Painting With Soil Activity Source: Soil Science Society of America, Adapted with permission Soils are one of our most important natural resources — just think of where all the food you eat comes from. They also are important for the beauty the many soil colors add to our landscapes. Most of us overlook this natural beauty because we see it every day. Often these colors blend with vegetation, sky, water, etc. [Read More]

Particle Size and Oil Production Activity Source: Adapted by AAPG from EarthComm and the American Geosciences Institute. Adapted with permission. What factors affect how easily a fluid can move through sediments? How is this flow rate connected to oil production? Many people think that oil lies in big pools below Earth’s surface. Oil actually is located in the pores within rocks (called “source rocks”). When the pores are connected, oil can flow slowly through the rock. [Read More]

Rain and Soil Activity Source: Adapted with permission by Soil Science Society of America. When it rains, much of the water drains directly into the ground. But why? Soil is made up of four main components: minerals, organic matter, water, and air. Ideal percentages of each is shown in the figure, but in reality the percentages vary from location to location. Water moves through open spaces in soil known as “pores. [Read More]

Reclaiming a Mine Site Activity Source: Adapted with permission by Minerals Education Coalition. Mined land is reclaimed for future use. The objective of this activity is to investigate how plants will grow on a reclaimed landscape. Over a period of days, you will learn how overburden is incorporated into the landscape after it has been removed during the mining process.Before beginning, discuss vocabulary terms: overburden, stockpile, grading, soil types, seeding, stability, seed germination, nutrients, closure planning, and reclamation. [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]

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]

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 Moisture Activity Source: Soil Science Society of America Soil moisture is the water stored in the soil and is affected by precipitation, temperature, soil characteristics, and more. These same factors help determine the type of biome present, and the suitability of land for growing crops. The health of our crops relies upon an adequate supply of moisture and soil nutrients, among other things. As moisture availability declines, the normal function and growth of plants are disrupted, and crop yields are reduced. [Read More]

Soil Properties Activity Source: Adapted with permission from Kristen Lucke, Views of the National Parks, National Park Service. “Soil porosity” refers to the amount of pores, or open space, between soil particles. Pore spaces may be formed due to the movement of roots, worms, and insects; expanding gases trapped within these spaces by groundwater; and/or the dissolution of the soil parent material. Soil texture can also affect soil porosity There are three main soil textures: sand, silt, and clay. [Read More]

Soil, the Forgotten Resource Activity Source: Adapted with permission by Ward’s Natural Science. Soil is often overlooked as a natural resource. Like fossil fuels, we depend on it for energy in the form of foods. And, like fossil fuels, it is nonrenewable. Soil is a delicate balance of inorganic minerals, organic matter, living organisms, soil water, and soil atmosphere. The natural development of soil is an exceedingly slow process. In a few hours, a heavy rain falling on exposed soil can remove inches of what took hundreds of years to form. [Read More]