Rocks are composed of different minerals and there are three main types: igneous, sedimentary, and metamorphic. Igneous rocks form from solidified magma or lava. Sedimentary rocks form through the compaction and cementation of sediments and may include sandstone, shale, and limestone. Metamorphic rocks were once igneous or sedimentary rocks that were changed by heat and pressure in the Earth's crust, such as limestone metamorphosing into marble or shale into slate.
This document discusses different types of rocks and where they are found. It describes rocks as being hard or soft, shiny or dull, smooth or rough, and various colors. Sedimentary rocks form from layers of sediment joining together, metamorphic rocks form from changes caused by pressure and heat to other rocks, and igneous rocks form when melted rock cools and hardens. Rocks are used for building, decoration, instruments, and even pets, chalk, and toothpaste. Rocks change size through erosion, earthquakes, volcanoes, floods, wind, and human activity. The three main types of rocks are sedimentary, metamorphic, and igneous.
The document summarizes various rock structures around the world, describing their composition, location, and uses. It discusses structures in Europe like the Colosseum (travertine), Arc de Triomphe (limestone), Bowerman's Nose (granite), and Devil's Organ Pipes (basalt). In North America it mentions Mount Rushmore (granite), Grand Canyon (limestone, shale), The Jug Rock (sandstone), and Old Man of the Mountain (granite). Structures in Asia described include the Great Wall of China (limestone, granite), India Gate (granite, sandstone), Amah Rock (granite), and Queen's Head (sandstone).
The document discusses the geology around Lake Tahoe, including the area's granite formations from the underlying Sierra Nevada batholith. It also describes various rock types found in the region such as diorite, andesite, gneiss, and an angular unconformity example on Twin Peaks. Local plants and animals like the sagebrush lizard and mule's ear flower are also mentioned. The area was impacted by a large 2007 wildfire on Angora Ridge that destroyed homes but led to new construction.
The document discusses different types of relief models that shape landscapes through erosion and deposition. The main models covered are fluvial (river), torrential, glacial, karstic (subterranean water), littoral (coastal), and eolic (wind-driven).
The fluvial model forms valleys, floodplains, and wave-cut platforms near rivers. The torrential model produces canyons and gullies through powerful erosion. The glacial model sculpts U-shaped valleys and cirques through ice erosion. The karstic model forms caves and sinkholes through rock dissolution. The littoral model generates cliffs, beaches, and arches along coastlines. The e
Strata are horizontal layers of rock formed over long periods of time. Sedimentary rock is formed through the stratification of sediment particles deposited in layers. Strata reveal the geological history of the Earth through their arrangement, composition, and changes indicating forces that altered their positioning over millions of years. Different rock types record this history through their formation processes of igneous, sedimentary, or metamorphic.
This document discusses igneous rocks and their formation. It explains that igneous rocks form as magma cools and crystallizes. There are different textures of igneous rocks depending on factors like cooling rate and mineral grain size. Igneous rocks are also classified based on their composition as felsic, intermediate, or mafic. Common igneous rocks are described like granite, rhyolite, basalt, and gabbro.
The document discusses three main types of rocks: igneous, metamorphic, and sedimentary. It provides details about the formation of each. Igneous rocks form from cooled magma and their color depends on the cooling rate. Metamorphic rocks form deep underground from the heat and pressure changing one rock into another. Sedimentary rocks like sandstone, limestone, and shale form from compressed sediments and contain visible layers. The document includes examples of each rock type and notes that the author collected mostly metamorphic rocks.
This document provides information about igneous rocks, including:
- Igneous rocks form from the crystallization of magma, which is molten rock located beneath the Earth's surface or lava on the surface.
- There are two main types of igneous rocks: extrusive rocks, which solidify on the surface, and intrusive rocks, which solidify underground.
- Factors like cooling rate and mineral composition determine the texture of the igneous rock, ranging from glassy to phaneritic.
- Igneous rocks can be classified based on their composition as felsic, intermediate, or mafic rocks like granite, andesite, and basalt respectively.
This document discusses different types of rocks and where they are found. It describes rocks as being hard or soft, shiny or dull, smooth or rough, and various colors. Sedimentary rocks form from layers of sediment joining together, metamorphic rocks form from changes caused by pressure and heat to other rocks, and igneous rocks form when melted rock cools and hardens. Rocks are used for building, decoration, instruments, and even pets, chalk, and toothpaste. Rocks change size through erosion, earthquakes, volcanoes, floods, wind, and human activity. The three main types of rocks are sedimentary, metamorphic, and igneous.
