A wine fault or defect is an unpleasant characteristic of a wine often resulting from poor winemaking practices or storage conditions, and leading to wine spoilage. Many of the compounds that cause wine faults are already naturally present in wine but at insufficient concentrations to adversely affect it. In fact, depending on perception, these concentrations may impart positive characters to the wine. However, when the concentration of these compounds greatly exceeds the sensory threshold, they replace or obscure the flavors and aromas that the wine should be expressing (or that the winemaker wants the wine to express). Ultimately the quality of the wine is reduced, making it less appealing and sometimes undrinkable.
There are many causes for the perception in wine faults, including poor hygiene at the winery, excessive and/or insufficient exposure of the wine to oxygen, excessive or insufficient exposure of the wine to sulphur, overextended maceration of the wine either pre- or post-fermentation, faulty fining, filtering and stabilization of the wine, the use of dirty oak barrels, over-extended barrel aging and the use of poor quality corks. Outside of the winery, other factors within the control of the retailer or end user of the wine can contribute to the perception of flaws in the wine. These include poor storage of the wine that exposes it to excessive heat and temperature fluctuations as well as the use of dirty stemware during wine tasting that can introduce materials or aromas to what was previously a clean and fault-free wine.
Ansel Roth, a writer and cult specialist, fraudulently uses an expired voucher to pay for a meal at a hotel restaurant and is forcibly removed after refusing to pay. The manager of the hotel tells Roth that his speaking engagement is almost ready, and Roth steals towels and batteries as he checks out. His presentation on cults is interrupted by a heckler, who proceeds to beat him up for his involvement in the suicide of a troubled woman, the man's sister, who had been involved with a cult. Evelyn and Paul approach Roth and request an autographed copy of his book for their daughter, Claire, who they explain has become involved in a mysterious cult. Roth declines to become involved.
Faults Official Trailer 1 (2015) - Mary Elizabeth Winstead Movie HD
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Faults Official Trailer 1 (2015) - Mary Elizabeth Winstead Movie HD
Claire (Mary Elizabeth Winstead) is under the grip of a mysterious cult called Faults. Desperate to be reunited with their daughter, Claire’s parents set out to recruit Ansel Roth (Leland Orser), one of the world’s foremost authorities on cults and mind control. But Ansel’s specialty, deprogramming cult members and returning them to their families, is not an exact science, and a series of financial setbacks has left him in debt to his manager. Ansel warns Claire’s parents that his deprogramm...
published: 05 Feb 2015
Types of Faults in Geology
Types of Faults in Geology explained and animated.
In this video, I cover strike-slip fault, normal fault and reverse fault.
published: 12 Jan 2020
Types of Faults
published: 01 Aug 2016
Lecture 4: Faults and folds—models of deformation
Dr. Robert Butler, University of Portland, discusses Faults and Folds.
More into at:
http://www.iris.edu/hq/programs/education_and_outreach/aotm/2
published: 18 Nov 2008
Classification of Faults
In this video we introduce viewers to two terms they will need to understand to classify faults. We define the terms strike and dip in relation of everyday inclined surfaces including sloping brick surfaces and dumpster panels. Next we introduce you to the hanging wall and footwall of faults and provide a brief assessment to allow you to practice using the terms. We apply all four of these new terms to classify dip-slip and strike-slip faults. We end by shaking up a Lego geologist during fault movement and by asking you to interpret three examples of strike-slip faults.
Visit our blog for free assessment questions about the content in this video: https://geosciencevideos.wordpress.com
published: 15 Oct 2014
Active or Inactive Faults | Animation
What are Active and Inactive Faults?
For our discussion continuation about the series of Cracks on the Earth’s Surface, after learning the different types of faults, we will distinguish today if these faults are Active or Inactive faults.
Did you know that history showed that 90 % of the world’s largest earthquakes happen in the Pacific Ring of Fire? Yes, you heard it right. This is the world’s greatest earthquake zone found along the rim of the pacific ocean’s continental plate. This zone extends from Chile to South America’s coast, then through Central America to Mexico, plus the west coast of the US, then southern Alaska, and then through Japan, the Philippines, New Guinea, and New Zealand.
