Geology Qur an English Arabic Math
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1 ١ Correlated to State Standards Hands on activities and crafts Fun geology projects Word for Word meanings of the Qur an Writing practice ٢ Cut out Arabic Cards Ages 6 & up! Geology Qur an English Arabic Math
2 Editors Note Asalamu alaykum! We are so pleased to share with you the first book in our series of curriculum based workbooks for Muslim students. This workbook is jam-packed with curriculum based activities, and exercises that reinforce what students are learning. Each workbook features writing practice to assist students in improving their penmanship, grammar, and sentences, as well as mathematics, and much more! Insha allah, each workbook will cover each subject in depth, and give students hands on projects and activities to encourage their love of learning so that it will blossom. Ma salama! Tarbiyah Publishing Team Copyright 2011, Tarbiyah Publishing All Rights Reserved Designed for Muslim families and Islamic Centers to increase early childhood literacy as well as increase the knowledge of Islam for all children and young adults.
3 quran reading log Juz 1 Al Fatiha 1 Al Baqarah 141 (1:1-2:141) Juz 2 Al Baqarah Al Baqarah 252 (2:142-2:252) Juz 3 Al Baqarah Al Imran 92 (2:253-3:92) Juz 4 Al Imran 93 - An Nisaa 23 (3:93-4:23) Juz 5 An Nisaa 24 - An Nisaa 147 (4:24-4:147) Juz 6 An Nisaa Al Ma idah 81 (4:148-5:81) Juz 7 Al Ma idah 82 - Al An am 110 (5:82-6:110) Juz 8 Al An am Al A raf 87 (6:111-7:87) Juz 9 Al A raf 88 - Al Anfal 40 (7:88-8:40) Juz 10 Al Anfal 41 - At Tauba 92 (8:41-9:92) facebook.com/islamichomeschooling Favorite words from the Qur an: Juz 11 At Tauba 93 - Hud 5 (9:93-11:5) Juz 12 Hud 6 - Yusuf 52 (11:6-12:52) Juz 13 Yusuf 53 Ibrahim 52 (12:53-14:52) Juz 14 Al Hijr 1 An Nahl 128 (15:1-16:128) Juz 15 Al Isra (or Bani Isra il) 1 - Al Kahf 74 (17:1-18:74) Juz 16 Al Kahf 75 Ta Ha 135 (18:75-20:135) Juz 17 Al Anbiyaa 1 - Al Hajj 78 (21:1-22:78) Juz 18 Al Muminum 1 - Al Furqan 20 (23:1-25:20) Juz 19 Al Furqan 21 - An Naml 55 (25:21-27:55) Juz 20 An Naml 56 - Al Ankabut 45 (27:56-29:45) Juz 21 Al Ankabut 46 - Al Azhab 30 (29:46-33:30) Juz 22 Al Azhab 31 - Ya Sin 27 (33:31-36:27) Juz 23 Ya Sin 28 - Az Zumar 31 (36:28-39:31) Juz 24 Az Zumar 32 - Fussilat 46 (39:32-41:46) Juz 25 Fussilat 47 - Al Jathiya 37 (41:47-45:37) Juz 26 Al Ahqaf 1 - Az Zariyat 30 (46:1-51:30) Juz 27 Az Zariyat 31 - Al Hadid 29 (51:31-57:29) Juz 28 Al Mujadila 1 At Tahrim 12 (58:1-66:12) Juz 29 Al Mulk 1 - Al Mursalat 50 (67:1-77:50) Juz 30 An Nabaa 1 - An Nas 6 (78:1-114:6)
4 Content Standards Geology English Mathematics Islamic Studies Standard Materials and Processes That Shape A Planet Grade 5 A.3 Explain how rock is formed from combinations of different minerals and how smaller rocks come from the breakage and weathering of bedrock (solid rock underlying soil components) and larger rocks; soil is made partly from weathered rock, partly from plant remains-and also contains many living organisms. Standard Comprehension of Informational Text Grade 2 1. Develop comprehension skills by reading a variety of selfselected and assigned informational texts Standard Writing Grade 2 4.b Acquire and use new vocabulary Standard 6.0 Knowledge of Number Relationships and Computation/Arithmetic Grade 2 C.1.a. Demonstrate proficiency with addition and subtraction basic facts using a variety of strategies. Quran 1. The Qur an on mountains. Hafiz 2. Surah Al Fatihah A.3.a. Observe and classify a collection of minerals based on their physical properties. Color Luster Hardness Streak A.3.b. Identify and compare the properties of rocks that are composed of a single mineral with those of other rocks made of several minerals using their physical properties. A.3.c. Describe ways that the following processes contribute to changes always occurring to the Earth's surface. Weathering Erosion Deposition Standard 2.0 Grade 6 A.4 Differentiate among sedimentary, igneous, and metamorphic rocks based upon the processes by which they are formed.