The document summarizes various rock structures around the world, describing their composition, location, and uses. It discusses structures in Europe like the Colosseum (travertine), Arc de Triomphe (limestone), Bowerman's Nose (granite), and Devil's Organ Pipes (basalt). In North America it mentions Mount Rushmore (granite), Grand Canyon (limestone, shale), The Jug Rock (sandstone), and Old Man of the Mountain (granite). Structures in Asia described include the Great Wall of China (limestone, granite), India Gate (granite, sandstone), Amah Rock (granite), and Queen's Head (sandstone).
The document discusses the geology around Lake Tahoe, including the area's granite formations from the underlying Sierra Nevada batholith. It also describes various rock types found in the region such as diorite, andesite, gneiss, and an angular unconformity example on Twin Peaks. Local plants and animals like the sagebrush lizard and mule's ear flower are also mentioned. The area was impacted by a large 2007 wildfire on Angora Ridge that destroyed homes but led to new construction.
The document discusses different types of relief models that shape landscapes through erosion and deposition. The main models covered are fluvial (river), torrential, glacial, karstic (subterranean water), littoral (coastal), and eolic (wind-driven).
The fluvial model forms valleys, floodplains, and wave-cut platforms near rivers. The torrential model produces canyons and gullies through powerful erosion. The glacial model sculpts U-shaped valleys and cirques through ice erosion. The karstic model forms caves and sinkholes through rock dissolution. The littoral model generates cliffs, beaches, and arches along coastlines. The e
Strata are horizontal layers of rock formed over long periods of time. Sedimentary rock is formed through the stratification of sediment particles deposited in layers. Strata reveal the geological history of the Earth through their arrangement, composition, and changes indicating forces that altered their positioning over millions of years. Different rock types record this history through their formation processes of igneous, sedimentary, or metamorphic.
This document discusses igneous rocks and their formation. It explains that igneous rocks form as magma cools and crystallizes. There are different textures of igneous rocks depending on factors like cooling rate and mineral grain size. Igneous rocks are also classified based on their composition as felsic, intermediate, or mafic. Common igneous rocks are described like granite, rhyolite, basalt, and gabbro.
The document discusses three main types of rocks: igneous, metamorphic, and sedimentary. It provides details about the formation of each. Igneous rocks form from cooled magma and their color depends on the cooling rate. Metamorphic rocks form deep underground from the heat and pressure changing one rock into another. Sedimentary rocks like sandstone, limestone, and shale form from compressed sediments and contain visible layers. The document includes examples of each rock type and notes that the author collected mostly metamorphic rocks.
This document provides information about igneous rocks, including:
- Igneous rocks form from the crystallization of magma, which is molten rock located beneath the Earth's surface or lava on the surface.
- There are two main types of igneous rocks: extrusive rocks, which solidify on the surface, and intrusive rocks, which solidify underground.
- Factors like cooling rate and mineral composition determine the texture of the igneous rock, ranging from glassy to phaneritic.
- Igneous rocks can be classified based on their composition as felsic, intermediate, or mafic rocks like granite, andesite, and basalt respectively.
The document describes three types of rocks - milky quartz, resin rock, and magnet rock - that a child collected. Milky quartz is clear and common, resin rock forms from sap over millions of years, and magnet rock sticks to metal and is shiny black. The child enjoys their clear milky quartz because they can see through it.
A man’s guide to wearing ruby studded jewelryRuby Gemstone
According to orthodox believes only women have right to wear jewelry’s or they have an inclination toward jewelry items. However, even in the ancient times, we get strong evidences that men also appreciates wearing jewelry items, And, in this modern age where fashion has no gender and both men and women are kept on experimenting with something unique and distinct all times. So, now this never remains a question that whether men should wear jewelry or not. And, men too can graciously include jewelry items in their wardrobe. http://ruby.org.in/blog/mans-guide-wearing-ruby-studded-jewelry-items/
India has a wide variety of dimensional stone resources found across the country, including granite, marble, sandstone, limestone, slate, and quartzite. It is a major producer and exporter of raw stone materials. The stone industry produces products like flooring slabs, sculptures, and landscape stones. Key stone types found in India include granite, sandstone, slate, limestone, and marble. Important stone producing regions include Rajasthan, Gujarat, Madhya Pradesh, Karnataka, and Andhra Pradesh.