These earthquakes occur in the Pacific Ring of fire because of the active movement of faults a...
www.iris.edu/earthquake
This was created using excerpts from the longer animation called, “Earthquake Faults, Plate Boundaries, & Stress” [to be released September 2019; STAY TUNED!!]
A fault is a rock fracture where the two sides have been displaced relative to each other. Faults are categorized into three general groups based on the sense of slip or movement.
Normal fault—the block above the inclined fault moves down relative to the block below the fault. This fault motion is caused by tensional forces and results in extension. [Other names: normal-slip fault, tensional fault or gravity fault] Examples include Basin & Range faults.
Reverse fault—the block above the inclined fault moves up relative to the block below the fault. This fault motion is caused by compressional forces and re...
published: 10 Sep 2019
Flying a small airplane over the San Andreas fault
One of the largest earthquakes in United States history happened here in 1857. Fly a small airplane over the San Andreas fault and learn about one of the most infamous earthquake faults in the world. Follow along in my Grumman Tiger as we explore the Carrizo Plain and see from a unique perspective how this deadly earthquake fault has changed over thousands of years. The 1857 Fort Tejon earthquake measured 7.9 on the richter scale. California is long overdue for another "Big One" from this massive fault.
Go to https://wolficornprints.com/ to order professionally printed, gallery-quality aerial prints from both this flight and other aerial flights.
Music in this video:
Discovery by Delnova
With some malice by Francesco Dandrea
Meteor by Roman P
Morning Sunbeams by Yehezkel Raz
Breathe by I...
published: 30 Jul 2020
Fault : Types and Characteristics |Geomorphology | Dr. Krishnanand
Link to E-book : https://mithilacraft.com/product/simplified-geomorphology-ebook/
In this video the various concepts related to the Faults: Types and Characteristics have been discussed ; which is part of World Physical Geography for UPSC - General Studies Paper-1, as well as beneficial for other geography students.
This video by Dr. Krishnanand, founder of TheGeoecolologist; is suitable and helpful for the UPSC/IAS aspirants and beginners as well.
Simplified explanation of the understanding of Faults: Types and Characteristics, for preparation of UPSC (general studies paper-1) has been made in this lecture.
#geography #faults #geomorphology
SUBSCRIBE to the YouTube channel THEGEOECOLOGIST, to get notification about our recent lecture uploads on Geography Optional for UPSC.
Foll...
published: 22 Sep 2020
Folds and Faults
For an introductory college-level earth sciences class: a review folds and faults found in Earth's crust: their causes, classification, and importance. Also reviews the various stresses that lead to the variety of deformation types. Includes definitions and modeling of reverse faults, normal faults, and strike-slip faults; anticlines, synclines, domes, and basins; and plastic, elastic, and brittle deformation.
**This video comes about 1/3 of the way through the semester, so there may be terms with which the audience is unfamiliar. For a full playlist, refer to the Geology playlist on the Earth Rocks! YouTube Channel.
Content within this video is based on information available in any standard introductory college geology textbook, such as Essentials of Geology -- Tarbuck and Lutgens -- Pe...
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Faults Official Trailer 1 (2015) - Mary Elizabeth Winstead Movie HD
Claire (Mary Elizabeth Winstead) is under the grip of a mysterious cult called Faults. Desperate to be reunited with their daughter, Claire’s parents set out to recruit Ansel Roth (Leland Orser), one of the world’s foremost authorities on cults and mind control. But Ansel’s specialty, deprogramming cult members and returning them to their families, is not an exact science, and a series of financial setbacks has left him in debt to his manager. Ansel warns Claire’s parents that his deprogramming methods are risky and expensive, but they agree to hire him to kidnap and deprogram their daughter. Claire quickly reveals herself to be a formidable challenge. Her belief is unshakeable, and her logic is undeniable. A battle of wits develops between the two as they delve deeper and deeper into each other’s minds.