5 سورة الفاتحة م حي ر ٱل ن حم ر ب س م الله ٱل ن ٱل ع ال م ي ب ر ال ح م د هلل م حي ر ٱل ن حم ر ٱل ن دي ٱل م ال ك ي و م إ ي اك ن ع ب د و إ ي اك ن س ت ع ي ن م ٱل م س ت قي ط را ص ٱل ٱه د ن ا ط را ص ٱ ل ذ ين أ ن ع م ت ع ل ي ه م غ ري ٱل م غ ض وب ع ل ي ه م و لا ن ضا ل ي ٱل 6 6 intervals 4-5 intervals 2,4,6 intervals 2 intervals 2 With nose Silent Roll the R 2,4,6 intervals (ghu nnah)
6 Name: Date: Practice Writing ب س م الله ٱل ر حم ن ٱل ر حي م! ال ح م د هلل ر ب ن ٱل ع ال م ي ٱل ر حم ن ٱل ر حي م م ال ك ي و م دي ن ٱل 6 intervals 4-5 intervals 2,4,6 intervals 2 intervals 2 With nose Silent Roll the R 2,4,6 intervals (ghu nnah)
7 Name: Date: إ ي اك ن ع ب د و إ ي اك ن س ت ع ي ن م ٱل م س ت قي ط را ص ٱل ٱ ه د ن ا ٱ ل ذ ي ن ط را ص أ ن ع م ت ع ل ي ه م غ ري ٱ ل م غ ض و ب ع ل ي ه م و لا ٱل ضا ل ي ن
8 Vocabulary Vocabulary Cards Materials: vocabulary cards 3x5 cards glue scissors metal rings (the kind that snap open easily) 1. Cut the 3x5 cards in half. You should have a 2.5 x 3 card. 2. Cut out each of the vocabulary cards, and glue them onto the 2.5 x 3 cards. 3. Hole punch the top left hand corner of each card, and use the metal rings to keep them together.
9 ب س م ن حم ر ٱل الله! ال ح م د م حي ر ٱل هلل ر ب م ال ك ن ٱل ع ال م ي إ ي اك ن دي ٱل ي و م
10 Back of the cards. Glue to the 3x5 cards. Use the rest of the blank cards to create your own vocabulary cards.
11 إ ي اك ن ع ب د و إ ي اك ط را ص ٱل ٱه د ن ا ن ن س ت ع ي ٱل ذ ي ن م ٱل م س ت قي أ ن ع م ت ع ل ي ه م غ ري ٱل م غ ض و ب
12 Back of the cards. Glue to the 3x5 cards. Use the rest of the blank cards to create your own vocabulary cards.
13 ن ضا ل ي ٱل و لا
14 Back of the cards. Glue to the 3x5 cards. Use the rest of the blank cards to create your own vocabulary cards.
15 Title: The Creation of Mountains و ت ر ى ال ج ب ال ت ح س ب ھ ا ج ام د ة و ھ ي ت م ر م ر ال سح اب ص ن ع الله ال ذ ي أ ت ق ن ك ل ش ي ء إ ن ه خ ب ير ب م ا ت ف ع ل ون
16 Title: Igneous Rocks By: Because igneous rocks have formed from molten magma or lava, they are composed of randomly
17 arranged intergrown crystals. Rapid cooling can make crystals too small to be visible. IGNEOUS LITHOLOGIC PATTERNS
18 Title: Igneous Rocks By: Igneous rocks are very hard and dense, layering is rare. Gas bubbles (vesicles) sometimes give rocks a
19 frothy texture. You can identify igneous rocks by random ingrown crystals, glassy textures, or if it has vesicles.
