PolarTREC has been an incredible experience for me, both professionally and personally. The expedition and experience have shifted the way I teach about science in the field and how I approach this with the students. It has also reiterated the fact that I am educating my students to think critically and ask testable questions. This experience
On 25 August, teacher Svea Anderson gave a presentation on the highlights from her PolarTREC expedition at the Arizona Sonora Desert Museum at their annual Teacher Appreciation Night.
Soil decomposers, such as some bacteria and fungi, obtain energy needed for life from dead and decomposing plant and animal remains, known as soil organic matter. Soil organic matter is important to local ecosystems because it affects soil structure, regulates soil moisture and temperature, and provides energy and nutrients to soil organisms. It is also important globally, because
Just as the increase in atmospheric CO2 is causing the global air temperture to rise, the container with the added CO2 will trap more heat inside and will show a higher internal temperature.
Overview
This activity/demonstration can be used directly following lessons on greenhouse gasses and their effects on warming the atmosphere by allowing shortwave UV energy
This one hour webinar is conducted by PolarTREC alumni Missy Holzer. She highlighted her work with the High Arctic Change expedition 2008 and bringing inquiry-based science into her classroom. This webinar is part of the C-ISE online professional development course.
This website is produced by the geological mapping programme GEOKART of the Norwegian Polar Institute. We want to provide information for geologists working or interested in the Norwegian polar areas, with emphasis on Svalbard (Spitsbergen).
We want to inform about: NPI's geological programmes, activities, services and products, logistic requirements and working conditions in polar areas, ongoing activities, and basic scientific
This geologic time calculator allows the user to manipulate the relativism of time to other markers. It builds from the classic analogy for illustrating the relative durations of parts of the geologic time scale is the yardstick.