File - Down To Earth Science
... South Africa line up with mountain ranges in Argentina (South America). ...
... South Africa line up with mountain ranges in Argentina (South America). ...
plate boundaries lab - Hastings Middle School
... What type of boundary is in the middle of the Atlantic ocean between The Americas and Europe/Africa plates? a. Transform b. Divergent c. Convergent The boundary in #3 is in an ocean, what is forming here? a. Mid ocean ridge b. Trench c. Rift Valley Where is the ocean rock the oldest in the Atlantic? ...
... What type of boundary is in the middle of the Atlantic ocean between The Americas and Europe/Africa plates? a. Transform b. Divergent c. Convergent The boundary in #3 is in an ocean, what is forming here? a. Mid ocean ridge b. Trench c. Rift Valley Where is the ocean rock the oldest in the Atlantic? ...
Right Side Crust
... To access the “Plate Tectonics Exercise” files, go to my website and click on where it says “click here for…” This will bring you to another website where you will need to scroll down and find the download titled “Google Earth data files and supporting animations.” Once downloaded, the file you will ...
... To access the “Plate Tectonics Exercise” files, go to my website and click on where it says “click here for…” This will bring you to another website where you will need to scroll down and find the download titled “Google Earth data files and supporting animations.” Once downloaded, the file you will ...
Developed in Consultation with Florida Educators
... move over the land. burning everything in its path. When the lava cools and hardens, it forms new igneous rock. Some volcanoes form over hot spots rather than at plate boundaries. A hot spot is an unusually hot, basically stationary area in the mantle through which magma rises. Volcanoes sometimes f ...
... move over the land. burning everything in its path. When the lava cools and hardens, it forms new igneous rock. Some volcanoes form over hot spots rather than at plate boundaries. A hot spot is an unusually hot, basically stationary area in the mantle through which magma rises. Volcanoes sometimes f ...
Geologic history - Hewlett
... • ABSOLUTE: actual date known. If 2 dates are known, then the RATE OF CHANGE can be known- such as Mountain Building. ...
... • ABSOLUTE: actual date known. If 2 dates are known, then the RATE OF CHANGE can be known- such as Mountain Building. ...
Deforming the Earth`s Crust
... and push up the margin of the plates. • When this happens mountain building may occur. • Three types of mountains are: Folded, Fault-Block and Volcanic. ...
... and push up the margin of the plates. • When this happens mountain building may occur. • Three types of mountains are: Folded, Fault-Block and Volcanic. ...
Terms you should be able to define and concepts you should
... than the structure it cuts. For example, if a granite dike cuts through a sandstone layer, the sandstone had to be there first and, therefore, is older than the dike. Figure 3 (see next page) illustrates a geological cross section showing sedimentary rocks (A,B,D,E,F, and G), an igneous intrusion fe ...
... than the structure it cuts. For example, if a granite dike cuts through a sandstone layer, the sandstone had to be there first and, therefore, is older than the dike. Figure 3 (see next page) illustrates a geological cross section showing sedimentary rocks (A,B,D,E,F, and G), an igneous intrusion fe ...
Plate Boundaries – Lesson Plan- WA
... Have students research a specific plate boundary and recent activity that has taken place at this site. Have students create a poster that describes that type of plate boundary, the recent activity, and a diagram predicting future activity in the area. ...
... Have students research a specific plate boundary and recent activity that has taken place at this site. Have students create a poster that describes that type of plate boundary, the recent activity, and a diagram predicting future activity in the area. ...
Rocks
... materials so hot that it was liquid. Most of the liquid rock material cooled and hardened below the surface of the earth. Some of the liquid rock broke through the surface, flowed out and then hardened. Igneous rocks underlie all other rocks of the earth. It forms the base of the continent and the c ...
... materials so hot that it was liquid. Most of the liquid rock material cooled and hardened below the surface of the earth. Some of the liquid rock broke through the surface, flowed out and then hardened. Igneous rocks underlie all other rocks of the earth. It forms the base of the continent and the c ...
2.1 Tectonic Forces
... A fringing reef forms around a volcanic island or land mass. It is made by corals which are colonies of animals that make shell homes of rock-like calcium carbonate (limestone). As coral organisms cement layer upon layer of their homes on lower layers, a reef structure arises from the ocean floor an ...
... A fringing reef forms around a volcanic island or land mass. It is made by corals which are colonies of animals that make shell homes of rock-like calcium carbonate (limestone). As coral organisms cement layer upon layer of their homes on lower layers, a reef structure arises from the ocean floor an ...