20 1 The Rock Cycle / 111 % accuracy WCPM What is the rock cycle? What does igneous mean? Rocks are constantly being formed, worn down, and then formed again. This process, known as the Rock Cycle, can take thousands and millions of years for rocks to change. Rocks can be divided into three types, and are classified based on the way they form. The first type are called igneous. Igneous means fire or heat, and come from volcanoes. When volcanoes erupt and liquid rock comes up to the earths surface, then new igneous rocks are made. Igneous rocks that form outside of the volcano and cool quickly are called extrusive igneous rocks. Igneous rocks that form inside of the earths crust, and cool slowly, are called intrusive igneous rocks. 1 minute timed reading ~ Score the number of words read aloud correctly in one minute.
21 WEBSITE GEM:
22 " # $ " & Step 1: Determine the texture Phaneritic Texture Phaneritic (phaner = visible)! Aphanitic Texture Aphanitic (a = not, phaner = visible)! % Porphyritic Texture!!
23 " % " % Step 1: Determine the texture (page 2) Glassy Texture % "! Vesicular Texture % % % Pyroclastic Texture % %
24 The more time the rock is spent in the heat, the more time available for larger crystals to form.
25 Igneous Rock ID Green to black Black/dark grey Grey to salt & pepper White, pink red Color Light Medium Dark Very Dark Chemical Composition " # "! Pyroxene Olivine/Pyroxene Amphibole Quarts Dominant Minerals Olivine Plagioclase Feldspar Plagioclase Feldspar Potassium Feldspar
26 What are minerals? Minerals % % # one or more elements % % % % % % % $ % % Step 1: Colors Step 2: Streak Test % % %! # " Step 3: Luster surface % " $ % % luster Metallic: % Submetallic: % Adamantine: % Glassy: % Resinous: % Waxy: % Pearly: % Dull: %
27 # Specimen # Test 1-4 STEP 1: COLOR Draw the texture of your rock below: % % " " % " " " % STEP 2: STREAK TEST STEP 4: Mohs Hardness Test " % %!!! "! STEP 3: LUSTER
28 STEP 6: Magnetism Test Specimen # Test 5-8 STEP 5: Cleavage Step 7: Acid Test (Use Vinegar or lemon juice) $!! Step 8: Now to identify your rock!
29 " " % % % % " "!! "!! " STEP 4: Mohs Hardness Test # $ $ % % % % " # % STEP 5: Cleavage or Fracture Test Fracture Cleaveage smooth, flat surfaces Cleavage not Fracture % cleave
30 STEP 6: Magnetism Test # # % % chromite pyrrhotite! " % calcium carbonate!! % %!!!! STEP 7: Chemical Reaction
31 Image courtesy of THE NATURE OF SEDIMENTARY ROCKS 2 Sedimentary rocks form from fragments derived from other rocks and by precipitation from water. They typically occur in layers, or strata, separated one from the other by bedding planes and differences in composition. The second type of rocks are called sedimentary rocks. They are formed from the breakdown and chemical decay of preexisting rocks. This sediment is compacted and cemented to form new solid rock. The origin of these sediment are formed from various substances: 1. Clastic: Fragments of other rocks and minerals. 2. Biologic: Organic materials such as plants or animals. Biologic sedimentary rocks will often contain fossils. 3. Chemical: corrosion and weathering by water or precipitation of other rocks being worn away to create new rocks. What are the three types of sedimentary rocks? Draw an example of a biologic rock in the box below:
32 % " " Types of Sedimentary Rock Groups Clastic Clastic (clasts = pieces) Biologic % perish Biologic sedimentary Chemical elements dissolved in water.