Rocks are used in many different ways such as pebbles for paths, gravel for driveways, sand for castles, and clay for chimneys according to the document. Pebbles were used to create the path, gravel was used to build the driveway, sand was used for the castle, and clay was used for the chimney. The document provides examples of different types of rocks and how they are used for paths, driveways, castles, and chimneys.
This document discusses different types of stones that are commonly used as building materials. It describes several stones including granite, limestone, marble, sandstone, slate, and basalt. These stones are classified based on factors like hardness, texture, and chemical composition. The document outlines the characteristics of good building stones, which include being durable, easily obtainable, and weathering well. It also lists common uses of stone in construction such as for floors, walls, roads, and filters.
Coastlines are under threat from natural forces like erosion and faults. Swanage Bay in England was formed when softer clay eroded away due to corrasion, leaving the harder limestone protruding and creating a headland feature. A cave and fault line arch collapsed at Old Harry Rocks due to the force of gravity.
Rocks continuously change forms through the rock cycle. There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma, sedimentary rocks form from compressed and cemented sediments, and metamorphic rocks form from existing rocks undergoing heat and pressure. Plate tectonics and the rock cycle drive the recycling of Earth's rocks as they change forms over millions of years.
This document introduces the three main types of rocks - igneous, sedimentary, and metamorphic rocks - and explores their definitions, formations, examples, and uses. It examines how rocks provide insights into Earth's history and cycles through different transformations over time. Finally, it discusses the many practical applications of rocks in construction, infrastructure, and everyday life.
This document provides an overview of the three main types of rocks: igneous, sedimentary, and metamorphic rocks. It describes their formation processes and gives examples. Igneous rocks such as granite and basalt form from the cooling of magma either underground or above ground. Sedimentary rocks like limestone and sandstone form through the compression of sediments over time. Metamorphic rocks including marble and quartzite form from existing rocks undergoing heat or pressure changes. The uses of different rock types such as limestone and granite in construction are also detailed.
Minerals are found in rocks and there are over 3000 known types of minerals. Minerals have different properties like color, hardness, streak, and luster that can be used to identify them. There are three main types of rocks: igneous rocks which form from cooling magma or lava, sedimentary rocks which form from compressed and cemented sediment, and metamorphic rocks which form from other rocks being subjected to heat and pressure below the earth's surface. Common rocks like granite, shale, and marble are used for construction materials, building monuments, and other purposes due to their unique properties.
The document discusses the internal structure of the Earth and the solid part known as the geosphere. It is composed mainly of minerals and rocks. Minerals form over long periods of time through crystallization and are extracted from mines and quarries. Some key minerals mentioned include quartz, the most abundant mineral in the Earth's crust, and graphite. Rocks are aggregates of minerals and can be classified as sedimentary, metamorphic, or igneous based on their formation process. Minerals and rocks have many important uses for buildings, infrastructure, agriculture, and more.
Rocks are naturally occurring mixtures of minerals, mineraloids, glass or organic matter that are divided into three main types - igneous, sedimentary, and metamorphic - based on how they were formed. Rocks are continually changed over time by various geological processes through the rock cycle, where one type of rock can be transformed into another through weathering, erosion, melting and other changes. The core, mantle and crust act as a recycling machine that redistributes rocks.
The document is a "Do Now" assignment for students that includes:
- Instructions to get materials and complete a reading on the rock cycle with 6 follow up questions
- The reading provides an overview of the rock cycle, explaining how rocks are formed from igneous, sedimentary, and metamorphic types through processes like weathering, melting, and pressure/heat.
- An agenda for the class period including the Do Now, a lesson on the rock cycle, a mastery assignment, a rock cycle lab, and an exit ticket.
This document provides information about rocks and minerals. It begins by defining minerals as natural, nonliving solid crystals that make up rocks. It then discusses the three main classifications of rocks: igneous, sedimentary, and metamorphic. Igneous rocks such as basalt form from cooled lava. Sedimentary rocks like shale and limestone form from compressed sediments. Metamorphic rocks like marble form from existing rocks undergoing heat and pressure. The document also explores properties of minerals like color, luster, hardness, and crystal shape that scientists use to identify them. It describes how rocks change through heat, pressure, chemical reactions and other forces in the rock cycle.