Terms you should be able to define and concepts you should
... than the structure it cuts. For example, if a granite dike cuts through a sandstone layer, the sandstone had to be there first and, therefore, is older than the dike. Figure 3 (see next page) illustrates a geological cross section showing sedimentary rocks (A,B,D,E,F, and G), an igneous intrusion fe ...
... than the structure it cuts. For example, if a granite dike cuts through a sandstone layer, the sandstone had to be there first and, therefore, is older than the dike. Figure 3 (see next page) illustrates a geological cross section showing sedimentary rocks (A,B,D,E,F, and G), an igneous intrusion fe ...
Ocean Basins Are Formed at Divergent Plate Boundaries
... (Above Right) A cross section through the west coast of South America, showing the convergence of a continental plate and an oceanic plate. The subducting oceanic plate becomes more dense as it descends, its downward slide propelled by gravity. At a depth of about 80 kilometers (50 miles), heat driv ...
... (Above Right) A cross section through the west coast of South America, showing the convergence of a continental plate and an oceanic plate. The subducting oceanic plate becomes more dense as it descends, its downward slide propelled by gravity. At a depth of about 80 kilometers (50 miles), heat driv ...
Measuring Earthquakes
... Earthquakes are vibrations caused by earth movements at plate boundaries and at major fault lines (cracks in the earth’s surface). They can occur at all 3 major plate boundaries but the most severe earthquakes are normally found at conservative and convergent plate boundaries. ...
... Earthquakes are vibrations caused by earth movements at plate boundaries and at major fault lines (cracks in the earth’s surface). They can occur at all 3 major plate boundaries but the most severe earthquakes are normally found at conservative and convergent plate boundaries. ...
Earthquakes - Epiphany Catholic School
... * Transform plate boundary * Rocks on either side of fault move past each other without much up or down motion. * relatively shallow – upper 50km of crust Big one – San Andreas Fault in CA ...
... * Transform plate boundary * Rocks on either side of fault move past each other without much up or down motion. * relatively shallow – upper 50km of crust Big one – San Andreas Fault in CA ...
Introduction to Geology
... • Sediments will lithify into sedimentary rocks • Accumulate in layers at Earth’s surface • Metamorphic rocks • Formed by “changing” preexisting igneous, sedimentary, or other metamorphic rocks • Driving forces are heat and pressure ...
... • Sediments will lithify into sedimentary rocks • Accumulate in layers at Earth’s surface • Metamorphic rocks • Formed by “changing” preexisting igneous, sedimentary, or other metamorphic rocks • Driving forces are heat and pressure ...
Applying Concepts 33. a. Index fossils in each sequence can be
... 2. Deep time is the theory that Earth has gone through a very long history (4.5 billion years) of development and change. 3. The eras are the Precambrian Era, the Paleozoic Era, the Mesozoic Era, and the Cenozoic Era. 4. Diagram C is the most accurate representation of time for each of the combined ...
... 2. Deep time is the theory that Earth has gone through a very long history (4.5 billion years) of development and change. 3. The eras are the Precambrian Era, the Paleozoic Era, the Mesozoic Era, and the Cenozoic Era. 4. Diagram C is the most accurate representation of time for each of the combined ...
Kenny Nielsen - Kenny`s Website
... The cause of earthquakes and the formation of the volcanoes all have to do with plate tectonics. When plates move or shift this is what creates and earthquake. Three main types of movements of the plates are involved, convergent, transform and divergent boundaries, causing earthquakes on land and in ...
... The cause of earthquakes and the formation of the volcanoes all have to do with plate tectonics. When plates move or shift this is what creates and earthquake. Three main types of movements of the plates are involved, convergent, transform and divergent boundaries, causing earthquakes on land and in ...
earthquakes and mountain building ppt
... understanding of earth's processes. – Although it is known where earthquakes and volcanic eruptions are likely to happen, there is currently no reliable way to predict precisely when an event will occur. – Volcanoes and earthquakes indicate the high temperatures and pressures that exist in earth's i ...
... understanding of earth's processes. – Although it is known where earthquakes and volcanic eruptions are likely to happen, there is currently no reliable way to predict precisely when an event will occur. – Volcanoes and earthquakes indicate the high temperatures and pressures that exist in earth's i ...
Geology of Lava Beds National Monument
... American and Pacific Plates came into direct contact and the San Andreas developed as a result of the shear between them (Fig. 3). It has since grown to a length of 750 kilometers, and is but one strand in a broad zone of right-lateral deformation that extends eastward to the Nevada border. In south ...
... American and Pacific Plates came into direct contact and the San Andreas developed as a result of the shear between them (Fig. 3). It has since grown to a length of 750 kilometers, and is but one strand in a broad zone of right-lateral deformation that extends eastward to the Nevada border. In south ...
Large igneous province
A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.