Science begins with wonder. We use inquiry and experimentation to explain the world surrounding us; this process is science.
Strong Foundations Charter School uses the Core Knowledge scope and sequence. We begin the year with a general introduction to what is science. Topics include scientific method, hypothesis, thesis and an exploration of what science can and can't answer. Most of our major units of science have a project or writing component to synthesize scientific information.
My sixth grade science class needs shoe boxes and clay. We don't need the modeling clay that dries in shape, but the other modeling kind that stays moist and can be kept in a bag for a long time. I know that some families might have a bag with all different colors mixed together--please send it in if you no longer need it. THANKS!
Also, if you have a container of cream of tartar that is older and want to replace it with fresh stuff--send that in as well.
We begin our foray into the Core Knowledge scope and sequence with a unit on:
Gravity
• Gravity: an attractive force between objects
Newton’s law of universal gravitation: Between any two objects in the universe there is an attractive force, gravity, which grows greater as the objects move closer to each other.
How gravity keeps the planets in orbit
Following the Core Knowledge scope and sequence we will focus on:
Astronomy: Stars and Galaxies
• Stars
The sun is a star.
Kinds of stars (by size): giants, dwarfs, pulsars
Supernova; black holes
Apparent movement of stars caused by rotation of the earth Constellations: visual groupings of stars, for example, Big Dipper, Orion Astronomical distance measured in light years
• Galaxies
The Milky Way is our galaxy; the Andromeda Galaxy is closest to the Milky Way. Quasars are the most distant visible objects (because the brightest).
Plate Tectonics
• The surface of the earth
The surface of the earth is in constant movement.
The present features of earth come from its ongoing history. After the sun was formed,matter cooled creating the planets. The continents were once joined (Pangaea).
• Layered structure of the earth
Crust: surface layer of mainly basalt or granite, 5 to 25 miles thick Mantle: 1,800 miles thick, rock of intermediate density, moves very slowly Outer core: liquid iron and nickel
Inner core: solid iron and nickel, 800 miles thick, about 7,000 degrees C
• Crust movements
The surface of earth is made up of rigid plates that are in constant motion.
Plates move because molten rock rises and falls under the crust causing slowly flowing currents under the plates.
Plates move at speeds ranging from 1 to 4 inches (5-10 centimeters) per year. Earthquakes usually occur where stress has been built up by plates moving in opposite directions against each other. Earthquakes cause waves (vibrations) which have:
focus, the point below the surface where the quake begins
epicenter, the point on the surface above the focus
Severity of ground shaking is measured on the Richter scale
• Volcanoes usually occur where plates are pulling apart or coming together, but some occur at holes (hot spots) in the crust away from plate boundaries. As plates move over these hot spots, they cause chains of volcanoes and island chains like the Hawaiian Islands.
• Evidence for long-term movement of plates includes fit of continents and matches of rock types, fossils, and structures; ocean floor age and topography; ancient climate zones; locations of earthquakes, volcanoes, and mountain ranges; magnetic directions in ancient rocks.
Oceans
• Surface
The world ocean covers most of the earth’s surface (71 %).
Three major subdivisions of the world ocean: Atlantic, Pacific,and Indian Oceans Islands consist of high parts of submerged continents, volcanic peaks, coral atolls.
• Subsurface land features
Continental shelf, continental slope, continental rise, abyssal plains Mid-ocean ridges and trenches, plate tectonics, Mid-Atlantic Ridge, Mariana Trench
• Ocean bottom: average depth of sediment .3 mile, consists of rock particles and organic remains
• Composition of seawater: dilute solution of salts which come from weathering and erosion of continental rocks. Sodium chloride is the main salt.
• Currents, tides, and waves
Surface currents: large circular streams kept in motion by prevailing winds and rotation of the earth; Gulf Stream (North Atlantic), Kuroshio (North Pacific) Subsurface currents are caused by upwelling from prevailing offshore winds (Peru, Chile) and density differences (Antarctica); the upwelling pushes up nutrients from the ocean floor.
Tides are caused by gravitational forces of the sun and moon; there are two tides daily. Waves are caused by wind on the ocean’s surface.
Water molecules tend to move up and down in place and not move with the wave. Crest and trough, wave height and wavelength, shoreline friction
Tsunamis: destructive, fast-moving large waves caused mainly by earthquakes
• Marine life
Life zones are determined by the depth to which light can penetrate making photosynthesis possible, and by the availability of nutrients.
The bottom (benthic zone) extends from sunlit continental shelf to dark sparsely populated depths. Shallow lighted water extending over continental shelf contains 90% of marine species.
Pelagic zone: water in open oceans
Classification of marine life
Bottom-living (benthic) such as kelp and mollusks
Free-swimming (nekton) such as fish and whales
Small drifting plants and animals (plankton), which are the dominant life and food source of the ocean
The basis for most marine life is phytoplankton (plant-plankton), which carry on photosynthesis near surface; contrast zooplankton (animal plankton).
Most deepwater life depends on rain of organic matter from above.
The densest concentration of marine life is found in surface waters, such as those off Chile, where nutrient-rich water wells up to the bright surface.