Type of sedimentary rock is formed from minerals that were once dissolved in water and formed when minerals precipitated from the solution, settle from the Type suspension, of sedimentary or are rock left behind is formed after from the minerals water that were once dissolved evaporates. in water and formed when minerals precipitated from the solution, settle from the suspension, or are left behind after the water evaporates. Type of sedimentary rock that is made up of rock fragments that become compacted or cemented together Type of sedimentary rock that is made up of rock fragments that become compacted or cemented together Process that causes minerals in metamorphic rock to realign into layers due to extreme pressure. The crystallization and removal of different minerals from cooling magma Process that causes minerals in metamorphic rock to realign into layers due to extreme pressure. The crystallization and removal of different minerals from cooling magma The sedimentary rock formation when small sediment settles on the bottom and large grains settle on top The sedimentary rock formation when small sediment settles on the bottom and large grains settle on top The sedimentary rock formation when large grains settle on the bottom and small sediment settles on top The sedimentary rock formation when large grains settle on the bottom and small sediment settles on top The tendency for currents of air or water to separate sediments according to size The process that causes layers and beds to form in sedimentary rock The tendency for currents of air or water to separate sediments according to size The process that causes layers and beds to form in sedimentary rock Three factors that determine whether rock melts The process by which different minerals melt at different temperatures Three factors that determine whether rock melts The process by which different minerals melt at different temperatures The name for this type of rock means from fire in Latin. The name for this type of rock means changed form in Latin. The name for this type of rock means from fire in Latin. The name for this type of rock means changed form in Latin.
Clastic Sedimentary Rock Chemical Sedimentary Rock Clastic Sedimentary Rock Chemical Sedimentary Rock Fractional crystallization Foliation Fractional crystallization Foliation graded bedding reverse grading graded bedding reverse grading Stratification Sorting Stratification Sorting Partial melting Temperature, Pressure, Presence of fluids in the rock Partial melting Temperature, Pressure, Presence of fluids in the rock Metamorphic rock (in Latin) Igneous rock (in Latin) Metamorphic rock (in Latin) Igneous rock (in Latin)
Tiny/No crystals w/ holes - rock that forms when magma is cooled instantly on Earth's surface so no crystals have time to grow, and has many dissolved gasses Tiny/No it crystals so bubbles w/ holes form - causing rock that holes forms to when be left magma is cooled in the instantly rock after on it Earth's cools surface so no crystals have time to grow, and has many dissolved gasses in it so bubbles form causing holes to be left in the rock after it cools rock that forms when existing rock is altered by the forces of heat or chemical processes, but NOT pressure, so the crystals are not aligned in layers. rock that forms when existing rock is altered by the forces of heat or chemical processes, but NOT pressure, so the crystals are not aligned in layers. No crystals or holes - rock that forms when magma is cooled instantly on Earth's surface so no crystals have time to grow, and has few/no dissolved gasses in it so no holes form in it No crystals or holes - rock that forms when magma is cooled instantly on Earth's surface so no crystals have time to grow, and has few/no dissolved gasses in it so no holes form in it rock that forms from the remains of plants or animals rock that forms from the remains of plants or animals rock that forms when existing rock is altered by the forces of heat & pressure causing the crystals to align in layers. rock that forms when existing rock is altered by the forces of heat & pressure causing the crystals to align in layers. Has small crystals - rock that forms when magma cools and hardens near the earth s surface; the magma cools quickly because it is further from the core & so only small crystals have time to grow. Has small crystals - rock that forms when magma cools and hardens near the earth s surface; the magma cools quickly because it is further from the core & so only small crystals have time to grow. Large crystals - rock that forms when magma cools and hardens deep in the mantle; the magma cools slowly because it is closer to the core & so large crystals have time to grow. Large crystals - rock that forms when magma cools and hardens deep in the mantle; the magma cools