unit cover page - Bremen High School District 228
... take place so sporadically or so slowly (over hundreds of millions of years) that we cannot observe them but only infer that they take place from other kinds of evidence. Identify the various features of the ocean floor which furnish evidence for plate tectonics: magnetic patterns, age, and topograp ...
... take place so sporadically or so slowly (over hundreds of millions of years) that we cannot observe them but only infer that they take place from other kinds of evidence. Identify the various features of the ocean floor which furnish evidence for plate tectonics: magnetic patterns, age, and topograp ...
Chapter 1: Basic Seismology and Earthquake Terminology
... are called hanging wall and foot wall (Fig. 1.4). The fault movement (rupture) does not always break through to the ground surface and is then known as Blind Fault. Faults normally exist along boundaries of the tectonic plates (inter-plate) but can also exist within a plate (intra-plate). ...
... are called hanging wall and foot wall (Fig. 1.4). The fault movement (rupture) does not always break through to the ground surface and is then known as Blind Fault. Faults normally exist along boundaries of the tectonic plates (inter-plate) but can also exist within a plate (intra-plate). ...
Crustal Interactions Midterm Rev
... 4) The crust is composed of denser rock than the mantle is. 9 The Himalaya Mountains are located along a portion of the southern boundary of the Eurasian Plate. At the top of Mt. Everest (29,028 feet) in the Himalaya Mountains, climbers have found fossilized marine shells in the surface bedrock. Fro ...
... 4) The crust is composed of denser rock than the mantle is. 9 The Himalaya Mountains are located along a portion of the southern boundary of the Eurasian Plate. At the top of Mt. Everest (29,028 feet) in the Himalaya Mountains, climbers have found fossilized marine shells in the surface bedrock. Fro ...
evidences of active faulting in thrace region (north
... work is focused on the N-S oriented faults and its activity potential, observed in Southern Thrace. The diachronic activity of these faults and the changes in the movement type (from clearly normal to oblique or strikeslip) are indicated in the slickenside groups observed on the existing polished fa ...
... work is focused on the N-S oriented faults and its activity potential, observed in Southern Thrace. The diachronic activity of these faults and the changes in the movement type (from clearly normal to oblique or strikeslip) are indicated in the slickenside groups observed on the existing polished fa ...
worksheet a MS Word file ()
... Objective: Address Learning Outcome #1 – Students will understand the methods and limits of scientific investigation by progressing through a problem or question about the earth and environment, in this case, damage caused by seismic waves, then see the design of an experiment to acquire verifiable ...
... Objective: Address Learning Outcome #1 – Students will understand the methods and limits of scientific investigation by progressing through a problem or question about the earth and environment, in this case, damage caused by seismic waves, then see the design of an experiment to acquire verifiable ...
Imaging Unknown Faults in Christchurch, New Zealand, after a M6.2 Earthquake
... and north of Christchurch. The Greendale Fault (Figure 1b) was not previously known until it ruptured to surface during the Darfield earthquake. The right-lateral displacement across the Greendale Fault is illustrated in Figure 2a. It is postulated that stress transfer from the Darfield earthquake, ...
... and north of Christchurch. The Greendale Fault (Figure 1b) was not previously known until it ruptured to surface during the Darfield earthquake. The right-lateral displacement across the Greendale Fault is illustrated in Figure 2a. It is postulated that stress transfer from the Darfield earthquake, ...
6 Unit 3 _ Internal Forces Study Guide - Google Docs
... 4. Explain why the three volcanos have distinctive shapes. 5. Explain the process of determining the distance a seismograph is from the epicenter. 6. Be able to identify a hanging wall and a footwall for a fault block diagram. 7. Be able to determine the fault type based on a fault block diagram ...
... 4. Explain why the three volcanos have distinctive shapes. 5. Explain the process of determining the distance a seismograph is from the epicenter. 6. Be able to identify a hanging wall and a footwall for a fault block diagram. 7. Be able to determine the fault type based on a fault block diagram ...
Lec-08 - nptel
... Even for P waves (which can travel all the way through) we see some changes in the path at certain points within Earth. This is due to the discontinuities present at different boundaries in earth structure ...
... Even for P waves (which can travel all the way through) we see some changes in the path at certain points within Earth. This is due to the discontinuities present at different boundaries in earth structure ...
F SR Faults and Folds Lab
... 2. Does this fault result from tension or compression? _______________________________ 3. What type of tectonic boundary does this fault represent? __________________________ 4. Which fault wall is showing, the foot wall or hanging wall? __________________________ 5. In a reverse fault, the hanging ...
... 2. Does this fault result from tension or compression? _______________________________ 3. What type of tectonic boundary does this fault represent? __________________________ 4. Which fault wall is showing, the foot wall or hanging wall? __________________________ 5. In a reverse fault, the hanging ...
Criticisms of the subduction concept – can mobilism renounce to it?
... filiform clusterized patterns. Very difficult to explain with plate motion. motion. A migration of a deep disturbance surfaceward is favoured. favoured. ...
... filiform clusterized patterns. Very difficult to explain with plate motion. motion. A migration of a deep disturbance surfaceward is favoured. favoured. ...
San Andreas Fault Trail – A Self
... between San Francisco and Portola Valley shifted 7 to 9 feet, and from this area southward it only shifted 2 to 3 feet. The 1906 earthquake may not have released all the energy stored in the southern part of the fault. Smaller quakes, similar to the Loma Prieta, may have released the energy. In any ...
... between San Francisco and Portola Valley shifted 7 to 9 feet, and from this area southward it only shifted 2 to 3 feet. The 1906 earthquake may not have released all the energy stored in the southern part of the fault. Smaller quakes, similar to the Loma Prieta, may have released the energy. In any ...
