1 Rocks and soil Introduction It is by no means necessary to be a geological expert to implement a worthwhile study of rocks and soil at primary school level. Rocks and soil are not difficult to collect, and are a very good vehicle for outdoor activities while at camp or on excursions, collecting and classifying, or making rocks in the classroom. Students can be fascinated by rocks and soil. A simple rock collection, showing a variety of shapes, sizes, colours and textures, is a good resource. Rocks and soil can be collected during trips to the country, at building sites around the city, or in the back garden. Mining and metals are very closely related to rocks and soils as a topic. We have included some interesting activities that could be covered under the topics of rocks, soil and mining. Key concepts of rocks and soil The activities in this topic are designed to explore the following key concepts: Early years Earth is covered with rocks, soil, water and ice. Rocks can vary in shape, texture and mass. Rocks can be a single colour or contain many colours. Some rocks contain fossils. Humans make rocks to help them live more easily. Rocks slowly change by wearing away. Crumbled rocks form part of soil. Some rocks are harder than others. Middle years Rock layers are located under soil, water and ice. Natural rocks are made in many different ways. Rocks that we find at a particular place may have been made elsewhere. Some natural rocks became solid very quickly, while others took a long time to become solid. Rocks are made of minerals. Deakin University 1
2 2 IDEAS FOR TEACHING SCIENCE: YEARS P 8 R O C K S A N D S O I L Deakin University Rocks can be made of one or more minerals. Minerals can form crystals. Crystals can have straight edges and flat slides. Some rocks act as magnets. Some rocks are conductors of electricity. Soils are produced, in part, from the weathering of rocks. Soil can be made up of organic (animal and plant) material, inorganic (grains of rock) components, and water. Eroded rock material can be deposited in layers to form sedimentary rocks, such as sandstone, limestone and mudstone. Igneous rocks, such as pumice and granite, are formed by magma from inside the Earth rising to the surface and cooling. Sedimentary and igneous rocks that are subject to heat and pressure form metamorphic rocks, such as marble, quartzite and slate. Minerals are constituents of rocks. Some minerals (e.g. gold and diamonds) are highly valued by humans. The ornamental use of rocks is determined by their colour, mineral content and markings. The varying hardness of rock is an important factor in its usage. Humans knowledge of rock formation helps them to find oil and precious stones (e.g. gold, opal, emeralds, etcetera). Students alternative conceptions of rocks and soil Research into students ideas about this topic has identified the following non-scientific ideas: Pebbles and stones are thought of as not rocks. All rocks are thought to be hard. Rocks stay the same for ever. Rocks must be heavy. Soil must have always been in its present form. Earth is molten, except for its crust. The rock cycle Earth s crust is not stationary as one may think; it is constantly moving. The dynamic nature of Earth s crust means that as new rock is formed at one location it deteriorates at other locations; this is the rock cycle. There is an enormous variety of rocks and their constituent minerals present in Earth s crust, but all rock varieties are classified as one of three basic types: igneous, sedimentary and metamorphic. These basic types of rock relate to the manner in which the rocks were formed. The mining of rocks and minerals from Earth s crust has provided humankind with many benefits, including building materials, fossil fuels (oil, coal and gas), and precious metals and minerals for cosmetic and industrial uses.
3 Deakin University IDEAS FOR TEACHING SCIENCE: YEARS P 8 ROCKS AND SOIL 3 A rock is an aggregate of minerals. Minerals are naturally occurring, inorganic, crystalline solids that have definite physical and chemical properties. There are two exceptions to this definition: these are naturally occurring glass, called obsidian, and sedimentary rock coal. More than 3500 minerals have been identified and described but only about a dozen make up the bulk of the rocks in Earth s crust. All rocks in Earth s crust, with the exception of meteorites, were formed from magma (molten rock material) pushed up from the mantle (interior layer of Earth). While the original rock material comes from the mantle, geologists (scientists who study rocks) distinguish three distinct processes of rock formation: every rock is then generally classified according to its mode of formation. The three major groups of rocks are igneous, sedimentary and metamorphic. The interrelationships between Earth s internal and exterior processes of rock formation and disintegration are described by the rock cycle. The rock cycle is shown in the figure below. The rock cycle: relates the three rock types to each other shows surface processes such as weathering, transportation and deposition shows internal processes such as magma generation and metamorphism. FIGURE: THE ROCK CYCLE Movements in Earth s crust are the mechanisms responsible for recycling rock materials; they therefore drive the rock cycle.
