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Education is no longer contained within classroom walls or the physical site of a school building. Learning isn’t confined to the eight hours between the school bells chimes or the struggling budget of an underfunded program. Today, education can be found anywhere, by teaming up with students in Kenya or Skyping with an author in Sweden or chatting with an astrophysicist on the International Space Station.
The ASK Programme supports schools, special schools and colleges in England to raise awareness of apprenticeships and technical qualifications. On May 19th at 15:30, ASK will be hosting an informative webinar for individuals with additional needs.
One of the many responsibilities of teaching is providing students with meaningful feedback. The goal is simple: to support their learning and help them improve. Whether written or verbal, feedback has the power to shape how students approach their education. The key is to provide feedback that encourages growth rather than discouraging effort. Here are a few strategies to make your feedback as an educator as effective as possible.
Weathering and Erosion: A Collaborative Process Weathering, the breakdown of rocks into smaller fragments, and erosion, the transportation of these fragments, work in tandem to shape the Earth's landscape. Physical weathering mechanisms, such as abrasion, frost wedging, and thermal stress, break rocks apart, while chemical weathering processes like oxidation, hydrolysis, and carbonation alter their composition.
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.
The Rock Cycle's Three Main Rock Types: The video explains the three major rock typesigneous (formed from cooling magma or lava), sedimentary (formed from weathered and compacted sediments), and metamorphic (formed from existing rocks under heat and pressure)and their interrelationships within the rock cycle. The processes involved in transforming one rock type into another are highlighted.
The Rock Cycle's Three Main Rock Types: The video explains the three major rock typesigneous (formed from cooling magma or lava), sedimentary (formed from weathered and compacted sediments), and metamorphic (formed from existing rocks under heat and pressure)and their interrelationships within the rock cycle. The processes involved in transforming one rock type into another are highlighted.
Renewable Resources: Renewable resources, such as solar, wind, hydroelectric, geothermal, and biomass energy, replenish at a rate comparable to or faster than their consumption. Air and water are also considered renewable, though they don't "regrow" in the same way as plants. Non-Renewable Resources: Non-renewable resources, including coal, oil, natural gas, nuclear fuel, and minerals like iron ore, are formed much slower than they are used.
Tectonic Plate Movement Mechanisms: At least four mechanisms explain tectonic plate movement: mantle convection (magma rising and sinking), ridge push (newly formed, less dense rock pushing older rock), and slab pull (denser plate sinking and pulling the rest). Slab suction, caused by convection currents in the mantle wedge, also contributes. Plate Boundaries: Tectonic plates interact in three ways: convergent boundaries (plates moving towards each other), divergent boundaries (plates moving a
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