33 " #!!! # #! Writing super sentences who or what predicate subject sentence! tells " #! # " Instructions: Subject Predicate determiner Adjective noun verb when? or where? "! " # " # "!!! # # " #! # " " " "! "
34 Let us practice! igneous rocks #! Subject Predicate determiner Adjective noun verb when? or where? "! " #! Subject Predicate determiner Adjective noun verb when? or where?
35 Name: Date:
36 Name: Date: Sedimentary rocks are formed from sediment grains deposited by water, wind or ice.
37 Name: Combine each pair of ideas into a compound sentence by using a comma and a conjunction such as and, but, or or. Compound Sentences
38 Title: Fossils By: Sedimentary rocks are always formed in layers, called beds or strata, and often contain fossils.
39 Draw an example of sediment accumulating alongside riverbanks. Stratification is the building up of layers. Stratified is an adjective referring to the arranging of layers, and is also the past form of the verb stratify, to separate or become separated into layers. Visit for examples of sedimentary rocks. KEY CONCEPTS ~ STRATIFICATION 2 Draw an example of stratified layers of sedimentary rock: Sedimentary rocks are formed from particles of sand, shells, pebbles, and other fragments of material. Together, all these particles are called sediment. Gradually, the sediment accumulates in layers and over a long period of time hardens into rock. Generally, sedimentary rock is fairly soft and may break apart or crumble easily. You can often see sand, pebbles, or stones in the rock, and it is usually the only type that contains fossils. (Types of Rocks) When you hold your rock and rub your fingers against it, if the textures feel grainy, chances are it is sedimentary rock. Another type of sedimentary rock has layers instead of particles. This type of sedimentary rock is even easier to identify than the particle type. It is still made up of particles, but particles that form definite layers, called stratum (more typically referred to using the plural, which is strata) Works Cited Types of Rocks (n.d.). Retrieved May 11, 2012, from Learner:
40 Name: Date: Title: Sediments Most often sediments settle outside of the water. For example the river carries lots of sediment, and
41 where the water slows down, the sediments collect along the riverbanks, into lakes, and in the ocean which then form layers.
42 Visit for a more detailed lesson on sedimentary rocks 2 What type of rocks can become sedimentary rocks? / 108 % accuracy WCPM Weathering and Erosion 12 Any type of rock exposed at the surface of the earth can 22 become a sedimentary rock. As rocks are continually exposed to 33 weathering over prolonged periods of time, they are broken down and 42 transported to streams, rivers, and oceans. Even large majestic 52 mountains such as the Appalachian Mountains slowly begin to crumble 61 because of rain, snow, ice, wind, and running water. What are sediments? 72 These little bits of rocks and sand are called sediments. These 83 sediments are transported through flowing bodies of water, and as the 95 water slows down the sediments settle to the bottom. Over many years, 108 layers of different rock settle to the bottom of rivers, lakes and oceans. 1 minute timed reading ~ Score the number of words read aloud correctly in one minute.
43 Name: Date: Erosion SEDIMENTARY LITHOLOGIC PATTERNS Erosion is the process when wind or water move pieces of sediment.
44 1 Weathering When a rock is weathered, it is broken down over time by forces like wind and water. Weathering turns rocks into sediment. 2 Erosion Sediment is carried away by erosion. Erosion is the process when wind or water move pieces of sediment.
45 Deposition 3 Deposition is when sediment is loosely put together in a layer by erosion. Compaction 4 The sediment is compacted. Compaction means that the sediment is being squeezed together and made smaller and tighter. As the layers of sediment build up, the pressure on the lower layers increases. The layers are squeezed together and any water mixed in with the sediments is forced out. This process is called compaction.
