Physical Geography Geomorphology
... overflow, and that this one channel survives - a fine example of ...
... overflow, and that this one channel survives - a fine example of ...
National Geographic – Colliding Continents Video
... formed? _______________ years old 7. What continent is believed to be the site of the earliest giant continental land mass on Earth? _______________ 8. What type of rock formed the first continents? _________________________ 9. As radioactive uranium decays it turns into what stable element? _______ ...
... formed? _______________ years old 7. What continent is believed to be the site of the earliest giant continental land mass on Earth? _______________ 8. What type of rock formed the first continents? _________________________ 9. As radioactive uranium decays it turns into what stable element? _______ ...
earthsciencechap17qu..
... 10: A convergent boundary is the place where two plates meet. 11: The youngest rocks on the sea flood are found in rifts in the mid-ocean ridges. 12: Alfred Wegener proposed the theory of continental drift. 13: According to plate tectonics, the Earth’s lithosphere is divided into several huge, movin ...
... 10: A convergent boundary is the place where two plates meet. 11: The youngest rocks on the sea flood are found in rifts in the mid-ocean ridges. 12: Alfred Wegener proposed the theory of continental drift. 13: According to plate tectonics, the Earth’s lithosphere is divided into several huge, movin ...
Metamorphic rock is the result of the transformation of an existing
... rock, (called a protolith), is subjected to heat and pressure (temperatures greater than 150 to 200 °C and pressures of 1500 bars) causing profound physical and/or chemical change. The protolith may be sedimentary rock, igneous rock or another older metamorphic rock. Metamorphic rocks make up a larg ...
... rock, (called a protolith), is subjected to heat and pressure (temperatures greater than 150 to 200 °C and pressures of 1500 bars) causing profound physical and/or chemical change. The protolith may be sedimentary rock, igneous rock or another older metamorphic rock. Metamorphic rocks make up a larg ...
Lesson 1: Earth Energy Lesson
... As the mantle moves around, the crust “floating” on top of it is “deformed” into different shapes and features! These features include: Mountains, valleys, canyons, volcanoes, oceans, deep sea trenches, etc… ...
... As the mantle moves around, the crust “floating” on top of it is “deformed” into different shapes and features! These features include: Mountains, valleys, canyons, volcanoes, oceans, deep sea trenches, etc… ...
Earth Science Lecture - Quiz 1
... c. open system / matter and energy are exchanged through sub-systems ...
... c. open system / matter and energy are exchanged through sub-systems ...
Document
... A single fold is a hinge defined by the maximum curvature of the beds. The hinge line joins the points of maximum bending along a bed. The axial surface, or plane, passes through the hinges of successive beds, while the axis of the fold is any line on the bed which is parallel to the hinge line. Whe ...
... A single fold is a hinge defined by the maximum curvature of the beds. The hinge line joins the points of maximum bending along a bed. The axial surface, or plane, passes through the hinges of successive beds, while the axis of the fold is any line on the bed which is parallel to the hinge line. Whe ...
Plate Tectonics Review Sheet
... very hot rock Lithosphere –uppermost part of mantle is very similar to the Earth’s crust Asthenosphere – a hotter soft layer beneath the lithosphere and is less rigid than the lithosphere; plastic “silly-putty” like The Lower Mantle – Beneath the asthenosphere is made up of solid rock and extends to ...
... very hot rock Lithosphere –uppermost part of mantle is very similar to the Earth’s crust Asthenosphere – a hotter soft layer beneath the lithosphere and is less rigid than the lithosphere; plastic “silly-putty” like The Lower Mantle – Beneath the asthenosphere is made up of solid rock and extends to ...
Plate Tectonics Review Sheet
... very hot rock Lithosphere –uppermost part of mantle is very similar to the Earth’s crust Asthenosphere – a hotter soft layer beneath the lithosphere and is less rigid than the lithosphere; plastic “silly-putty” like The Lower Mantle – Beneath the asthenosphere is made up of solid rock and extends to ...
... very hot rock Lithosphere –uppermost part of mantle is very similar to the Earth’s crust Asthenosphere – a hotter soft layer beneath the lithosphere and is less rigid than the lithosphere; plastic “silly-putty” like The Lower Mantle – Beneath the asthenosphere is made up of solid rock and extends to ...
Year 9 - Bedford Free School
... outside the Earth's surface, and instrusive, which form over a longer period of time under the Earth's surface. Igneous rocks can be identified by their crystalline internal structure. The larger the crystals, the longer the rock took to cool and soldify. Sedimentary rocks are formed when debris and ...
... outside the Earth's surface, and instrusive, which form over a longer period of time under the Earth's surface. Igneous rocks can be identified by their crystalline internal structure. The larger the crystals, the longer the rock took to cool and soldify. Sedimentary rocks are formed when debris and ...
plate tectonics
... – One tectonic plate is forced under another plate as the plates push together. ...