4 4 IDEAS FOR TEACHING SCIENCE: YEARS P 8 R O C K S A N D S O I L Deakin University Igneous rocks Igneous rocks are formed through the crystallisation of magma as it cools either in the mantle or on the surface after a volcanic eruption. The components of rock are minerals and each mineral forms, or crystallises, under a certain temperature and pressure. The variation in pressures and temperatures is great when one extends from the mantle to the surface, so it is not surprising that a huge variety of minerals exist. Crystallisation is the process by which the mineral particles form tight bonds in a well-defined three-dimensional shape. CRYSTAL SHAPES Look at the crystal shapes of sugar and salt under a magnifying glass. The size of the crystal is determined by the time that it takes to cool. If cooled slowly, the crystal shapes are large. As magma cools, minerals crystallise, and the resulting rock is characterised by interlocking mineral crystalline grains. Magma that cools beneath Earth s surface produces intrusive igneous rocks (also called plutonic rocks), while magma that cools at Earth s surface produces extrusive igneous rocks (also called volcanic rocks) (refer to Figure 1). Igneous rocks that cool slowly have a coarse-grained texture characterised by large mineral crystals, whereas rocks that cool quickly are fine grained and have small mineral crystals. Generally, intrusive rocks are coarse grained, whereas extrusive rocks are fine grained. Common volcanic rocks include tuff, rhyolite, andesite and basalt. Common plutonic rocks include granite, diorite and gabbro. Weathering, erosion and deposition Weathering is the physical breakdown (disintegration) and/or chemical alteration (decomposition) of rocks on Earth s surface. These changes are caused by the weather by air and water. There are two types of weathering: mechanical and chemical; usually taking place at the same time. Mechanical weathering is the breaking up of rocks and mineral into smaller pieces. This can occur in various ways: trees and other plants send down roots into cracks in rocks, wedging them apart water and wind erode the surface of rocks temperature changes in the environment expand and contract rock to create cracks liquid water gets into cracks and as it freezes it expands, and wedges apart rocks (water expands about nine per cent when it freezes) animals burrow and help break up the rock. Chemical weathering includes all the chemical changes that take place when air and water attack the rocks. Chemicals in the water break down the rocks. As mechanical weathering breaks apart the rocks, there is more surface area on the rocks for chemical weathering to occur. Weathering yields the raw materials for both soils and sedimentary rocks. The small particles of rock are called sediment, which is generally transported to
5 Deakin University IDEAS FOR TEACHING SCIENCE: YEARS P 8 ROCKS AND SOIL 5 another site where it accumulates. The method of transportation varies. Glaciers can move any sized particle, whereas wind transports only sand-sized and smaller sediment. Waves and marine currents also transport sediments, but by far the most common method of transportation is by running water (rivers and streams). Any geographical area in which sediment is deposited is a depositional environment. Soils are sediments that combine with humus. Humus gives many soils their dark colour and is derived from bacterial decay of organic matter. Sedimentary rocks Following the weathering of rocks, the sediment formed is transported and deposited at a depositional environment. These deposits may become compacted and/or cemented and thereby converted into sedimentary rock. The process by which sediment is transformed into rock is called lithification. About ninety-five per cent of Earth s crust is composed of igneous and metamorphic rocks, but sedimentary rocks are most common at or near the surface. Approximately seventy-five per cent of the surfaces exposed on continents consist of sediments or sedimentary rocks. Sedimentary rocks are generally classified as detrital or chemical. Detrital sedimentary rocks consist of solid particles of pre-existing rocks. The fragments might be tiny or large. The following table gives the name of the original sediment, the lithification process and the rock type produced. TABLE: SEDIMENT TO ROCK Sediment Gravel (greater than 2 mm) Lithification process Compaction/ cementation Rock Conglomerate (rounded particles) Breccia (angled particles) Sand (2 mm to 0.06 mm) Compaction/ cementation Sandstone Silt (0.06 mm to mm) Compaction/ cementation Siltstone Clay (less than mm) Compaction Shale Chemical sedimentary rocks originate from the weathering process where rock material is dissolved into water and transported to lakes and oceans. Here chemical processes take place that result in the accumulation of minerals. Organic material may also be involved in the chemical processes. The rocks produced are called biochemical sedimentary rocks. For example, coal is composed of the compressed, altered remains of organisms, mainly plants. Another example is a type of limestone called coquina that consists entirely of broken seashells cemented by calcium carbonate. Areas on Earth s surface where sedimentary rock is found are characterised by distinctive layers and the presence of fossils. Rivers transport sediment from
6 6 IDEAS FOR TEACHING SCIENCE: YEARS P 8 R O C K S A N D S O I L Deakin University one location to another deposit in layers. Over many years different layers build up. Sometimes dead animals and plants get immersed into the sediment layers. Therefore, following lithification, the sedimentary rock produced is in layers that quite often contain the remains of ancient organisms, called fossils. Metamorphic rocks Metamorphic rocks result from the transformation of other rocks by metamorphic processes that occur below Earth s surface. Through heat and pressure, igneous and sedimentary rocks are transformed into metamorphic rocks. In the metamorphic process the change in the rock may be minor and the features of the parent rock are still recognisable. The change may also be major and result in the formation of new minerals and/or a change in texture of the rock. In this situation any features of the parent rock may be unrecognisable. Activities CLASSIFICATION Properties of rocks Key idea: Natural rocks have a range of properties and appearances. a collection of rock samples. This activity is best done in pairs or small groups. Choose one of the rock samples supplied and write a description of it. Your partner should do the same. Then exchange descriptions and see if you can each identify the sample the other one described. Group a number of rock samples according to one characteristic and see if your partner can identify the characteristics used. One member of the group chooses a rock sample from a group of rock samples. The other members then ask questions which enable them to identify the sample chosen. The person who has chosen the sample should only answer yes or no to the questions. How many questions are required to find the sample chosen? TESTING ROCKS Key idea: Natural rocks have a range of properties and appearances. a collection of rock samples measuring scales sketching paper and a pencil a hammer a magnifying glass a copper coin a pin a penknife a drop of vinegar
7 Deakin University IDEAS FOR TEACHING SCIENCE: YEARS P 8 ROCKS AND SOIL 7 some water a piece of metal a bathroom tile. This activity is best done individually. Choose a rock from the collection and try the following tests on it: Is your rock light or heavy? Estimate its weight, then check your answer. Sketch your rock. Describe your rock. Is it single or multi-coloured, bright or dull? Has it got layers? Does it look like it has small rocks stuck together? Rub the rock with your finger. Does any rub off? Hammer off a portion. Can you crush it? Look at the particles with your eye or a hand-lens. Are the particles fine or coarse? Are the particles single or multi-coloured? What is the colour of the inside remaining rock? Try a hardness test with a fingernail, copper coin, pin, and penknife. Are there layers to be seen? Does a drop of vinegar (acid) cause bubbles? If so, the rock contains lime. Does it absorb water? Easily? Knock a piece of metal against your rock. What sort of sound is produced? High pitch, low pitch or metallic? What is the colour of its streak on the back of a bathroom tile? Explanatory note: The following tables, when read from left to right, represent rock-type identification keys. The first table gives a clue to the rock type in general, whereas the following tables provide extra information to determine the name of the rock.
