Landslidefleetwood Mac
2021年7月23日Download here: http://gg.gg/vhi8u
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Stevie Nicks and Lindsey Buckingham wrote ’Landslide’ while living in Aspen, Colorado in 1973
*Add ’Landslide’ by Fleetwood Mac to your Rock Band™ song library. ’Landslide’ - Fleetwood Mac is currently not available.
*Live In Boston - Say You Will Tour.
*Landslide – Fleetwood Mac. How to play ’Landslide’ Font −1 +1. Watch our community members perform this song.
The song, ’Landslide’ is about her life in general at that time. Everything seemed to be coming down like a landslide. The Buckingham Nicks album had been dropped from Polydor. Stevie Nicks had gone back to being a waitress and a cleaning lady in order to pay the bills and allow Lindsey to work on their music. Stevie’s parents told her that if she wanted to go back to school, they’d support her.
In the lyrics, climbing the mountain and snow-covered hills refers to the Rocky Mountains that she was able to see from the window of the house that she and Lindsey were living in. She was unsure about making a change in the direction her life was going.
Download the latest drivers, firmware, and software for your HP PSC 1210 All-in-One Printer.This is HP’s official website that will help automatically detect and download the correct drivers free of cost for your HP Computing and Printing products for Windows and Mac operating system. Hp psc 1210 all-in-one driver download for macbeattree.
’Time makes you bolder, even children get older, I’m getting older too’ is an important part of the song. Stevie is realizing that she is getting older and that if her musical career doesn’t work out soon, she will have to make a change. Part of her struggle is that she isn’t sure how much longer she should wait before deciding that she has to move on. Within a year’s time, Lindsey Buckingham and Stevie Nicks had joined Fleetwood Mac and were on their way to musical success.The Chain
Tribute to Fleetwood Mac. Website by Sky High Social Media Kansas CitySky High Social Media Kansas City. You can go to you tube and hear Stevie Nicks tell you what Landslide means in her own words, but to sum up, it was 1974, and she was a waitress and absolutely sick of doing it, and she had no money, ’only enough to eat and put gas in the car,’ and the anxiety of constantly being on the brink like that was destroying her relationship.
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Add your own interpretation and discuss lyrics of this song:
Landslide Please select which sections you would like to print: While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Our editors will review what you’ve submitted and determine whether to revise the article. Join Britannica’s Publishing Partner Program and our community of experts to gain a global audience for your work! Articles from Britannica Encyclopedias for elementary and high school students.Xingmin MengGeographic Database Manager and Geographic Information Systems Analyst, Department of Geography, Royal Holloway, University of London, Egham, Surrey, U.K.Alternative Title: landslip
Landslide, also called landslip, the movement downslope of a mass of rock, debris, earth, or soil (soil being a mixture of earth and debris). Landslides occur when gravitational and other types of shear stresses within a slope exceed the shear strength (resistance to shearing) of the materials that form the slope.
Shear stresses can be built up within a slope by a number of processes. These include oversteepening of the base of the slope, such as by natural erosion or excavation, and loading of the slope, such as by an inflow of water, a rise in the groundwater table, or the accumulation of debris on the slope’s surface. Short-term stresses, such as those imposed by earthquakes and rainstorms, can likewise contribute to the activation of landslides. Landslides can also be activated by processes that weaken the shear strength of a slope’s material. Shear strength is dependent mainly on two factors: frictional strength, which is the resistance to movement between the slope material’s interacting constituent particles, and cohesive strength, which is the bonding between the particles. Coarse particles such as sand grains have high frictional strength but low cohesive strength, whereas the opposite is true for clays, which are composed of fine particles. Another factor that affects the shear strength of a slope-forming material is the spatial disposition of its constituent particles, referred to as the sediment fabric. Some materials with a loose, open sediment fabric will weaken if they are mechanically disturbed or flooded with water. An increase in water content, resulting from either natural causes or human activity, typically weakens sandy materials through the reduction of interparticle friction and weakens clays through the dissolution of interparticle cements, the hydration of clay minerals, and the elimination of interparticle (capillary) tension.Types of landslides
Landslides are generally classified by type of movement (slides, flows, spreads, topples, or falls) and type of material (rock, debris, or earth). Sometimes more than one type of movement occurs within a single landslide, and, because the temporal and spatial relationships of these movements are often complex, their analysis often requires detailed interpretation of both landforms and geological sections, or cores.