slowly because it is closer to the core & so large crystals have time to grow. Mixture of big & small crystals - rock that forms when magma starts out cooling slowly deep in the mantle (so some minerals grow big crystals), but is then moved Mixture closer of big to (or & small onto) crystals Earth s surface - rock that and forms finishes cooling when magma quickly starts (so other out cooling minerals slowly only have deep time in the mantle (so some to grow minerals small crystals) grow big crystals), but is then moved closer to (or onto) Earth s surface and finishes cooling quickly (so other minerals only have time to grow small crystals) Which conditions would produce the largest crystals in igneous rock? Which conditions would produce the smallest crystals in igneous rock? Which conditions would produce the largest crystals in igneous rock? Which conditions would produce the smallest crystals in igneous rock? Name the 3 classes of Sedimentary rock Name the 3 classes of Sedimentary rock The process in which one type of rock changes into another type of rock because of chemical processes or changes in temperature and pressure The process in which one type of rock changes into another type of rock because of chemical processes or changes in temperature and pressure
Nonfoliated metamorphic rock Vesicular igneous rock Nonfoliated metamorphic rock Vesicular igneous rock Organic sedimentary rock Glassy igneous rock Organic sedimentary rock Glassy igneous rock Fine-grained igneous rock Foliated metamorphic rock Fine-grained igneous rock Foliated metamorphic rock Porphyritic igneous rock Coarse-grained igneous rock Porphyritic igneous rock Coarse-grained igneous rock minerals with low melting points, cooling quickly minerals with high melting points, cooling slowly minerals with low melting points, cooling quickly minerals with high melting points, cooling slowly Metamorphism Metamorphism Chemical Sedimentary Rock Clastic Sedimentary Rock Organic Sedimentary Rock Chemical Sedimentary Rock Clastic Sedimentary Rock Organic Sedimentary Rock
the process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock the process in which the volume and porosity of a sediment is decreased by the weight of the layers above it. the process in which minerals precipitate into pore spaces between sediment grains and bind sediments together to form rock the process in which the volume and porosity of a sediment is decreased by the weight of the layers above it. Type of formation environment Petoskey stones tells us & why Type of formation environment Gypsum & Halite tells us & why Type of formation environment Petoskey stones tells us & why Type of formation environment Gypsum & Halite tells us & why Type of formation environment Conglomerate tells us & why Type of formation environment Breccia tells us & why Type of formation environment Conglomerate tells us & why Type of formation environment Breccia tells us & why Type of formation environment Limestone tells us & why Type of formation environment Coal tells us & why Type of formation environment Limestone tells us & why Type of formation environment Coal tells us & why Characteristics of Sedimentary rock Characteristics of Metamorphic rock Characteristics of Sedimentary rock Characteristics of Metamorphic rock Name the 5 classes of Igneous rock Characteristics of Igneous rock Name the 5 classes of Igneous rock Characteristics of Igneous rock
Compaction Cementation Compaction Cementation Shallow saltwater environment - b/c these are formed by water evaporating and leaving large amounts of minerals behind. In order to have all evaporated, the area Shallow must've saltwater been shallow, environment & to leave - b/c large these amounts are formed of minerals, by water it would evaporating have been and classified leaving large amounts of minerals as saltwater. behind. In order to have all evaporated, the area must've been shallow, & to leave large amounts of minerals, it would have been classified as saltwater. Shallow, warm saltwater - b/c the fossils in this stone are the remains of coral, which only live in this type of environment. Shallow, warm saltwater - b/c the fossils in this stone are the remains of coral, which only live in this type of environment. Glacial drift/ mountain foothills - b/c the rock fragments in this rock have jagged unevenly broken edges, which form as they are tumbled down a hill by gravity or dragged along by a glacier. Glacial drift/ mountain foothills - b/c the rock fragments in this rock have jagged unevenly broken edges, which form as they are tumbled down a hill by gravity or dragged along by a glacier. Streambed - b/c the rock fragments in this rock have rounded edges, which form as they are tumbled along the bottom of a body of moving water and evenly worn smooth. Streambed - b/c the rock