Rock Abrasion Activity Source: Association of American State Geologists. Adapted with permission. Rocks break down into smaller pieces through weathering. Rocks and sediment grinding against each other wear away surfaces. This type of weathering is called abrasion, and it happens as wind and water rush over rocks. The rocks become smoother as rough and jagged edges break off. In this activity, you will model how abrasion works. Materials For each person: [Read More]

Rock Around the World Activity Source: National Aeronautics and Space Administration and Arizona State University, 2006. Adapted with permission. Background Scientists need your help. Those studying Mars are asking students from around the world to help them understand “the red planet.” Send in a rock collected by you or your classroom from your region of the world, and NASA scientists will use a special tool like the one on the Mars Rover to tell you what it’s made of. [Read More]

Rock Art in the National Parks Activity Source: Views of the National Parks, National Park Service. Adapted with permission. Human beings have been linked to earth materials since prehistoric times. They used caves for shelter, shaped rocks into stone implements, and later refined metals to make tools. Beyond practical purposes, Earth materials also were used to make pigments for paint. Rock walls became canvases where ancient artists expressed themselves. In this exercise, we will explore the link between Earth materials and art. [Read More]

Rock Pop Activity Source: Geological Society of America. Adapted with permission. How can a cave form from solid rock? Most caves are found in limestone, a rock made of materials of calcium carbonate. This rock is unusual because the solid minerals it is made of easily dissolve in weak acids. The most common weak acid in the environment is actually water! This acid forms when carbon dioxide in the atmosphere dissolves in the rain water to form carbonic acid. [Read More]

Seismic Mapping Activity Source: The Society of Petroleum Engineers. Adapted with permission. Scientists use seismic technology to map patterns of rock formations below the surface of the Earth. Different types of rocks affect sound waves. Geologists use these sound waves to locate rocks that may contain oil and/or natural gas. You can explore this principle with a tuning fork and various rocks. Gently strike a fork against the rocks. Note variations in sounds produced by different rocks. [Read More]

ShakeAlert Earthquake Early Warning Activity Source: U.S. Geological Survey, Adapted with permission. Have you ever felt an earthquake? What was it like? Where were you? What did you do? More than 143 million people are exposed to potentially damaging shaking in the United States. When an earthquake happens, seismic waves travel outward in all directions. Primary (P) waves travel faster than secondary (S) waves, which do most damage. But electronic information can be sent faster than P and S waves. [Read More]

Shoebox Geologist Activity Source: Adapted with permission by National Park Service. Earth processes such as volcanic eruptions, floods, landslides, and glaciers leave behind evidence of their passing in the form of layers known as deposits . By studying deposits of recent geologic events, geologists are able to better understand older deposits and identify the processes that caused them. A fundamental principle of geology is the Law of Superposition, which states that younger layers will be deposited on top of older layers. [Read More]

Sinkholes in a Cup Activity Source: Adapted from Project Underground, A Natural Resource Education Guide Background Sinkholes are natural depressions in the land caused when limestone and soils dissolve. They form when groundwater removes rock underground. They can form by slow gradual sinking or by sudden collapse of an underlying hole. Sinkholes are common in about one quarter of the U.S. You can usually identify them as circular or oval low spots in fields that may gather standing water after rains. [Read More]

Soil Color and Redox Chemistry Activity Source: Soil Science Society of America. Adapted with permission. Are soils like M&Ms™? Yes! Typical soil colors are red, brown, yellow, or black. These colors are often not the color of the minerals in the soil but coatings of iron oxides (Fe203, FeOOH, and so on) or organic matter on particles. The minerals beneath are often quartz or feldspar, which are grey. To see how coating affects soil color, consider red M&Ms™. [Read More]

Soil Glue Activity Source: Soil Science Society of America Background The health of soils is crucial in reducing soil degradation and supporting the systems of the underground life cycle. In healthy soils, sand, silt and clay particles are held together by “soil glues”, or glomalin, a protein produced by fungi. Glomalin sticks to soil particles and holds them together, much like glue, to form stable aggregates (clods). This ability is called aggregate stability. [Read More]