Rockslides and other types of slides involve the displacement of material along one or more discrete shearing surfaces. The sliding can extend downward and outward along a broadly planar surface (a translational slide), or it can be rotational along a concave-upward set of shear surfaces (a slump). A translational slide typically takes place along structural features, such as a bedding plane or the interface between resistant bedrock and weaker overlying material. If the overlying material moves as a single, little-deformed mass, it is called a block slide. A translational slide is sometimes called a mud slide when it occurs along gently sloping, discrete shear planes in fine-grained rocks (such as fissured clays) and the displaced mass is fluidized by an increase in pore water pressure. In a rotational slide the axis of rotation is roughly parallel to the contours of the slope. The movement near the head of the slide is largely downward, exposing a steep head scarp, and movement within the displaced mass takes place along internal slip planes, each tending to tilt backward. Over time, upslope ponding of water by such back-tilted blocks can enlarge the area of instability, so that a stable condition is reached only when the slope is reduced to a very low gradient. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe NowLandslide Fleetwood Nbsp Mac Demarco
A type of landslide in which the distribution of particle velocities resembles that of a viscous fluid is called a flow. The most important fluidizing agent is water, but trapped air is sometimes involved. Contact between the flowing mass and the underlying material can be distinct, or the contact can be one of diffuse shear. The difference between slides and flows is gradational, with variations in fluid content, mobility, and type of movement, and composite slide movement and flow movement are common.
A spread is the complex lateral movement of relatively coherent earth materials resting on a weaker substrate that is subject to liquefaction or plastic flow. Coherent blocks of material subside into the weaker substrate, and the slow downslope movement frequently extends long distances as a result of the retrogressive extension from the zone of origin, such as an eroding riverbank or coastline. Spreads occur as the result of liquefaction caused by water saturation or earthquake shock in such substrates as loess, a weakly cemented wind-lain silt.
Rotation of a mass of rock, debris, or earth outward from a steep slope face is called toppling. This type of movement can subsequently cause the mass to fall or slide.
Earth materials can become detached from a steep slope without significant shearing, fall freely under gravity, and land on a surface from which they bounce and fall farther. Falls of large volume can trap enough air to facilitate the very rapid flow of rock or debris, forming rock avalanches and debris avalanches, respectively. Entrapped snow and ice may also help mobilize such flows, but the unqualified term avalanche is generally used to refer only to an avalanche of snow. (Seeavalanche.) Triggered by earthquake shock or torrential rain in mountainous relief with steep gradients, a huge volume of avalanching rock or debris (of up to millions of metric tons) can reach a velocity of more than 50 metres (160 feet) per second and leave a long trail of destruction.Landslide Fleetwood Nbsp Mac DownloadQuick FactsLandslide Fleetwood Nbsp Mac Shortcutrelated topics
Download here: http://gg.gg/vhi8u
https://diarynote.indered.space
*Landslide Fleetwood Nbsp Mac Demarco
*Landslide Fleetwood Nbsp Mac Download
*Landslide Fleetwood Nbsp Mac ShortcutBack to song list
Stevie Nicks and Lindsey Buckingham wrote ’Landslide’ while living in Aspen, Colorado in 1973
*Add ’Landslide’ by Fleetwood Mac to your Rock Band™ song library. ’Landslide’ - Fleetwood Mac is currently not available.
*Live In Boston - Say You Will Tour.
*Landslide – Fleetwood Mac. How to play ’Landslide’ Font −1 +1. Watch our community members perform this song.
The song, ’Landslide’ is about her life in general at that time. Everything seemed to be coming down like a landslide. The Buckingham Nicks album had been dropped from Polydor. Stevie Nicks had gone back to being a waitress and a cleaning lady in order to pay the bills and allow Lindsey to work on their music. Stevie’s parents told her that if she wanted to go back to school, they’d support her.
In the lyrics, climbing the mountain and snow-covered hills refers to the Rocky Mountains that she was able to see from the window of the house that she and Lindsey were living in. She was unsure about making a change in the direction her life was going.
Download the latest drivers, firmware, and software for your HP PSC 1210 All-in-One Printer.This is HP’s official website that will help automatically detect and download the correct drivers free of cost for your HP Computing and Printing products for Windows and Mac operating system. Hp psc 1210 all-in-one driver download for macbeattree.
’Time makes you bolder, even children get older, I’m getting older too’ is an important part of the song. Stevie is realizing that she is getting older and that if her musical career doesn’t work out soon, she will have to make a change. Part of her struggle is that she isn’t sure how much longer she should wait before deciding that she has to move on. Within a year’s time, Lindsey Buckingham and Stevie Nicks had joined Fleetwood Mac and were on their way to musical success.The Chain
Tribute to Fleetwood Mac. Website by Sky High Social Media Kansas CitySky High Social Media Kansas City. You can go to you tube and hear Stevie Nicks tell you what Landslide means in her own words, but to sum up, it was 1974, and she was a waitress and absolutely sick of doing it, and she had no money, ’only enough to eat and put gas in the car,’ and the anxiety of constantly being on the brink like that was destroying her relationship.
