mud flats along the southeastern shore of Great Salt Lake. Aerial view from a drone. Photographer: Adam Hiscock 2018
A bird-foot delta forms as Lee Creek sinuously winds through mud flats along the southeastern shore of Great Salt Lake. Aerial view from a drone. Photographer: Adam Hiscock 2018
Stream erosion during uplift of the Colorado Plateau incised the Green River channel deep into the Triassic–Jurassic-age Wingate Sandstone and underlying Chinle Formation. At Bowknot Bend, the channel turns back on itself in a huge meander loop. Horseshoe Canyon Wilderness Study Area, Emery County, Utah Photographer: Sonja Heuscher
Stream erosion during uplift of the Colorado Plateau incised the Green River channel deep into the Triassic–Jurassic-age Wingate Sandstone and underlying Chinle Formation. At Bowknot Bend, the channel turns back on itself in a huge meander loop. Horseshoe Canyon Wilderness Study Area, Emery County, Utah Photographer: Sonja Heuscher
Whirlpool Canyon from Harpers Corner, Colorado (view west into Utah), showing Precambrian-age through Permian-age strata cut by the Green River.
Whirlpool Canyon from Harpers Corner, Colorado (view west into Utah), showing Precambrian-age through Permian-age strata cut by the Green River.
Looking down on the Bear River showing the main channel and old meander scars and oxbows.
Looking down on the Bear River showing the main channel and old meander scars and oxbows.
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Earthquakes & Hazards

Geologic hazards are geologic conditions that may cause substantial loss or damage to property, damage to the environment and economy, health risks, injury, or even death. Geologic hazards that affect Utah include earthquakes, landslides, flooding, problem soils and rocks, and volcanic hazards. We can live and deal with geologic hazards by understanding what they are, where they exist, how large or difficult they are, and how to effectively mitigate them.

Utah has experienced 17 earthquakes greater than magnitude (M) 5.5 since pioneer settlement in 1847, and geologic investigations of our region’s faults indicate a long history of repeated large earthquakes of M 6.5 and greater prior to settlement.

In this Section:

Earthquakes Virtual Field Trip Video

Utah Earthquakes Story Map

Geologic Hazard Photos

Earthquakes Virtual Field Trip Video

Video: Natural History Museum of Utah Virtual Field Trip, Earthquake!

View all NHMU virtual field trips

Utah Earthquakes Story Map

Large Earthquakes on the Wasatch Fault

A timeline of earthquakes through geologic time

Geologic Hazard Photos

Click on the photos below to view them full-screen with descriptions.

In Utah’s only historical surface-rupturing earthquake event, the ground was displaced about 0.5 meters (1.5 ft) from the 1934 Hansel Valley M6.6 earthquake.
In Utah’s only historical surface-rupturing earthquake event, the ground was displaced about 0.5 meters (1.5 ft) from the 1934 Hansel Valley M6.6 earthquake.
The Manefay landslide at the Bingham Canyon open-pit copper mine on April 11, 2013. Also notable are the two different slides—the earlier light gray slide of pyritized Bingham Mine Formation quartz sandstones overlain by the yellow-brown, oxidized dump material which slid about 1.5 hours later. Multiple pieces of mining equipment caught up in the slide are barely visible at the toe of the slide in the lower left. Photo courtesy of Kennecott Utah Copper.
The Manefay landslide at the Bingham Canyon open-pit copper mine on April 11, 2013. Also notable are the two different slides—the earlier light gray slide of pyritized Bingham Mine Formation quartz sandstones overlain by the yellow-brown, oxidized dump material which slid about 1.5 hours later. Multiple pieces of mining equipment caught up in the slide are barely visible at the toe of the slide in the lower left. Photo courtesy of Kennecott Utah Copper.
An example of a clearly active landslide on the Wasatch Plateau in the Seely Creek drainage. The landslide shows a lack of vegetation, hummocky rough surface, and distinctive head and toe features. The lower landslide averaged 14 feet of movement per year between 2004 and 2009. Photograph taken September 24, 2009.
An example of a clearly active landslide on the Wasatch Plateau in the Seely Creek drainage. The landslide shows a lack of vegetation, hummocky rough surface, and distinctive head and toe features. The lower landslide averaged 14 feet of movement per year between 2004 and 2009. Photograph taken September 24, 2009.
Flooding along State Street, Salt Lake City, Utah, June 1983. Photo by S. Thiriot.
Flooding along State Street, Salt Lake City, Utah, June 1983. Photo by S. Thiriot.
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Teacher Resources

Learn more about our teacher resources at the UGS.

  • TEACHING KITS

    The UGS has teaching kits available for check out in topics such as landforms, rocks, minerals, and fossils, ice age, and dinosaurs. Call to reserve today!

  • FIELD TRIPS

    Discover guides, tours, and road logs on areas of geologic interest around the state. Among our guides are field trips to do on your own and virtual field trips.

  • CLASSROOM MEDIA

    View videos, photos, and downloadable content available for the classroom.  From the UGS YouTube channel, see scientists in the field, paleontology, the Wasatch fault, and more.

  • TEACHER WORKSHOPS

    Teacher workshops and educational classes are available from a variety of organizations. Contact and sign-up information here.

  • GLAD YOU ASKED ARTICLES

    Read the tri-annual Survey Notes column that answers general geologic questions on a variety of subjects.

View all teaching materials and topics from the UGS.

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