The document discusses the three main types of rocks: sedimentary, metamorphic, and igneous. Sedimentary rocks are formed from the compression of sediment layers over time. Metamorphic rocks were once sedimentary or igneous rocks, but were changed by heat and pressure. Igneous rocks form either underground from cooled magma or above ground from volcanic eruptions. Examples of each rock type are also provided.
Rocks form in three main types - igneous, sedimentary, and metamorphic - depending on their formation process. Igneous rocks form when magma cools and hardens, sedimentary rocks form through the compaction and cementation of sediments, and metamorphic rocks form through the alteration of existing rocks by heat, pressure, and chemical reactions. The main types of rocks each have distinguishing characteristics and provide clues about Earth's environmental history.
The document discusses three main types of rocks: sedimentary rocks which are formed from compressed layers of settled earth materials; metamorphic rocks which were once igneous or sedimentary rocks but were changed by heat and pressure; and igneous rocks which form from cooled lava either underground or from volcanoes. Examples of each rock type are provided.
The document discusses three main types of rocks: sedimentary rocks which are formed from compressed layers of settled earth materials; metamorphic rocks which were once igneous or sedimentary rocks but were changed by heat and pressure; and igneous rocks which form from cooled lava either underground or from volcanoes. Examples of each rock type are provided.
The document discusses the rock cycle and different types of rocks. It describes how igneous rocks such as basalt and pumice are formed by volcanic activity. Sedimentary rocks like sandstone and limestone form through the compaction and cementation of sediments. Metamorphic rocks such as marble and slate are formed by the transformation of other rock types under heat and pressure. Fossils provide evidence of past life and the document includes examples. Weathering, erosion, temperature and pressure are identified as natural processes that change and cycle rocks over time.
The document discusses the three main types of rocks: sedimentary, metamorphic, and igneous. Sedimentary rocks are formed from the compression of sediment layers over time. Metamorphic rocks were once sedimentary or igneous rocks, but were changed by heat and pressure. Igneous rocks form from the cooling of magma, either underground or from volcanic eruptions. Examples of each rock type are provided.
Minerals are nonliving substances that occur naturally with distinct properties. Common minerals include calcite, feldspar, mica, and hornblende. Sedimentary rocks form from the compaction and cementation of minerals and organic materials like plant and animal fragments. Igneous rocks form from cooling magma either below or above the Earth's surface. Metamorphic rocks are formed from the alteration of existing rock types like sedimentary and igneous rocks through heat, pressure, and chemical changes. The rock cycle illustrates how the three main rock types are interrelated and can transform into one another over time through geological processes.
The document describes three types of rocks - milky quartz, resin rock, and magnet rock - that a child collected. Milky quartz is clear and common, resin rock forms from sap over millions of years, and magnet rock sticks to metal and is shiny black. The child enjoys their clear milky quartz because they can see through it.
A man’s guide to wearing ruby studded jewelryRuby Gemstone
According to orthodox believes only women have right to wear jewelry’s or they have an inclination toward jewelry items. However, even in the ancient times, we get strong evidences that men also appreciates wearing jewelry items, And, in this modern age where fashion has no gender and both men and women are kept on experimenting with something unique and distinct all times. So, now this never remains a question that whether men should wear jewelry or not. And, men too can graciously include jewelry items in their wardrobe. http://ruby.org.in/blog/mans-guide-wearing-ruby-studded-jewelry-items/
India has a wide variety of dimensional stone resources found across the country, including granite, marble, sandstone, limestone, slate, and quartzite. It is a major producer and exporter of raw stone materials. The stone industry produces products like flooring slabs, sculptures, and landscape stones. Key stone types found in India include granite, sandstone, slate, limestone, and marble. Important stone producing regions include Rajasthan, Gujarat, Madhya Pradesh, Karnataka, and Andhra Pradesh.
Rocks are used in many different ways such as pebbles for paths, gravel for driveways, sand for castles, and clay for chimneys according to the document. Pebbles were used to create the path, gravel was used to build the driveway, sand was used for the castle, and clay was used for the chimney. The document provides examples of different types of rocks and how they are used for paths, driveways, castles, and chimneys.
This document discusses different types of stones that are commonly used as building materials. It describes several stones including granite, limestone, marble, sandstone, slate, and basalt. These stones are classified based on factors like hardness, texture, and chemical composition. The document outlines the characteristics of good building stones, which include being durable, easily obtainable, and weathering well. It also lists common uses of stone in construction such as for floors, walls, roads, and filters.