Visit Music Banter - The Internet’s Top Music Community
Add your own interpretation and discuss lyrics of this song:
Landslide Please select which sections you would like to print: While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Our editors will review what you’ve submitted and determine whether to revise the article. Join Britannica’s Publishing Partner Program and our community of experts to gain a global audience for your work! Articles from Britannica Encyclopedias for elementary and high school students.Xingmin MengGeographic Database Manager and Geographic Information Systems Analyst, Department of Geography, Royal Holloway, University of London, Egham, Surrey, U.K.Alternative Title: landslip
Landslide, also called landslip, the movement downslope of a mass of rock, debris, earth, or soil (soil being a mixture of earth and debris). Landslides occur when gravitational and other types of shear stresses within a slope exceed the shear strength (resistance to shearing) of the materials that form the slope.
Shear stresses can be built up within a slope by a number of processes. These include oversteepening of the base of the slope, such as by natural erosion or excavation, and loading of the slope, such as by an inflow of water, a rise in the groundwater table, or the accumulation of debris on the slope’s surface. Short-term stresses, such as those imposed by earthquakes and rainstorms, can likewise contribute to the activation of landslides. Landslides can also be activated by processes that weaken the shear strength of a slope’s material. Shear strength is dependent mainly on two factors: frictional strength, which is the resistance to movement between the slope material’s interacting constituent particles, and cohesive strength, which is the bonding between the particles. Coarse particles such as sand grains have high frictional strength but low cohesive strength, whereas the opposite is true for clays, which are composed of fine particles. Another factor that affects the shear strength of a slope-forming material is the spatial disposition of its constituent particles, referred to as the sediment fabric. Some materials with a loose, open sediment fabric will weaken if they are mechanically disturbed or flooded with water. An increase in water content, resulting from either natural causes or human activity, typically weakens sandy materials through the reduction of interparticle friction and weakens clays through the dissolution of interparticle cements, the hydration of clay minerals, and the elimination of interparticle (capillary) tension.Types of landslides
Landslides are generally classified by type of movement (slides, flows, spreads, topples, or falls) and type of material (rock, debris, or earth). Sometimes more than one type of movement occurs within a single landslide, and, because the temporal and spatial relationships of these movements are often complex, their analysis often requires detailed interpretation of both landforms and geological sections, or cores.
Rockslides and other types of slides involve the displacement of material along one or more discrete shearing surfaces. The sliding can extend downward and outward along a broadly planar surface (a translational slide), or it can be rotational along a concave-upward set of shear surfaces (a slump). A translational slide typically takes place along structural features, such as a bedding plane or the interface between resistant bedrock and weaker overlying material. If the overlying material moves as a single, little-deformed mass, it is called a block slide. A translational slide is sometimes called a mud slide when it occurs along gently sloping, discrete shear planes in fine-grained rocks (such as fissured clays) and the displaced mass is fluidized by an increase in pore water pressure. In a rotational slide the axis of rotation is roughly parallel to the contours of the slope. The movement near the head of the slide is largely downward, exposing a steep head scarp, and movement within the displaced mass takes place along internal slip planes, each tending to tilt backward. Over time, upslope ponding of water by such back-tilted blocks can enlarge the area of instability, so that a stable condition is reached only when the slope is reduced to a very low gradient. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe NowLandslide Fleetwood Nbsp Mac Demarco
A type of landslide in which the distribution of particle velocities resembles that of a viscous fluid is called a flow. The most important fluidizing agent is water, but trapped air is sometimes involved. Contact between the flowing mass and the underlying material can be distinct, or the contact can be one of diffuse shear. The difference between slides and flows is gradational, with variations in fluid content, mobility, and type of movement, and composite slide movement and flow movement are common.
A spread is the complex lateral movement of relatively coherent earth materials resting on a weaker substrate that is subject to liquefaction or plastic flow. Coherent blocks of material subside into the weaker substrate, and the slow downslope movement frequently extends long distances as a result of the retrogressive extension from the zone of origin, such as an eroding riverbank or coastline. Spreads occur as the result of liquefaction caused by water saturation or earthquake shock in such substrates as loess, a weakly cemented wind-lain silt.
Rotation of a mass of rock, debris, or earth outward from a steep slope face is called toppling. This type of movement can subsequently cause the mass to fall or slide.
Earth materials can become detached from a steep slope without significant shearing, fall freely under gravity, and land on a surface from which they bounce and fall farther. Falls of large volume can trap enough air to facilitate the very rapid flow of rock or debris, forming rock avalanches and debris avalanches, respectively. Entrapped snow and ice may also help mobilize such flows, but the unqualified term avalanche is generally used to refer only to an avalanche of snow. (Seeavalanche.) Triggered by earthquake shock or torrential rain in mountainous relief with steep gradients, a huge volume of avalanching rock or debris (of up to millions of metric tons) can reach a velocity of more than 50 metres (160 feet) per second and leave a long trail of destruction.Landslide Fleetwood Nbsp Mac DownloadQuick FactsLandslide Fleetwood Nbsp Mac Shortcutrelated topics
Download here: http://gg.gg/vhi8u
https://diarynote.indered.space
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