8 8 IDEAS FOR TEACHING SCIENCE: YEARS P 8 R O C K S A N D S O I L Deakin University TABLE: WHAT ROCK TYPE IS IT? Grains visible to the naked eye Interlocking grains Grains do not interlock Rock types No alignment of grains Some grains aligned Bubbles with acid Separate grains held together by finer material Igneous Metamorphic Metamorphic Sedimentary Texture Grains not obvious Can be scratched with a knife Cannot be scratched with a knife Sedimentary Bubbles with acid may have fossils Fossils present no acid reaction Can be split into thin rock sheets Cannot be split into thin rock sheets Sedimentary Sedimentary Sedimentary Metamorphic Igneous TABLE: WHAT IS THE NAME OF THIS IGNEOUS ROCK? Igneous rocks key Light Large crystals/speckled Granite coloured Small crystals/layered Rhyolite Texture Visible crystals Dark coloured Large crystals Small crystals Black Green Black/grey Grabbo Peridotite Basalt No visible crystals Black/glassy White/porous (floats on water) Red/black porous Obsidian Pumice Scoria Rock and mineral fragments Layered Tuff
9 Deakin University IDEAS FOR TEACHING SCIENCE: YEARS P 8 ROCKS AND SOIL 9 TABLE: WHAT IS THE NAME OF THIS SEDIMENTARY ROCK? Visible fragments Sedimentary rocks key Rock and mineral fragments Angular Over fragments 2 mm size Round fragments Sand-size 0.6 mm to 2 mm Breccia Conglomerate Sandstone Texture Plant and animal fragments Plant fragments Animal fragments Black or brown Shell or Coral Coal Limestone Reacts with acid Limestone No visible particles. Very fine No reaction with acid Breaks into layers Uniform structure, not layered Shale Siltstone Mudstone TABLE: WHAT IS THE NAME OF THIS METAMORPHIC ROCK? Appearance Shows layers, smooth parallel surfaces No layers, no smooth parallel rock surfaces Metamorphic rocks key Texture very fine. Grains not visible to naked eye Texture coarser. Grains visible to naked eye Not scratched with knife Dark, dull surfaces Light, shiny surfaces Mica grains and layers visible Banded appearance Reacts with acid Slate Phyllite Schist Gneiss Marble Dark in colour Homfels Light in colour or quartz grains visible Scratched with knife. Reacts with acid Quartzite Marble
10 10 IDEAS FOR TEACHING SCIENCE: YEARS P 8 R O C K S A N D S O I L Deakin University BREAKING UP ROCKS Key idea: Sedimentary rocks are made through crushing soil or sediment. a collection of rocks including sandstone, mudstone, limestone and granite some samples of soil types a hammer. Crush some sandstone, some mudstone and some limestone. Examine the materials formed. In what ways are they similar? In what ways are they different? Compare your crushed samples with soil. In what ways are they different? Examine a small piece of coarse-grained granite. How many different minerals are present? Estimate the relative amounts of the three main components. Crush the granite with a hammer to pieces about rice-grain size, and separate into the different mineral components (quartz, feldspar and a little mica). How close was your initial estimate? Explanatory note: The sedimentary rocks, when broken up, reverse the process by which they were formed. Sandstone and mudstone were originally small rock particles that were crushed, whereas the limestone was tiny rock particles that underwent chemical processes in addition to being crushed. The coarsegrained granite was formed by slowly cooling magma to form an igneous rock. ROCKS THAT FLOAT Key idea: Some rocks are light and may float. samples of pumice, en-tout-cas, basalt, coal, coke, toffee and honeycomb a bowl of water. Examine a piece of pumice (pumice is aerated rock foam that has been rapidly cooled). Try floating it in water. Can you find other rocks with air bubbles? Do particles of en-tout-cas (from a tennis court) float? Describe the common difference between toffee/honeycomb, coal/coke and basalt/pumice. Explanatory note: These types of igneous rocks were formed by volcanic eruptions that have cooled very quickly in the air. In cooling, bubbles of air were trapped. SOIL FACTORY Rock and soil formation Key ideas: Crumbled rocks form part of soil. Weathering of rocks creates soil. soil from different parts of the garden water in a container with a lid