Coastlines are under threat from natural forces like erosion and faults. Swanage Bay in England was formed when softer clay eroded away due to corrasion, leaving the harder limestone protruding and creating a headland feature. A cave and fault line arch collapsed at Old Harry Rocks due to the force of gravity.
Rocks continuously change forms through the rock cycle. There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma, sedimentary rocks form from compressed and cemented sediments, and metamorphic rocks form from existing rocks undergoing heat and pressure. Plate tectonics and the rock cycle drive the recycling of Earth's rocks as they change forms over millions of years.
This document introduces the three main types of rocks - igneous, sedimentary, and metamorphic rocks - and explores their definitions, formations, examples, and uses. It examines how rocks provide insights into Earth's history and cycles through different transformations over time. Finally, it discusses the many practical applications of rocks in construction, infrastructure, and everyday life.
This document provides an overview of the three main types of rocks: igneous, sedimentary, and metamorphic rocks. It describes their formation processes and gives examples. Igneous rocks such as granite and basalt form from the cooling of magma either underground or above ground. Sedimentary rocks like limestone and sandstone form through the compression of sediments over time. Metamorphic rocks including marble and quartzite form from existing rocks undergoing heat or pressure changes. The uses of different rock types such as limestone and granite in construction are also detailed.
Minerals are found in rocks and there are over 3000 known types of minerals. Minerals have different properties like color, hardness, streak, and luster that can be used to identify them. There are three main types of rocks: igneous rocks which form from cooling magma or lava, sedimentary rocks which form from compressed and cemented sediment, and metamorphic rocks which form from other rocks being subjected to heat and pressure below the earth's surface. Common rocks like granite, shale, and marble are used for construction materials, building monuments, and other purposes due to their unique properties.
The document discusses the internal structure of the Earth and the solid part known as the geosphere. It is composed mainly of minerals and rocks. Minerals form over long periods of time through crystallization and are extracted from mines and quarries. Some key minerals mentioned include quartz, the most abundant mineral in the Earth's crust, and graphite. Rocks are aggregates of minerals and can be classified as sedimentary, metamorphic, or igneous based on their formation process. Minerals and rocks have many important uses for buildings, infrastructure, agriculture, and more.
Rocks are naturally occurring mixtures of minerals, mineraloids, glass or organic matter that are divided into three main types - igneous, sedimentary, and metamorphic - based on how they were formed. Rocks are continually changed over time by various geological processes through the rock cycle, where one type of rock can be transformed into another through weathering, erosion, melting and other changes. The core, mantle and crust act as a recycling machine that redistributes rocks.
The document is a "Do Now" assignment for students that includes:
- Instructions to get materials and complete a reading on the rock cycle with 6 follow up questions
- The reading provides an overview of the rock cycle, explaining how rocks are formed from igneous, sedimentary, and metamorphic types through processes like weathering, melting, and pressure/heat.
- An agenda for the class period including the Do Now, a lesson on the rock cycle, a mastery assignment, a rock cycle lab, and an exit ticket.
This document provides information about rocks and minerals. It begins by defining minerals as natural, nonliving solid crystals that make up rocks. It then discusses the three main classifications of rocks: igneous, sedimentary, and metamorphic. Igneous rocks such as basalt form from cooled lava. Sedimentary rocks like shale and limestone form from compressed sediments. Metamorphic rocks like marble form from existing rocks undergoing heat and pressure. The document also explores properties of minerals like color, luster, hardness, and crystal shape that scientists use to identify them. It describes how rocks change through heat, pressure, chemical reactions and other forces in the rock cycle.
The document discusses the three main types of rocks: sedimentary, metamorphic, and igneous. Sedimentary rocks are formed from the compression of sediment layers over time. Metamorphic rocks were once sedimentary or igneous rocks, but were changed by heat and pressure. Igneous rocks form either underground from cooled magma or above ground from volcanic eruptions. Examples of each rock type are also provided.
Rocks form in three main types - igneous, sedimentary, and metamorphic - depending on their formation process. Igneous rocks form when magma cools and hardens, sedimentary rocks form through the compaction and cementation of sediments, and metamorphic rocks form through the alteration of existing rocks by heat, pressure, and chemical reactions. The main types of rocks each have distinguishing characteristics and provide clues about Earth's environmental history.