Subscribe to TRAILERS: http://bit.ly/sxaw6h
Subscribe to COMING SOON: http://bit.ly/H2vZUn
Subscribe to INDIE & FILM FESTIVALS: http://bit.ly/1wbkfYg
Like us on FACEBOOK: http://goo.gl/dHs73
Follow us on TWITTER: http://bit.ly/1ghOWmt
Faults Official Trailer 1 (2015) - Mary Elizabeth Winstead Movie HD
Claire (Mary Elizabeth Winstead) is under the grip of a mysterious cult called Faults. Desperate to be reunited with their daughter, Claire’s parents set out to recruit Ansel Roth (Leland Orser), one of the world’s foremost authorities on cults and mind control. But Ansel’s specialty, deprogramming cult members and returning them to their families, is not an exact science, and a series of financial setbacks has left him in debt to his manager. Ansel warns Claire’s parents that his deprogramming methods are risky and expensive, but they agree to hire him to kidnap and deprogram their daughter. Claire quickly reveals herself to be a formidable challenge. Her belief is unshakeable, and her logic is undeniable. A battle of wits develops between the two as they delve deeper and deeper into each other’s minds.
In this video we introduce viewers to two terms they will need to understand to classify faults. We define the terms strike and dip in relation of everyday incl...
In this video we introduce viewers to two terms they will need to understand to classify faults. We define the terms strike and dip in relation of everyday inclined surfaces including sloping brick surfaces and dumpster panels. Next we introduce you to the hanging wall and footwall of faults and provide a brief assessment to allow you to practice using the terms. We apply all four of these new terms to classify dip-slip and strike-slip faults. We end by shaking up a Lego geologist during fault movement and by asking you to interpret three examples of strike-slip faults.
Visit our blog for free assessment questions about the content in this video: https://geosciencevideos.wordpress.com
In this video we introduce viewers to two terms they will need to understand to classify faults. We define the terms strike and dip in relation of everyday inclined surfaces including sloping brick surfaces and dumpster panels. Next we introduce you to the hanging wall and footwall of faults and provide a brief assessment to allow you to practice using the terms. We apply all four of these new terms to classify dip-slip and strike-slip faults. We end by shaking up a Lego geologist during fault movement and by asking you to interpret three examples of strike-slip faults.
Visit our blog for free assessment questions about the content in this video: https://geosciencevideos.wordpress.com
What are Active and Inactive Faults?
For our discussion continuation about the series of Cracks on the Earth’s Surface, after learning the different types of f...
What are Active and Inactive Faults?
For our discussion continuation about the series of Cracks on the Earth’s Surface, after learning the different types of faults, we will distinguish today if these faults are Active or Inactive faults.
Did you know that history showed that 90 % of the world’s largest earthquakes happen in the Pacific Ring of Fire? Yes, you heard it right. This is the world’s greatest earthquake zone found along the rim of the pacific ocean’s continental plate. This zone extends from Chile to South America’s coast, then through Central America to Mexico, plus the west coast of the US, then southern Alaska, and then through Japan, the Philippines, New Guinea, and New Zealand.
These earthquakes occur in the Pacific Ring of fire because of the active movement of faults around it. The plates in this region are constantly moving by the compressing, expanding, and sliding forces which resulted in the creation of numerous land formations like trenches, volcanoes, and mountains. This region has 75 percent of the world’s volcanoes which is more than 450 volcanoes.
These are just the products of active faults in a bigger picture. Yet, how are we going to identify whether a fault is an active fault or an inactive fault?
Simply, Active faults are faults that recently created a movement of the Earth’s crust over the historical period of 10,000 years. If a fault is classified as an active fault, it means that it could still potentially create minor or major earthquakes over the period of time.
Enjoy this video about Active and Inactive Faults.
#ActiveInactiveFaults #EarthPen #EducationalVideo
CONTACT US
Email: [email protected]
Facebook Page: https://www.facebook.com/EarthPen
Youtube Channel: https://www.youtube.com/channel/UCX1Hh7CvEc3RCUd4NRBWJMw
What are Active and Inactive Faults?
For our discussion continuation about the series of Cracks on the Earth’s Surface, after learning the different types of faults, we will distinguish today if these faults are Active or Inactive faults.
Did you know that history showed that 90 % of the world’s largest earthquakes happen in the Pacific Ring of Fire? Yes, you heard it right. This is the world’s greatest earthquake zone found along the rim of the pacific ocean’s continental plate. This zone extends from Chile to South America’s coast, then through Central America to Mexico, plus the west coast of the US, then southern Alaska, and then through Japan, the Philippines, New Guinea, and New Zealand.