46 5 Cementation Sediment is cemented together. At the same time the particles of sediment begin to stick to each other - they are cemented together by clay, or by minerals like silica or calcite. Image courtesy of Tulane University 2012 ~ geol212/sedrxintro.htm for information on the process of cementation. Identifying Sedimentary Rocks After compaction and cementation the sedimentary sequence has changed into a sedimentary rock. Sedimentary rocks like sandstone, shale and limestone differ from other rocks in that they: 1. Are formed from layers of sediment built up over many years. 2. Are grains of sediment cemented together by various minerals. 3. May contain fossils - remains of plants and animals that were caught up in the sediment.
47 Name: Date: Weathering When a rock is weathered, it is broken down over time by forces like wind and water.
48 3 Metamorphic Rock / 127 % accuracy WCPM How are metamorphic rocks created? Metamorphic rocks are formed deep within the earth when heat and pressure are applied to igneous, sedimentary rocks, or even other metamorphic rocks. This process of heating and adding pressure changes the physical structure of the rock, and/or the chemicals within them are rearranged so the final rock is very different from the original rock. During a chemical change, ions move and new minerals form. The new minerals are more stable in the new environment. Although the minerals in the rock change they do not melt. The final state of the metamorphic rock depends on the amount of pressure and heat the original rock was subjected to, and length of time the rock was subjected to the pressure and heat. This process of changing is called metamorphism.
49 / 159 % accuracy WCPM REGIONAL METAMORPHISM Regional metamorphic rocks happens when rocks get buried under other rocks. The weight of the rocks on top forces them deeper into the earth. The deeper the rocks are pushed into the ground, the more they are exposed to pressure and heat. Regional metamorphism occurs over a very wide geographical area. Regional metamorphic rocks often display layering or banding called foliation. Extreme pressure may also result in foliation. Foliation occurs when rocks are squeezed, and if pressure is exerted from one direction, the rocks can form layers. If pressure is exerted from all directions, the rock usually does not show foliation. Regional metamorphism with high pressure and low temperatures can often result in blue schist. Some examples of foliated rocks are Slate, Schist and Mica. Slate is transformed shale and it splits into smooth slabs. Schist is the most common metamorphic rock. Mica is the most common mineral. Gneiss has a streaky look because of alternating layers of minerals. What is foliation? Image courtesy of ~ Website Gem. Visit their website for more information about metamorphic (A) FOLIATION (B) BLUE SCHIST
50 Name: Date: Metamorphic Rocks Read the sentence below Practice writing the words Spell each word aloud Draw a picture of the paragraph below. Metamorphic rocks are rocks that have changed. The word comes from the Greek word meta and morph which means to change form.
51 Name: Date: Metamorphic Rock Origins Read the sentence below Practice writing the words Spell each word aloud Draw a picture of the paragraph below. Metamorphic rocks were originally igneous or sedimentary rock, but due to movement of the earth s crust, were changed.
52 CONTACT METAMORPHISM Contact metamorphism occurs when magma intrudes or forces its way into existing rock. The heat of the magma bakes the surrounding rocks causing them to change. This is a local event. The changes due to contact metamorphism are relatively small and are said to be low-grade metamorphism. An example of contact metamorphism is the metamorphic rock marble. Marble is created from limestone and dolostone that has been subjected to heat. Contact Metamorphic Rocks Limestone Marble The word marble comes from the Greek word marmaros which means shining stone. There are many types of rocks found throughout the world.
53 CAUSES OF METAMORPHISM The causes of metamorphism are heat, pressure, and hydrothermal solution. But where does this heat and pressure come from? The heat and pressure comes from inside the earth. From the upper mantle up to within a few kilometers of the surface of the earth there is a tremendous amount of heat and pressure. This heat and pressure increase with depth. It is estimated that the temperature increases about 20 to 30 C per kilometer of depth. Plate Tectonics Adds Heat And Pressure There is something else that adds to both the heat and pressure, and that is plate tectonics. When the plates of the earth collide, they squeeze the rocks at the borders with unbelievable force. This force increases the pressure in this and surrounding areas. Friction is also created by the plates grinding together. This friction generates enough heat to melt the rocks at the point of contact. Pressure The pressure within the earth is the result of gravity pulling the crust of the earth downward. Like heat, pressure increases with depth. This pressure can actually squeeze the spaces out of the minerals within the rock. This makes the rocks denser. The heat and pressure together cause the rock to flow instead of break or fracture. The mineral grains become realigned. They flatten out and get longer. Hydrothermal Solution Magma contains many different gasses including H2O. That s right water! Or more properly steam. Minerals are carried by the steam. When this hot fluid escapes from the magma it is called Hydrothermal Solution. These hot fluids can change the crystallization in rock by dissolving the minerals and then depositing new ones. Rocks that come in contact with this hydrothermal solution can have their composition altered as a result of this recrystalization. Heat For metamorphism to occur energy is needed to fuel the chemical reactions. Heat is the primary source of this energy. What causes metamorphism?