The document discusses three main types of rocks: sedimentary rocks which are formed from compressed layers of settled earth materials; metamorphic rocks which were once igneous or sedimentary rocks but were changed by heat and pressure; and igneous rocks which form from cooled lava either underground or from volcanoes. Examples of each rock type are provided.
The document discusses three main types of rocks: sedimentary rocks which are formed from compressed layers of settled earth materials; metamorphic rocks which were once igneous or sedimentary rocks but were changed by heat and pressure; and igneous rocks which form from cooled lava either underground or from volcanoes. Examples of each rock type are provided.
The document discusses the rock cycle and different types of rocks. It describes how igneous rocks such as basalt and pumice are formed by volcanic activity. Sedimentary rocks like sandstone and limestone form through the compaction and cementation of sediments. Metamorphic rocks such as marble and slate are formed by the transformation of other rock types under heat and pressure. Fossils provide evidence of past life and the document includes examples. Weathering, erosion, temperature and pressure are identified as natural processes that change and cycle rocks over time.
The document discusses the three main types of rocks: sedimentary, metamorphic, and igneous. Sedimentary rocks are formed from the compression of sediment layers over time. Metamorphic rocks were once sedimentary or igneous rocks, but were changed by heat and pressure. Igneous rocks form from the cooling of magma, either underground or from volcanic eruptions. Examples of each rock type are provided.
Minerals are nonliving substances that occur naturally with distinct properties. Common minerals include calcite, feldspar, mica, and hornblende. Sedimentary rocks form from the compaction and cementation of minerals and organic materials like plant and animal fragments. Igneous rocks form from cooling magma either below or above the Earth's surface. Metamorphic rocks are formed from the alteration of existing rock types like sedimentary and igneous rocks through heat, pressure, and chemical changes. The rock cycle illustrates how the three main rock types are interrelated and can transform into one another over time through geological processes.
The document discusses the rock cycle and how different types of rocks are formed. It defines rocks as aggregates of minerals and describes the three main types - igneous, sedimentary, and metamorphic - based on their mode of origin. The rock cycle describes how rocks can be transformed into different types through geological processes like crystallization, weathering and erosion, deposition, lithification, and metamorphism due to pressure and heat within the Earth. Plate tectonics also influence the rock cycle as rocks form at sites of volcanic activity, mountain building, and sediment deposition at plate boundaries.
There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from cooled lava or magma, sedimentary rocks form from compressed layers of sediment, and metamorphic rocks form from existing rocks that are altered by heat and pressure. Rocks are constantly changing between these types in the rock cycle as they are exposed to different environmental conditions over long periods of time.
Metamorphic rocks are formed deep within the earth's crust under conditions of high heat and pressure. Sedimentary rock layers sink over time, heating up and experiencing increasing weight as they move closer to the center of the earth, transforming them into metamorphic rocks. These metamorphic rocks can be exposed at the surface through mountain building when tectonic plates collide and push rock upwards, or through erosion of overlying rock over time. Examples of metamorphic rocks include slate, marble, and greenstone.
This document discusses three main rock types: igneous, metamorphic, and sedimentary rocks. It provides details on how each type forms, characteristics of each type, and examples of common rocks for each type. The concluding summary is that the described rock is likely an igneous rock based on its dark color and heavy weight.
3. RocksRocks
All the rocks you see around you areAll the rocks you see around you are
made up of different mineralsmade up of different minerals
Imagine a rock is a chocolate chip cookie,Imagine a rock is a chocolate chip cookie,
what does the cookie contain?what does the cookie contain?
Flour, butter, sugar, chocolate chipsFlour, butter, sugar, chocolate chips
A rock contains different ingredients, theyA rock contains different ingredients, they
are called minerals. There are about 3000are called minerals. There are about 3000
minerals in the world.minerals in the world.
4. 3 Types of Rocks3 Types of Rocks
There are 3 main types of rocksThere are 3 main types of rocks
IgneousIgneous
SedimentarySedimentary
MetamorphicMetamorphic
5. Igneous RocksIgneous Rocks
Igneous means made from fire or heat.Igneous means made from fire or heat.
When volcanoes erupt and the liquid rockWhen volcanoes erupt and the liquid rock
comes up to the earth's surface, then newcomes up to the earth's surface, then new
igneous rock is made.igneous rock is made.
When the rock is liquid & inside theWhen the rock is liquid & inside the
earth, it is called magma.earth, it is called magma.