These earthquakes occur in the Pacific Ring of fire because of the active movement of faults around it. The plates in this region are constantly moving by the compressing, expanding, and sliding forces which resulted in the creation of numerous land formations like trenches, volcanoes, and mountains. This region has 75 percent of the world’s volcanoes which is more than 450 volcanoes.
These are just the products of active faults in a bigger picture. Yet, how are we going to identify whether a fault is an active fault or an inactive fault?
Simply, Active faults are faults that recently created a movement of the Earth’s crust over the historical period of 10,000 years. If a fault is classified as an active fault, it means that it could still potentially create minor or major earthquakes over the period of time.
Enjoy this video about Active and Inactive Faults.
#ActiveInactiveFaults #EarthPen #EducationalVideo
CONTACT US
Email: [email protected]
Facebook Page: https://www.facebook.com/EarthPen
Youtube Channel: https://www.youtube.com/channel/UCX1Hh7CvEc3RCUd4NRBWJMw
www.iris.edu/earthquake
This was created using excerpts from the longer animation called, “Earthquake Faults, Plate Boundaries, & Stress” [to be released Septem...
www.iris.edu/earthquake
This was created using excerpts from the longer animation called, “Earthquake Faults, Plate Boundaries, & Stress” [to be released September 2019; STAY TUNED!!]
A fault is a rock fracture where the two sides have been displaced relative to each other. Faults are categorized into three general groups based on the sense of slip or movement.
Normal fault—the block above the inclined fault moves down relative to the block below the fault. This fault motion is caused by tensional forces and results in extension. [Other names: normal-slip fault, tensional fault or gravity fault] Examples include Basin & Range faults.
Reverse fault—the block above the inclined fault moves up relative to the block below the fault. This fault motion is caused by compressional forces and results in shortening. A reverse fault is called a thrust fault if the dip of the fault plane is small. [Other names: reverse-slip fault or compressional fault.] Examples include the Rocky Mountains and the Himalayan Mountains.
Strike-slip fault—movement of blocks along a fault is horizontal and the fault plane is nearly vertical. If the block on the far side of the fault moves to the left, as shown in this animation, the fault is called left-lateral (Figure 2). If it moves to the right, the fault is called right-lateral. The fault motion of a strike-slip fault is caused by shearing forces. [Other names: trans current fault, lateral fault, tear fault or wrench fault.] Examples include the San Andreas Fault, California; Anatolian Fault, Turkey.
Narrated by Dr. Wendy Bohon
Animated by Jenda Johnson, Earth Sciences Animated
www.iris.edu/earthquake
This was created using excerpts from the longer animation called, “Earthquake Faults, Plate Boundaries, & Stress” [to be released September 2019; STAY TUNED!!]
A fault is a rock fracture where the two sides have been displaced relative to each other. Faults are categorized into three general groups based on the sense of slip or movement.
Normal fault—the block above the inclined fault moves down relative to the block below the fault. This fault motion is caused by tensional forces and results in extension. [Other names: normal-slip fault, tensional fault or gravity fault] Examples include Basin & Range faults.
Reverse fault—the block above the inclined fault moves up relative to the block below the fault. This fault motion is caused by compressional forces and results in shortening. A reverse fault is called a thrust fault if the dip of the fault plane is small. [Other names: reverse-slip fault or compressional fault.] Examples include the Rocky Mountains and the Himalayan Mountains.
Strike-slip fault—movement of blocks along a fault is horizontal and the fault plane is nearly vertical. If the block on the far side of the fault moves to the left, as shown in this animation, the fault is called left-lateral (Figure 2). If it moves to the right, the fault is called right-lateral. The fault motion of a strike-slip fault is caused by shearing forces. [Other names: trans current fault, lateral fault, tear fault or wrench fault.] Examples include the San Andreas Fault, California; Anatolian Fault, Turkey.
Narrated by Dr. Wendy Bohon
Animated by Jenda Johnson, Earth Sciences Animated
One of the largest earthquakes in United States history happened here in 1857. Fly a small airplane over the San Andreas fault and learn about one of the most i...