11 Deakin University IDEAS FOR TEACHING SCIENCE: YEARS P 8 ROCKS AND SOIL 11 crushed sedimentary rock compost a bottle to mix the water and soil in. Mix the soil with plenty of water, shake and let settle. Note the sand/silt/clay/humus composition. Which particles settle out first? Can you make some soil to match, using crushed sedimentary rock and compost? SEDIMENTS IN LAKE AND RIVER WATER Teaching note: This activity, and Breaking up rocks and Soil factory, gives the students insight into the processes by which sedimentary rocks are formed. Key idea: Sedimentary rocks are formed from crushing existing rock particles. a bottle of water collected from a nearby lake or river a magnifying glass or microscope. Ideally, water should be collected from moving water near the shore of the lake or from the current in the river. Don t stir up the bottom sediment when collecting the samples. Let the sample of water stand. How long does it take for the sediment to settle and the water to clear? Is there any scum or pollution collected on top of the water? If possible collect water from a stream after it has rained and collect water when there has been a dry spell. Which samples had more sediment? Why? Pour off most of the water, and let the rest evaporate. Study the sediment under a magnifying glass or microscope. What do you see? ROCK FACTORY Teaching note: The classification keys outlined in the Testing rocks activity provide a means of classifying rocks. Determine whether the artificial rocks match the descriptions in these classification keys. Key idea: Rocks are made in different ways, both by nature and by humans. a collection of sedimentary, metamorphic and igneous rocks water plastic crushed sandstone clay sand cement. Survey the classroom, the building and the grounds for a list of material manufactured by humans from mineral/metal origins and now used in construction. Include the gardens, nature strip and road in your list. Classify the artificial rocks as sedimentary, metamorphic, conglomerate, etcetera.
12 12 IDEAS FOR TEACHING SCIENCE: YEARS P 8 R O C K S A N D S O I L Deakin University Make a sedimentary rock, using crushed sandstone and water. Investigate what works as binding (plaster? clay?). Make some concrete blocks (conglomerate) using screenings, and different proportions of sand and cement (e.g. 1:2, 2:1, 3:1). Devise a test to determine the strongest concrete. Compare your samples with samples of commercial concrete. Make bricks using clay (metamorphic). Try adding various materials which could affect the strength, for example, straw. FOSSILS Key idea: Some rocks contain fossils. limestone rocks a hammer a leaf a petri dish petroleum jelly plaster of Paris. Break up some limestone with a hammer. You should be able to find some fossils to investigate. Make a fossil using the following steps: choose a leaf or flat object grease it and a petri dish with petroleum jelly cover with plaster of Paris and allow to set. MANIPULATING MUD SCIENTIFICALLY Key idea: There are different types of soil. samples of different soils a teaspoon water. Place a teaspoon of soil in the palm of your hand. Add water drop by drop until it is thoroughly wet but there is no excess water on your hand. Record what happens when you try to: use your finger to press the soil flat on your palm roll it into a long thin worm mould it into a tiny bowl make it into a cube. Explanatory note: Soil scientists operating in field locations describe soils as sands, loams or clays according to whether they fall apart (sand), hold together in blocks but do not roll into a thin worm (loam), or roll out well to a thin worm (clay), when moistened and then manipulated as you have done.
