Landslide – Fleetwood Mac. How to play 'Landslide' Font −1 +1. Watch our community members perform this song. Fleetwood Mac's Stevie Nicks and Lindsey Buckingham perform 'Landslide' live on stage.Subscribe to the Amex YouTube Channel: http://bit.ly/SubscribeAMEXAbout. Landslide Fleetwood Mac. This is one of my all-time favorite songs and this is onw of the first song. Which I learned the entire thing. It should by pretty accurate.

Landslide is a song written by Stevie Nicks and performed by her with Lindsey Buckingham on acoustic guitar for Fleetwood Mac 's self-titled 1975 album. Nicks wrote the song while visiting Aspen, Colorado at a time when considering whether to return to education or continue with music.

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from the album The Very Best Of Fleetwood Mac ·Copyright: Writer(s): Stevie Nicks Lyrics Terms of Use

I took my love, I took it down
I climbed a mountain and I turned around
And I saw my reflection in the snow covered hills
'Til the landslide brought me down

Oh, mirror in the sky
What is love?
Can the child within my heart rise above?
Can I sail through the changin' ocean tides?
Can I handle the seasons of my life?

Well, I've been afraid of changin'
'Cause I've built my life around you
But time makes you bolder
Even children get older
And I'm getting older too

Well, I've been afraid of changin'
'Cause I've built my life around you
But time makes you bolder
Even children get older
And I'm getting older too
Oh! I'm getting older too

Oh-oh, take my love, take it down
Oh-oh, climb a mountain and you turn around
And if you see my reflection in the snow covered hills
Well the landslide bring it down
And if you see my reflection in the snow covered hills
Well the landslide bring it down
The landslide bring it down

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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.

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.

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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 Os