One of the largest earthquakes in United States history happened here in 1857. Fly a small airplane over the San Andreas fault and learn about one of the most infamous earthquake faults in the world. Follow along in my Grumman Tiger as we explore the Carrizo Plain and see from a unique perspective how this deadly earthquake fault has changed over thousands of years. The 1857 Fort Tejon earthquake measured 7.9 on the richter scale. California is long overdue for another "Big One" from this massive fault.
Go to https://wolficornprints.com/ to order professionally printed, gallery-quality aerial prints from both this flight and other aerial flights.
Music in this video:
Discovery by Delnova
With some malice by Francesco Dandrea
Meteor by Roman P
Morning Sunbeams by Yehezkel Raz
Breathe by Ian Post
One of the largest earthquakes in United States history happened here in 1857. Fly a small airplane over the San Andreas fault and learn about one of the most infamous earthquake faults in the world. Follow along in my Grumman Tiger as we explore the Carrizo Plain and see from a unique perspective how this deadly earthquake fault has changed over thousands of years. The 1857 Fort Tejon earthquake measured 7.9 on the richter scale. California is long overdue for another "Big One" from this massive fault.
Go to https://wolficornprints.com/ to order professionally printed, gallery-quality aerial prints from both this flight and other aerial flights.
Music in this video:
Discovery by Delnova
With some malice by Francesco Dandrea
Meteor by Roman P
Morning Sunbeams by Yehezkel Raz
Breathe by Ian Post
Link to E-book : https://mithilacraft.com/product/simplified-geomorphology-ebook/
In this video the various concepts related to the Faults: Types and Characte...
Link to E-book : https://mithilacraft.com/product/simplified-geomorphology-ebook/
In this video the various concepts related to the Faults: Types and Characteristics have been discussed ; which is part of World Physical Geography for UPSC - General Studies Paper-1, as well as beneficial for other geography students.
This video by Dr. Krishnanand, founder of TheGeoecolologist; is suitable and helpful for the UPSC/IAS aspirants and beginners as well.
Simplified explanation of the understanding of Faults: Types and Characteristics, for preparation of UPSC (general studies paper-1) has been made in this lecture.
#geography #faults #geomorphology
SUBSCRIBE to the YouTube channel THEGEOECOLOGIST, to get notification about our recent lecture uploads on Geography Optional for UPSC.
Follow us on the following links for the latest updates :
Email: [email protected]
Visit our Website: https://thegeoecologist.com/
Follow us on Instagram @: https://www.instagram.com/thegeoecolo...
ALL RIGHTS RESERVED.
Link to E-book : https://mithilacraft.com/product/simplified-geomorphology-ebook/
In this video the various concepts related to the Faults: Types and Characteristics have been discussed ; which is part of World Physical Geography for UPSC - General Studies Paper-1, as well as beneficial for other geography students.
This video by Dr. Krishnanand, founder of TheGeoecolologist; is suitable and helpful for the UPSC/IAS aspirants and beginners as well.
Simplified explanation of the understanding of Faults: Types and Characteristics, for preparation of UPSC (general studies paper-1) has been made in this lecture.
#geography #faults #geomorphology
SUBSCRIBE to the YouTube channel THEGEOECOLOGIST, to get notification about our recent lecture uploads on Geography Optional for UPSC.
Follow us on the following links for the latest updates :
Email: [email protected]
Visit our Website: https://thegeoecologist.com/
Follow us on Instagram @: https://www.instagram.com/thegeoecolo...
ALL RIGHTS RESERVED.
For an introductory college-level earth sciences class: a review folds and faults found in Earth's crust: their causes, classification, and importance. Also rev...
For an introductory college-level earth sciences class: a review folds and faults found in Earth's crust: their causes, classification, and importance. Also reviews the various stresses that lead to the variety of deformation types. Includes definitions and modeling of reverse faults, normal faults, and strike-slip faults; anticlines, synclines, domes, and basins; and plastic, elastic, and brittle deformation.
**This video comes about 1/3 of the way through the semester, so there may be terms with which the audience is unfamiliar. For a full playlist, refer to the Geology playlist on the Earth Rocks! YouTube Channel.
Content within this video is based on information available in any standard introductory college geology textbook, such as Essentials of Geology -- Tarbuck and Lutgens -- Pearson Publishing.