... – One tectonic plate is forced under another plate as the plates push together. ...
UP7.LP3.RockCycleGNStarburst
... The series of processes that change one type of rock into another type of rock is called the ________________________ ...
... The series of processes that change one type of rock into another type of rock is called the ________________________ ...
Plate Tectonics Crossword
... 5. this forms at a subduction zone 8. a country sometimes referred to as a sub-continent that crashed into Asia and formed the Himalayas 9. the German scientist who hypothesized about continental drift 10. a supercontinent that existed in the past 11. any trace of an ancient organism preserved in ro ...
... 5. this forms at a subduction zone 8. a country sometimes referred to as a sub-continent that crashed into Asia and formed the Himalayas 9. the German scientist who hypothesized about continental drift 10. a supercontinent that existed in the past 11. any trace of an ancient organism preserved in ro ...
Spheres glossary quiz - HSIE Teachers
... A theory which proposes that all the continents were once joined together in a giant supercontinent, which subsequently split apart, with the continents drifting away from one another until they reached their current locations ...
... A theory which proposes that all the continents were once joined together in a giant supercontinent, which subsequently split apart, with the continents drifting away from one another until they reached their current locations ...
Vocabulary Review - POTOSI SCHOOL DISTRICT
... an event or object is older or younger than other events or objects ...
... an event or object is older or younger than other events or objects ...
Plate Tectonics Crossword - www .alexandria .k12 .mn .us
... 5. Section of the Earth below the crust. 7. Paleontologists noticed that these were the same on different continents even though the continents were separated by oceans. 9. Source of heat in the mantle. (Hints: Starts with something you listen to in the car, and, it ends in –ity) 11. Seafloor ______ ...
... 5. Section of the Earth below the crust. 7. Paleontologists noticed that these were the same on different continents even though the continents were separated by oceans. 9. Source of heat in the mantle. (Hints: Starts with something you listen to in the car, and, it ends in –ity) 11. Seafloor ______ ...
OUTDOOR SCIENCE SCHOOL VOC (#1 – Test)
... most portion of the crust that floats above the asthenosphere, which causes the rigid area of the crust to crack and form the lithospheric plates (b) asthenosphere – liquid, tar-like layer of the upper mantle below the lithosphere creating a convection current movement, which causes the plates to mo ...
... most portion of the crust that floats above the asthenosphere, which causes the rigid area of the crust to crack and form the lithospheric plates (b) asthenosphere – liquid, tar-like layer of the upper mantle below the lithosphere creating a convection current movement, which causes the plates to mo ...
File
... lava cools instantly through contact with air and water. The minerals do not have time to form, so they are microscopic. Examples : obsidian, basalt ...
... lava cools instantly through contact with air and water. The minerals do not have time to form, so they are microscopic. Examples : obsidian, basalt ...
Intrusive Igneous Activity
... Expansion of a near-surface magma chamber leading to the inflation of a volcano Changes in the amount and/or composition of the gases that are ...
... Expansion of a near-surface magma chamber leading to the inflation of a volcano Changes in the amount and/or composition of the gases that are ...
Slide 1
... in any sequence of sedimentary strata, the order in which he strata were deposited from the bottom up. older strata are truncated by erosion before younger strata are deposited. fine deposits overlie coarser units. strata were deposited as horizontal layers. ...
... in any sequence of sedimentary strata, the order in which he strata were deposited from the bottom up. older strata are truncated by erosion before younger strata are deposited. fine deposits overlie coarser units. strata were deposited as horizontal layers. ...
convection current
... (upper part is solid, lower part is partly melted). The upper mantle together with the crust forms the lithosphere. - The rock material in the mantle can flow very slowly. - Below the mantle is the core. The outer core is made up mainly of liquid iron and nickel, while the inner core is solid. Evide ...
... (upper part is solid, lower part is partly melted). The upper mantle together with the crust forms the lithosphere. - The rock material in the mantle can flow very slowly. - Below the mantle is the core. The outer core is made up mainly of liquid iron and nickel, while the inner core is solid. Evide ...
Geology
Geology (from the Greek γῆ, gē, i.e. ""earth"" and -λoγία, -logia, i.e. ""study of, discourse"") is an earth science comprising the study of solid Earth, the rocks of which it is composed, and the processes by which they change. Geology can also refer generally to the study of the solid features of any celestial body (such as the geology of the Moon or Mars).Geology gives insight into the history of the Earth by providing the primary evidence for plate tectonics, the evolutionary history of life, and past climates. Geology is important for mineral and hydrocarbon exploration and exploitation, evaluating water resources, understanding of natural hazards, the remediation of environmental problems, and for providing insights into past climate change. Geology also plays a role in geotechnical engineering and is a major academic discipline.