Today in integrated science, students finished up some quick investigations into friction and learned that friction is affected by mass and surface type, and that’s about it! Surface area and speed don’t affect friction. They also learned about friction types, including static friction (the friction when something isn’t moving yet) and kinetic friction, which is the friction of motion. Static friction was always greater than kinetic friction, and it builds up until an object starts moving, when it switches to kinetic friction. There are two types of kinetic friction as well! Rolling friction is almost always greater than sliding friction. Tomorrow we’ll be wrapping up some notes on Friction (Friction Notes) and taking our quiz on friction.
Science 8 students today measured the density of several objects in preparation for a learning activity. However, we first watched the first 11 minutes of a video on the Birth of the Earth and worked on the Birth of the Earth Video notes. This video outlined the early formation of our planet and the scientific evidence that supports this explanation. After watching the video, students learned that the earth’s layers formed because of melting, and the denser materials sank to the core. Applying this concept, students were asked to take the densities they had calculated and figure out what a new planet made of those materials would look like. Which material would make up the core? Which material would make up the crust? This information will be quizzed tomorrow as well.
HOMEWORK: Integrated= study for the friction quiz and week 10 retake quiz
Science 8=study your Earth’s model notes and any notes from today on density and/or the video.