This site uses cookies to improve your experience. To help us insure we adhere to various privacy regulations, please select your country/region of residence. If you do not select a country, we will assume you are from the United States. Select your Cookie Settings or view our Privacy Policy and Terms of Use.
Cookie Settings
Cookies and similar technologies are used on this website for proper function of the website, for tracking performance analytics and for marketing purposes. We and some of our third-party providers may use cookie data for various purposes. Please review the cookie settings below and choose your preference.
Used for the proper function of the website
Used for monitoring website traffic and interactions
Cookie Settings
Cookies and similar technologies are used on this website for proper function of the website, for tracking performance analytics and for marketing purposes. We and some of our third-party providers may use cookie data for various purposes. Please review the cookie settings below and choose your preference.
Strictly Necessary: Used for the proper function of the website
Performance/Analytics: Used for monitoring website traffic and interactions
Summary Soil Composition: Soil consists of 45% minerals, 25% water, 25% air, and 5% organic matter (decaying plants and animals). This composition is crucial for plant growth and overall soil health. Soil Profile and Horizons: The soil profile is a vertical section showing distinct layers called horizons (O, A, E, B, C, R). Each horizon has unique physical properties and composition, reflecting different stages of soil formation and organic matter decomposition.
Mineralization: This fossilization process occurs when an organism's remains are buried and replaced by minerals from groundwater, hardening into a rock-like structure; petrified wood serves as a prime example. Carbonization: Over time, compression of deceased organisms leaves behind a carbon film outlining the original organism's shape. Molds, Casts, and Trace Fossils: Molds are impressions left by organisms in sediment, which can later be filled to create a cast.
Speaker: Andrew Cohen, Founder & CEO of Brainscape
The instructor’s PPT slides are brilliant. You’ve splurged on the expensive interactive courseware. Student engagement is stellar. So… why are half of your students still forgetting everything they learned in just a matter of weeks? It's likely a matter of cognitive science! With so much material to "teach" these days, we often forget to incorporate key proven principles into our curricula — namely active recall, metacognition, spaced repetition, and interleaving practice.
From the Cool Cat Teacher Blog by Vicki Davis Follow @coolcatteacher on Twitter This week, there continues to be news about AI. ChatGPT and some other tools are giving themselves away to college students. Notebook LM has rolled out new features making it a more popular tool for studying finals than probably anything else (we talked about this last week as well.
We organize all of the trending information in your field so you don't have to. Join 28,000+ users and stay up to date on the latest articles your peers are reading.
You know about us, now we want to get to know you!
Let's personalize your content
Let's get even more personalized
We recognize your account from another site in our network, please click 'Send Email' below to continue with verifying your account and setting a password.
52 
Let's personalize your content