If you are an earth science enthusiast and would like to support our ongoing video development and engage with us behind the scenes...
Or if you are a student and would like access to interactive lessons built around these videos...
you can do so by JOINING the Earth Rocks! YouTube Channel:
https://www.youtube.com/channel/UCBEwiHo718rNAekZrqjjDjQ/join.
Thank you!
For an introductory college-level earth sciences class: a review folds and faults found in Earth's crust: their causes, classification, and importance. Also reviews the various stresses that lead to the variety of deformation types. Includes definitions and modeling of reverse faults, normal faults, and strike-slip faults; anticlines, synclines, domes, and basins; and plastic, elastic, and brittle deformation.
**This video comes about 1/3 of the way through the semester, so there may be terms with which the audience is unfamiliar. For a full playlist, refer to the Geology playlist on the Earth Rocks! YouTube Channel.
Content within this video is based on information available in any standard introductory college geology textbook, such as Essentials of Geology -- Tarbuck and Lutgens -- Pearson Publishing.
If you are an earth science enthusiast and would like to support our ongoing video development and engage with us behind the scenes...
Or if you are a student and would like access to interactive lessons built around these videos...
you can do so by JOINING the Earth Rocks! YouTube Channel:
https://www.youtube.com/channel/UCBEwiHo718rNAekZrqjjDjQ/join.
Thank you!
Subscribe to TRAILERS: http://bit.ly/sxaw6h
Subscribe to COMING SOON: http://bit.ly/H2vZUn
Subscribe to INDIE & FILM FESTIVALS: http://bit.ly/1wbkfYg
Like us on FACEBOOK: http://goo.gl/dHs73
Follow us on TWITTER: http://bit.ly/1ghOWmt
Faults Official Trailer 1 (2015) - Mary Elizabeth Winstead Movie HD
Claire (Mary Elizabeth Winstead) is under the grip of a mysterious cult called Faults. Desperate to be reunited with their daughter, Claire’s parents set out to recruit Ansel Roth (Leland Orser), one of the world’s foremost authorities on cults and mind control. But Ansel’s specialty, deprogramming cult members and returning them to their families, is not an exact science, and a series of financial setbacks has left him in debt to his manager. Ansel warns Claire’s parents that his deprogramming methods are risky and expensive, but they agree to hire him to kidnap and deprogram their daughter. Claire quickly reveals herself to be a formidable challenge. Her belief is unshakeable, and her logic is undeniable. A battle of wits develops between the two as they delve deeper and deeper into each other’s minds.
In this video we introduce viewers to two terms they will need to understand to classify faults. We define the terms strike and dip in relation of everyday inclined surfaces including sloping brick surfaces and dumpster panels. Next we introduce you to the hanging wall and footwall of faults and provide a brief assessment to allow you to practice using the terms. We apply all four of these new terms to classify dip-slip and strike-slip faults. We end by shaking up a Lego geologist during fault movement and by asking you to interpret three examples of strike-slip faults.
Visit our blog for free assessment questions about the content in this video: https://geosciencevideos.wordpress.com
What are Active and Inactive Faults?
For our discussion continuation about the series of Cracks on the Earth’s Surface, after learning the different types of faults, we will distinguish today if these faults are Active or Inactive faults.
Did you know that history showed that 90 % of the world’s largest earthquakes happen in the Pacific Ring of Fire? Yes, you heard it right. This is the world’s greatest earthquake zone found along the rim of the pacific ocean’s continental plate. This zone extends from Chile to South America’s coast, then through Central America to Mexico, plus the west coast of the US, then southern Alaska, and then through Japan, the Philippines, New Guinea, and New Zealand.
These earthquakes occur in the Pacific Ring of fire because of the active movement of faults around it. The plates in this region are constantly moving by the compressing, expanding, and sliding forces which resulted in the creation of numerous land formations like trenches, volcanoes, and mountains. This region has 75 percent of the world’s volcanoes which is more than 450 volcanoes.
These are just the products of active faults in a bigger picture. Yet, how are we going to identify whether a fault is an active fault or an inactive fault?