When the magma gets hard inside theWhen the magma gets hard inside the
crust, it turns into granite.crust, it turns into granite.
Most mountains are made of granite. ItMost mountains are made of granite. It
cools very slowly and is very hardcools very slowly and is very hard..
8. Sedimentary RocksSedimentary Rocks
Mountains are made of rockMountains are made of rock
Weather can make the mountain rockWeather can make the mountain rock
crumblecrumble
These little bits of rock fall into rivers andThese little bits of rock fall into rivers and
streams and rest on the riverbedstreams and rest on the riverbed
11. Sedimentary RocksSedimentary Rocks
Limestone is a type ofLimestone is a type of
sedimentary rocksedimentary rock
The EgyptianThe Egyptian
pyramids were madepyramids were made
using limestone.using limestone.
12. Metamorphic RocksMetamorphic Rocks
Metamorphic rocks are ones that haveMetamorphic rocks are ones that have
changed.changed.
‘‘Meta’ and ‘morph’ both mean change inMeta’ and ‘morph’ both mean change in
GreekGreek
All metamorphic rocks would once haveAll metamorphic rocks would once have
been igneous or sedimentary.been igneous or sedimentary.
What do you think made them change?What do you think made them change?
14. Metamorphic RocksMetamorphic Rocks
Squeeze your hands together as tightly asSqueeze your hands together as tightly as
you can.you can.
What do you notice?What do you notice?
Your hands will start to get warm and youYour hands will start to get warm and you
will feel pressure. This is a bit like thewill feel pressure. This is a bit like the
Earth’s crust pressing its rocks. The heatEarth’s crust pressing its rocks. The heat
and pressure changes them into aand pressure changes them into a
different type of rock.different type of rock.
16. Slate is another metamorphic rock, formed from shale. It is used to roof
houses because it forms in thin layers.
17. Rocks and their usesRocks and their uses
Rocks are very useful, can you think whatRocks are very useful, can you think what
they are used for?they are used for?
Fireplaces, roofs, worktops, tables, walls,Fireplaces, roofs, worktops, tables, walls,
sharpening knives, headstones,sharpening knives, headstones,
ornaments, pathways, jewellery, drawing,ornaments, pathways, jewellery, drawing,
scrubbing feet!scrubbing feet!
What are the properties of rocks?What are the properties of rocks?
Do they all have the same properties?Do they all have the same properties?
18. Beautiful Rocks!Beautiful Rocks!
People like to wear rocks as jewellery andPeople like to wear rocks as jewellery and
decorate their homes with rocks.decorate their homes with rocks.
Can you think of examples of these rocks?Can you think of examples of these rocks?
21. Other words for RocksOther words for Rocks
We sometimes call rocks pebbles, boulders,We sometimes call rocks pebbles, boulders,
stones, crystals or gemstones.stones, crystals or gemstones.
A boulder is a large rockA boulder is a large rock
A pebble is a small rock that has been roundedA pebble is a small rock that has been rounded
by wind or water.by wind or water.
Stones are larger than pebbles.Stones are larger than pebbles.
Crystals and gemstones are rocks made of justCrystals and gemstones are rocks made of just
one mineral. E.g a diamond is made of carbon.one mineral. E.g a diamond is made of carbon.
Editor's Notes
The whole earth is made of rocks & minerals. Inside the earth there is a liquid core of molten rock and on the outside there is a hard crust. If you compare the earth to an egg, the shell on an egg is like the crust on the earth. The crust is made up of rocks and minerals. Much of the crust is covered by water, sand, soil and ice. If you dig deep enough, you will always hit rocks
Think of the fragments of rock as pieces of paper, a few sheets of paper wouldn’t make any weight difference, but a big stack of yellow pages would soon weigh heavily. Eventually the weight of the rocks forms sedimentary rocks (over millions of years)
Sandstone and shale are two examples of sedimentary rocks, they are both soft rocks. Many sedimentary rocks contain the fossilised remains of plants and animals which have fallen onto the river bed after dying. They then become mixed with the layers of rock, forming sedimentary rocks over time.
The Earth’s crust is made up of lots of plates which are moving, when they move rapidly they can cause earthquakes. Metamorphic rocks are formed by changes in the Earth’s crust.
The fireplace is made of marble.
Allow children to discuss their ideas with talking partner/table group. Introduce terms permeable/impermeable. Hard/soft, rough/smooth, can be scratched, can’t be scratched.