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Jordon Valley Landslide EarthCache

Hidden : 3/19/2024
Difficulty:
2 out of 5
Terrain:
2.5 out of 5

Size: Size:   other (other)

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Geocache Description:


BE CAREFUL

The posted coordinates should put you at a bench at the landslide overlook.  There is a fence between the bench and the landslide area.  There is a very steep and deep drop off on the other side of the fence.  THERE IS NO NEED TO CROSS THE FENCE

LANDSLIDE TYPES

The are 4 main types of landslides:

falls
topples
slides (rotational and translational)
flows

FALLS

Falls are landslides that involve the collapse of material from a cliff or steep slope. Falls usually involve a mixture of free fall through the air, bouncing or rolling. A fall-type landslide results in the collection of rock or debris near the base of a slope.

TOPPLES

Topple failures involve the forward rotation and movement of a mass of rock, earth or debris out of a slope. This kind of slope failure generally occurs around an axis (or point) at or near the base of the block of rock.

ROTATIONAL SLIDE

Rotational Slides are a slide in which the surface of rupture is curved concavely upward and the slide movement is roughly rotational about an axis that is parallel to the ground surface and transverse across the slide.

TRANSLATIONAL SLIDE

In a translational slide, the landslide mass moves along a roughly planar surface with little rotation or backward tilting

FLOW

Flows are landslides that involve the movement of material down a slope in the form of a fluid. Flows often leave behind a distinctive, upside-down funnel shaped deposit where the landslide material has stopped moving. There are different types of flows: mud, debris and rock.

BENT TREES

Trees tend to grow straight up. This is especially true in the forest when there is competition for light. If you look around the slope, you will see some bent trees. Trees with trunks that curve in one direction before eventually straightening out. This typically doesn't happen on flat ground, but on a slope, and the outward side of the bend always angles downhill. The reason for this is the movement of the soil. "Soil creep" is the gradual movement of the substrate downhill over time. It’s a slow process, but all the soil on a slope is moving. Importantly for trees, the soil moves more quickly on the surface than deeper down. Because of this, there’s more soil pushing the tree at ground level than below – and gradually, eventually, this tilts the tree. To compensate, trees will put on thicker growth – wider rings – on the downhill side, slowly changing the angle of the trunk to regain an upright posture. Eventually, the roots grow deep enough and strong enough that the soil can no longer tilt the tree. At this point, the growth will even out to correct the angle, and the curve straightens! You can even find trees that apparently overcorrected, and you get what looks like a very stretched-out S-shape before the tree goes fully vertical.

LOGGING REQUIREMENTS

In order to log this EarthCache, send me your answers to the following questions either through email or messaging from my profile page.

1: What type of landslide happened here?

2: Is it still sliding?

3: What do you see that supports your answer for #2?

4: Post a pic of you or a signature item with the overlook view in the background.

references

https://www.mtpr.org/

https://www.bgs.ac.uk/

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