13 Deakin University IDEAS FOR TEACHING SCIENCE: YEARS P 8 ROCKS AND SOIL 13 CONCEPT MAP Key idea: Rocks are formed through different processes. poster paper a list of ideas related to rocks and soil. Construct a concept map on poster paper to link the following ideas: mineral soil stone bedrock bricks water volcano crystal sand sedimentary rock concrete metamorphic rock granite igneous rock erosion quartz layering. FEELY BOX Properties of rocks, metals and mining Key idea: Metals are minerals that make up rocks. a feely box that contains various metals (iron, lead, zinc, brass and aluminium), wood and other non-metallic objects. Feel the objects in the feely box. Which are metal? What properties are you using to decide? Using the objects in the feely box, distinguish between wood, lead, zinc, brass and aluminium. All but one of the metal objects in the feely box are made of the same metal. Which is the odd one out? TESTING FOR ELECTRICAL CONDUCTION Key idea: Metals are good electrical conductors. a battery a light bulb
14 14 IDEAS FOR TEACHING SCIENCE: YEARS P 8 R O C K S A N D S O I L Deakin University connecting wires rods made of different metallic and non-metallic materials. Use the battery, bulb and connecting wires to check how well the rods provided conduct electric current. That is, the brighter the bulb, the better the conductor. What appliances around the home make use of the conduction of metals? HOW HARD IS IT? Key idea: Metals have different hardnesses. a collection of different metal surfaces a ball bearing. Compare the hardness of various metals by dropping a ball bearing onto the surface and measuring the height of bounce. The balls will bounce higher from harder surfaces. CONDUCTION OF HEAT Teaching note: A simple test of electrical conductivity can decide whether an object is metallic. Key idea: Metals are good conductors of heat. a candle a metal rod. Use the candle to place drops of wax along the length of a metal rod. Now place the rod horizontally. Light the candle and heat up one end of the metal rod take a note of the time it takes each drop of wax along the length of the rod to melt. Does the heat travel at a steady speed along the length of the rod? Do all metals conduct heat equally well? In how many ways can you prevent a drop of wax melting at one end of an aluminium rod when the other end is heated? Can you think of ways in which the property of heat conduction is useful? WHAT IS IT MADE FROM? Key idea: Metals have a range of properties. a collection of objects that are metallic or have some metallic components (a variety of metals). For each object, determine whether it is metallic, or contains some metallic components. What criteria are you using in your determination? Are you able to name the type of metal found?
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5-Minute Refresher: WEATHERING AND EROSION Weathering and Erosion Key Ideas Weathering is the wearing away of the surface of rock, soil, and minerals into smaller pieces. Example of weathering: Wind and
ROCKS, FOSSILS AND SOILS SECTION 8: FOSSILS From Hands on Science by Linda Poore, 2003 STANDARDS: Westminster College Students will write or draw descriptions of a sequence of steps, events and observations,
Magnetism Introduction This topic explores the key concepts of magnetism as they relate to: the phenomenon of magnetism magnetic forces and fields a theory of magnetism. Key concepts of magnetism The activities
Ocean Floor Continental Shelf Begins at the shoreline Gently slopes underwater Average depth of 430 feet Thick layers of sand, mud, and rocks The beach is part of the Continental Shelf Ocean Floor Continental
reflect Everything around us is made out of tiny bits of matter. These particles may combine in different ways to produce new materials. Sometimes we need to separate the parts of a material. If we know
Part Two Our Ever Changing Earth Grade Level: 1 *Part Two is actually a unit plan and contains more than one lesson. You can pick and choose those that best fit your goals and the ability level of your
Reference: CLASSIFICATION // CHARACTERIZATION OF SOME ROCK FEATURES Engineering characteristics of main rock material: - Geological name, (type of rock) - Orientation of foliation/bedding/layering - Anisotropy,
