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  2. Soil formation - Wikipedia

    en.wikipedia.org/wiki/Soil_formation

    Soil develops through a series of changes. [2] The starting point is weathering of freshly accumulated parent material.A variety of soil microbes (bacteria, archaea, fungi) feed on simple compounds released by weathering and produce organic acids and specialized proteins which contribute in turn to mineral weathering.

  3. Vishnu Basement Rocks - Wikipedia

    en.wikipedia.org/wiki/Vishnu_Basement_Rocks

    In the case of the unconformity between the Vishnu Basement Rocks and the Unkar Group, studies of the underlying Vishnu Basement Rocks indicate they were uplifted from a depth of about 25 km (16 mi) to a depth of about 10 km (6.2 mi), between 1.75 and 1.66 billion years ago, and from a depth of about 10 km (6.2 mi) to the weathered surface on ...

  4. Soil conservation - Wikipedia

    en.wikipedia.org/wiki/Soil_conservation

    The rows formed slow surface water run-off during rainstorms to prevent soil erosion and allow the water time to infiltrate into the soil. Soil conservation is the prevention of loss of the topmost layer of the soil from erosion or prevention of reduced fertility caused by over usage, acidification, salinization or other chemical soil contamination

  5. Wapma Thura–Southern Flinders Ranges National Park

    en.wikipedia.org/wiki/Wapma_Thura–Southern...

    The Napperby Block, formerly within Mount Remarkable Conservation Park, is a parcel of land of 16.72 km 2 (6.46 sq mi), located immediately east of the town of Napperby, about 4 km (2.5 mi) south of the Telowie Gorge Conservation Park and about 12 km (7.5 mi) north-east of the city of Port Pirie. Added in 1993, it is not contiguous with the ...

  6. Olduvai Gorge - Wikipedia

    en.wikipedia.org/wiki/Olduvai_Gorge

    The Olduvai Gorge Museum, located 5 km beyond the monument, is situated on the rim of the gorge at the junction of the main gorge and the side gorge. As one of the largest onsite museums in Africa, the museum provides educational exhibits related to the gorge and its long history.

  7. Todgha Gorge - Wikipedia

    en.wikipedia.org/wiki/Todgha_Gorge

    A well-maintained asphalt road leads up the valley from Tinerhir to the gorge. A concrete road continues up the valley, past the hotels at the mouth of the gorge all the way to the villages of Aït Hani, and Tamtatouchte. Thanks to its robust rock sides with many uneven surfaces, Todgha Gorge is popular among rock climbers. [2]

  8. Landslide - Wikipedia

    en.wikipedia.org/wiki/Landslide

    Debris slides and debris flows are usually shallow. Shallow landslides can often happen in areas that have slopes with high permeable soils on top of low permeable soils. The low permeable soil traps the water in the shallower soil generating high water pressures. As the top soil is filled with water, it can become unstable and slide downslope.

  9. Cheddar Gorge - Wikipedia

    en.wikipedia.org/wiki/Cheddar_Gorge

    Cheddar Gorge is a limestone gorge in the Mendip Hills, near the village of Cheddar, Somerset, England. The gorge is the site of the Cheddar show caves, where Britain's oldest complete human skeleton , Cheddar Man , estimated to be 9,000 years old, was found in 1903. [ 1 ]

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