54 LANDMARKS In our experiment, we are using baking soda (Sodium bicarbonate), an alkali and Acetic Acid vinegar. When we combine the two ingredients, and the reaction creates carbonic acid. The carbonic acid is unstable and immediately becomes carbon dioxide and water. This is where the bubbles come from! Draw a picture of your volcano below: INSTRUCTIONS Step 1: Step 2: Step 3: Optional Step: Step 4: MATERIALS:
55 Name: Date: Circle an adjective from the word bank. Draw a picture of one of your rocks. Write a sentence with adjectives that describes one of the rocks you have chosen below. Spell each word aloud Color Adjectives red orange yellow green blue purple gray black white
56 Name: Date: Write a sentence with an adjective and verb, that describes cementation. Spell each word aloud and check your spelling. Draw a picture to represent the paragraph below
57 Name: Date: Write a sentence that describes what type of rocks fossils are found in. Spell each word aloud and check your spelling. Draw a picture to represent the paragraph below
58 TIME READING PASSAGES Words correct per minute (WCPM). Choose a passage. Time the student when s/he reads the passage. Example A student read a story with 148 words in 2 minutes, 55 seconds. She made 8 errors. To determine WCPM: 1. Count the total number of words. Example: Count the number of mistakes. Example: Take the number of words minus the number of mistakes = number of words read correctly. Example: = Calculate percent accuracy: number of words read correctly divided by total number of words. Example: 130/148 = 87% 5. Convert the time it took to read the passage to seconds. Example: 2 minutes, 55 seconds = 175 seconds 6. Convert the number of seconds to a decimal by dividing the number of seconds by 60. This is the total reading time. Example: 175 / 60 = Divide the number of words read correctly by the total reading time in decimal form. Example: 130 / 2.91 = 45 WCPM
59 Matthew Age 7 Matthew Age 7
60
61 ARABIC CARD GAME Cut out each of the cards below. ت ت ت ب ب ب ا ا أ ح ح ح ج ج ج ث ث ث
62 ARABIC CARD GAME
63 ذ ذ ذ د د د خ خ خ س س س ز ز ز ر ر ر
64 ARABIC CARD GAME
65 ARABIC CARD GAME Cut out each of the cards below. ض ض ض ص ص ص ش ش ش ع ع ع ظ ظ ظ ط ط ط
66 ARABIC CARD GAME
67 ق ق ق ف ف ف غ غ غ م م م ل ل ل ك ك ك
68 ARABIC CARD GAME
69 ARABIC CARD GAME Cut out each of the cards below. ي ي ي ه ه ه ن ن ن و و و
70 ARABIC CARD GAME
71 Name: Date: Practice Writing and Connecting Arabic Letters Use the cards to write each letter in its original form. Practice connecting each of the letters together to form a word. Spell each word aloud
72 Name: Date: Practice Writing and Connecting Arabic Letters Use the cards to write each letter in its original form. Practice connecting each of the letters together to form a word. Spell each word aloud
73 Name: Date: Practice Writing and Connecting Arabic Letters Use the cards to write each letter in its original form. Practice connecting each of the letters together to form a word. Spell each word aloud
74
6/20/2018. Lesson 1 (Properties of Minerals) 6 th Grade. Earth s Structure Chapter 2: Minerals and Rocks. density =
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