Fierce Volcanoes and Extreme Earthquakes
... 1. Layers of the Earth: Pinhole Book If you could slice through the earth, you would see different layers of matter making up the earth, almost like a boiled egg. The topmost covering is called the crust. It is a layer of rocks that is thicker under land than under the ocean. It is about 5 km deep ...
... 1. Layers of the Earth: Pinhole Book If you could slice through the earth, you would see different layers of matter making up the earth, almost like a boiled egg. The topmost covering is called the crust. It is a layer of rocks that is thicker under land than under the ocean. It is about 5 km deep ...
Volcano Earthquake Notes
... • Scientists use the similarity of rock types and fossil types that date to the same age to support their theory that the continents were connected to form a super continent. • The map below give just one example of areas on different continents that show the same fossils and rock types. ...
... • Scientists use the similarity of rock types and fossil types that date to the same age to support their theory that the continents were connected to form a super continent. • The map below give just one example of areas on different continents that show the same fossils and rock types. ...
EarthScience_Topic 9-Properties of Earths Interior
... 1) Take a sheet of paper and line up the left edge with the vertical axis (time). Be sure that most of the paper is hanging down below the graph. This is important. 2) Make a small, thin, and accurate mark on the paper at 0 time. Make another small, thin, and accurate, mark at 4:30 ...
... 1) Take a sheet of paper and line up the left edge with the vertical axis (time). Be sure that most of the paper is hanging down below the graph. This is important. 2) Make a small, thin, and accurate mark on the paper at 0 time. Make another small, thin, and accurate, mark at 4:30 ...
Footwall uplift during normal faulting
... Abstract: In recent years, studies of major normal faults in actively extending regions (Aegean, Basin and Range) have documented the vertical motions associated with normal faulting. In addition to the expected subsidence of the hanging wall, it has been found that uplift of the footwall occurs dur ...
... Abstract: In recent years, studies of major normal faults in actively extending regions (Aegean, Basin and Range) have documented the vertical motions associated with normal faulting. In addition to the expected subsidence of the hanging wall, it has been found that uplift of the footwall occurs dur ...
Asian quake even more powerful
... University. And they have assigned the temblor an intensity of magnitude-9.3 -- 2.5 times greater than initial reports, which estimated it at approximately 9.0. Their research, along with another study by Chinese scientists, appears in today's edition of the British science journal Nature. They are ...
... University. And they have assigned the temblor an intensity of magnitude-9.3 -- 2.5 times greater than initial reports, which estimated it at approximately 9.0. Their research, along with another study by Chinese scientists, appears in today's edition of the British science journal Nature. They are ...
Additional Teaching Materials NEXT PAGE
... Materials—Graham crackers, fruit roll-up, water, frosting, wax paper, plastic knife, overheads Objectives—Explore how the tectonic plates (lithosphere) ride atop the asthenosphere; and ...
... Materials—Graham crackers, fruit roll-up, water, frosting, wax paper, plastic knife, overheads Objectives—Explore how the tectonic plates (lithosphere) ride atop the asthenosphere; and ...
Packet #9
... _ cc. What is the t minimum m number of seismograp phic stations needed to lo ocate the ep picenter of a an earthqua ake? ...
... _ cc. What is the t minimum m number of seismograp phic stations needed to lo ocate the ep picenter of a an earthqua ake? ...
EARTHQUAKES
... frequency (occurrence) of earthquakes at those locations. Additionally, stronger earthquakes are more likely to occur along active plate boundaries. Strong earthquakes are more common at transform and convergent plate boundaries. The San Andreas fault in California is an example of an active transfo ...
... frequency (occurrence) of earthquakes at those locations. Additionally, stronger earthquakes are more likely to occur along active plate boundaries. Strong earthquakes are more common at transform and convergent plate boundaries. The San Andreas fault in California is an example of an active transfo ...
Earthquake
An earthquake (also known as a quake, tremor or temblor) is the perceptible shaking of the surface of the Earth, which can be violent enough to destroy major buildings and kill thousands of people. The severity of the shaking can range from barely felt to violent enough to toss people around. Earthquakes have destroyed whole cities. They result from the sudden release of energy in the Earth's crust that creates seismic waves. The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time.Earthquakes are measured using observations from seismometers. The moment magnitude is the most common scale on which earthquakes larger than approximately 5 are reported for the entire globe. The more numerous earthquakes smaller than magnitude 5 reported by national seismological observatories are measured mostly on the local magnitude scale, also referred to as the Richter magnitude scale. These two scales are numerically similar over their range of validity. Magnitude 3 or lower earthquakes are mostly almost imperceptible or weak and magnitude 7 and over potentially cause serious damage over larger areas, depending on their depth. The largest earthquakes in historic times have been of magnitude slightly over 9, although there is no limit to the possible magnitude. The most recent large earthquake of magnitude 9.0 or larger was a 9.0 magnitude earthquake in Japan in 2011 (as of March 2014), and it was the largest Japanese earthquake since records began. Intensity of shaking is measured on the modified Mercalli scale. The shallower an earthquake, the more damage to structures it causes, all else being equal.At the Earth's surface, earthquakes manifest themselves by shaking and sometimes displacement of the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes can also trigger landslides, and occasionally volcanic activity.In its most general sense, the word earthquake is used to describe any seismic event — whether natural or caused by humans — that generates seismic waves. Earthquakes are caused mostly by rupture of geological faults, but also by other events such as volcanic activity, landslides, mine blasts, and nuclear tests. An earthquake's point of initial rupture is called its focus or hypocenter. The epicenter is the point at ground level directly above the hypocenter.