Simply, Active faults are faults that recently created a movement of the Earth’s crust over the historical period of 10,000 years. If a fault is classified as an active fault, it means that it could still potentially create minor or major earthquakes over the period of time.
Enjoy this video about Active and Inactive Faults.
#ActiveInactiveFaults #EarthPen #EducationalVideo
CONTACT US
Email: [email protected]
Facebook Page: https://www.facebook.com/EarthPen
Youtube Channel: https://www.youtube.com/channel/UCX1Hh7CvEc3RCUd4NRBWJMw
www.iris.edu/earthquake
This was created using excerpts from the longer animation called, “Earthquake Faults, Plate Boundaries, & Stress” [to be released September 2019; STAY TUNED!!]
A fault is a rock fracture where the two sides have been displaced relative to each other. Faults are categorized into three general groups based on the sense of slip or movement.
Normal fault—the block above the inclined fault moves down relative to the block below the fault. This fault motion is caused by tensional forces and results in extension. [Other names: normal-slip fault, tensional fault or gravity fault] Examples include Basin & Range faults.
Reverse fault—the block above the inclined fault moves up relative to the block below the fault. This fault motion is caused by compressional forces and results in shortening. A reverse fault is called a thrust fault if the dip of the fault plane is small. [Other names: reverse-slip fault or compressional fault.] Examples include the Rocky Mountains and the Himalayan Mountains.
Strike-slip fault—movement of blocks along a fault is horizontal and the fault plane is nearly vertical. If the block on the far side of the fault moves to the left, as shown in this animation, the fault is called left-lateral (Figure 2). If it moves to the right, the fault is called right-lateral. The fault motion of a strike-slip fault is caused by shearing forces. [Other names: trans current fault, lateral fault, tear fault or wrench fault.] Examples include the San Andreas Fault, California; Anatolian Fault, Turkey.
Narrated by Dr. Wendy Bohon
Animated by Jenda Johnson, Earth Sciences Animated
One of the largest earthquakes in United States history happened here in 1857. Fly a small airplane over the San Andreas fault and learn about one of the most infamous earthquake faults in the world. Follow along in my Grumman Tiger as we explore the Carrizo Plain and see from a unique perspective how this deadly earthquake fault has changed over thousands of years. The 1857 Fort Tejon earthquake measured 7.9 on the richter scale. California is long overdue for another "Big One" from this massive fault.
Go to https://wolficornprints.com/ to order professionally printed, gallery-quality aerial prints from both this flight and other aerial flights.
Music in this video:
Discovery by Delnova
With some malice by Francesco Dandrea
Meteor by Roman P
Morning Sunbeams by Yehezkel Raz
Breathe by Ian Post
Link to E-book : https://mithilacraft.com/product/simplified-geomorphology-ebook/
In this video the various concepts related to the Faults: Types and Characteristics have been discussed ; which is part of World Physical Geography for UPSC - General Studies Paper-1, as well as beneficial for other geography students.
This video by Dr. Krishnanand, founder of TheGeoecolologist; is suitable and helpful for the UPSC/IAS aspirants and beginners as well.
Simplified explanation of the understanding of Faults: Types and Characteristics, for preparation of UPSC (general studies paper-1) has been made in this lecture.
#geography #faults #geomorphology
SUBSCRIBE to the YouTube channel THEGEOECOLOGIST, to get notification about our recent lecture uploads on Geography Optional for UPSC.
Follow us on the following links for the latest updates :
Email: [email protected]
Visit our Website: https://thegeoecologist.com/
Follow us on Instagram @: https://www.instagram.com/thegeoecolo...
ALL RIGHTS RESERVED.
For an introductory college-level earth sciences class: a review folds and faults found in Earth's crust: their causes, classification, and importance. Also reviews the various stresses that lead to the variety of deformation types. Includes definitions and modeling of reverse faults, normal faults, and strike-slip faults; anticlines, synclines, domes, and basins; and plastic, elastic, and brittle deformation.
**This video comes about 1/3 of the way through the semester, so there may be terms with which the audience is unfamiliar. For a full playlist, refer to the Geology playlist on the Earth Rocks! YouTube Channel.
Content within this video is based on information available in any standard introductory college geology textbook, such as Essentials of Geology -- Tarbuck and Lutgens -- Pearson Publishing.
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