Investigation 1-Part 1: Investigating Mock Rocks Geology: the scientific study of Earth s history and structure Geologist: a person who studies the Earth and the materials of which it is made Property:
Igneous Rocks Geology 200 Geology for Environmental Scientists Magma Compositions Ultramafic - composition of mantle Mafic - composition of basalt, e.g. oceanic crust. 900-1200 o C, 50% SiO 2 Intermediate
Geologic Site of the Month February, 2002 The Geology of the Marginal Way, Ogunquit, Maine 43 14 23.88 N, 70 35 18.36 W Text by Arthur M. Hussey II, Bowdoin College and Robert G. Marvinney,, Department
CHAPTER 3 2 Wind Erosion and Deposition SECTION Agents of Erosion and Deposition BEFORE YOU READ After you read this section, you should be able to answer these questions: How can wind erosion shape the
: Finding Clues Like a Scientist Author: Kris Poduska Date Created: 2000 Subject: Earth Science, Classification Level: Elementary and Middle School Standards: New York State- Intermediate Science (www.emsc.nysed.gov/ciai/)
GEOL 104 Dinosaurs: A Natural History Geology Assignment DUE: Mon. Sept. 18 Part I: Environments of Deposition Geologists can use various clues in sedimentary rocks to interpret their environment of deposition:
Volcano in the lab: a wax volcano in action: teacher s notes Level This activity is designed for students aged 11-14, as a simple demonstration of igneous activity. English National Curriculum reference
SEDIMENTARY ROCKS INTRODUCTION Weathering, erosion and deposition The start of sedimentary rocks is the weathering process of the rock cycle as surface materials are weathered they decay to particles and
Lab Activity on Minerals 2002 Ann Bykerk-Kauffman, Dept. of Geological and Environmental Sciences, California State University, Chico * Introduction Rocks are made of many mineral grains stuck together.
IF YOU BIT A ROCK Teacher Page This activity has been modified from a lesson plan for meteorite education from NASA. It has been refitted for more common rocks. The web site for the original lesson plan,
Layers of the Earth s Interior 1 Focus Question How is the Earth like an ogre? 2 Objectives Explain how geologists have learned about the interior of the Earth. Describe the layers of the Earth s interior.
2 MATTER Matter is the material of which the universe is composed. It has two characteristics: It has mass; and It occupies space (i.e., it has a volume). Matter can be found in three generic states: Solid;
Target Grade or Age Level Sixth grade science Lesson 5: The Rock Cycle: Making the Connection Scientific Processes Addressed Defining operationally, formulating and testing hypotheses, constructing models
KINDERGARTEN WATER 1 WEEK LESSON PLANS AND ACTIVITIES WATER CYCLE OVERVIEW OF KINDERGARTEN WEEK 1. PRE: Defining the states of matter. LAB: Discovering the properties of water. POST: Analyzing the water
1. Michigan Geological History Presentation (Michigan Natural Resources) The Michigan Geological History Presentation provides an overview of the approximately 3 billion years of Earth Processes that the
Young naturalists ASK A ROCK Would you like to hear a good story? Ask a rock. Big or small, sharp or round, each rock you see has a tale to tell about how the land around it has been shaped for millions
Cambridge International Examinations Cambridge Secondary 1 Checkpoint SCIENCE 1113/01 Paper 1 For Examination from 2014 SPECIMEN PAPER Candidates answer on the Question Paper. Additional Materials: Pen
Objectives You will learn about how the land of North Dakota was formed. Introduction North Dakota is a wonderful place to live. Have you ever though about how it was formed? To answer that question, you
KINDERGARTEN PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF KINDERGARTEN VOLCANOES WEEK 1. PRE: Learning that all mountains are not volcanoes. LAB: Investigating rocks
Chapter 2 Igneous Rocks Most students find the definition of a mineral to be rather long and cumbersome. In contrast, the definition of a rock is short and sweet. A rock is any naturally occurring aggregate
SEE HOW TO MAKE LIME PLASTER PATTI STOUTER, BUILD SIMPLE INC. FEBRUARY 2013 WHY USE LIME? Lime plaster forms a light, clean, and durable surface that is resistant to weather and mold. A thin layer attaches