fragments in this rock have rounded edges, which form as they are tumbled along the bottom of a body of moving water and evenly worn smooth. Tropical swamp - b/c it is formed out of spagnum moss which only grows in tropical swamps Tropical swamp - b/c it is formed out of spagnum moss which only grows in tropical swamps marine (saltwater) - b/c it is made of marine invertabrate shells containing calcite that we can detect b/c it reacts with acid. marine (saltwater) - b/c it is made of marine invertabrate shells containing calcite that we can detect b/c it reacts with acid. foliated or nonfoliated, crystals (some), very compressed layers, doesn't feel gritty or dirty sediment/rock fragments, plant/animal material, reacts w/acid, feels gritty or dirty foliated or nonfoliated, crystals (some), very compressed layers, doesn't feel gritty or dirty sediment/rock fragments, plant/animal material, reacts w/acid, feels gritty or dirty Crystal (most), Coarse-grained, fine-grained, porphyritic, vesicular, glassy, holes Coarse-grained, Fine-grained, Porphyritic, Glassy, Vesicular Crystal (most), Coarse-grained, fine-grained, porphyritic, vesicular, glassy, holes Coarse-grained, Fine-grained, Porphyritic, Glassy, Vesicular
a change in the texture, structure, or chemical composition of a rock due to changes in temperature and pressure over a large area, generally as a result a change of tectonic in the forces texture, (most structure, common or type chemical of composition metamorphism) of a rock due to changes in temperature and pressure over a large area, generally as a result of tectonic forces (most common type of metamorphism) a rock that forms from compressed or cemented layers of sediment a rock that forms from compressed or cemented layers of sediment a rock that forms from other rocks as a result of intense heat, pressure, or chemical processes the metamorphic rock texture in which mineral grains are not arranged in planes or bands a rock that forms from other rocks as a result of intense heat, pressure, or chemical processes the metamorphic rock texture in which mineral grains are not arranged in planes or bands magma that flows onto Earth s surface liquid rock produced under the Earth's surface magma that flows onto Earth s surface liquid rock produced under the Earth's surface rock that forms when magma cools and solidifies rock formed from the cooling and solidification of magma beneath the Earth's surface rock that forms when magma cools and solidifies rock formed from the cooling and solidification of magma beneath the Earth's surface a process in which the materials of Earth's surface are loosened, dissolved, or worn away and transported from one place to another by a natural agent, such as wind, water, ice, or gravity a process in which the materials of Earth's surface are loosened, dissolved, or worn away and transported from one place to another by a natural agent, such as wind, water, ice, or gravity rock that forms from the cooling and solidification of lava on Earth's surface rock that forms from the cooling and solidification of lava on Earth's surface a change in the texture, structure, or chemical composition of a rock due to contact with magma the process in which material is laid down a change in the texture, structure, or chemical composition of a rock due to contact with magma the process in which material is laid down
Sedimentary rock Regional metamorphism Sedimentary rock Regional metamorphism Nonfoliated Metamorphic rock Nonfoliated Metamorphic rock Magma Lava Magma Lava Intrusive igneous rock Igneous rock Intrusive igneous rock Igneous rock Extrusive igneous rock Erosion Extrusive igneous rock Erosion Deposition Contact Metamorphism Deposition Contact Metamorphism
This type of material is made of eroded or dissolved plant or animal remains This type of material is made of eroded or dissolved plant or animal remains The series of processes in which rock forms, changes from one type to another, is destroyed, and forms again by geologic processes The series of processes in which rock forms, changes from one type to another, is destroyed, and forms again by geologic processes fragments of organic or inorganic material that are transported and deposited by wind, water, or ice and that accumulate in layers on the Earth's surface fragments of organic or inorganic material that are transported and deposited by wind, water, or ice and that accumulate in layers on the Earth's surface This type of material is made of eroded or dissolved rock fragments or minerals that are not made of plant or animal remains This type of material is made of eroded or dissolved rock fragments or minerals that are not made of plant or animal remains
The rock cycle Organic material The rock cycle Organic material Inorganic material Sediment Inorganic material Sediment