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  2. Fault (geology) - Wikipedia

    en.wikipedia.org/wiki/Fault_(geology)

    [21] [22] Thrust faults typically form ramps, flats and fault-bend (hanging wall and footwall) folds. A section of a hanging wall or foot wall where a thrust fault formed along a relatively weak bedding plane is known as a flat and a section where the thrust fault cut upward through the stratigraphic sequence is known as a ramp. [23]

  3. Lacustrine deposits - Wikipedia

    en.wikipedia.org/wiki/Lacustrine_deposits

    Lacustrine deposits are sedimentary rock formations which formed in the bottom of ancient lakes. [1] A common characteristic of lacustrine deposits is that a river or stream channel has carried sediment into the basin. Lacustrine deposits form in all lake types including rift graben lakes, oxbow lakes, glacial lakes, and crater lakes ...

  4. Lake - Wikipedia

    en.wikipedia.org/wiki/Lake

    Tectonic lakes are lakes formed by the deformation and resulting lateral and vertical movements of the Earth's crust. These movements include faulting, tilting, folding, and warping. Some of the largest lakes on Earth are rift lakes occupying rift valleys, e.g. Central African Rift lakes and Lake Baikal.

  5. Basin and range topography - Wikipedia

    en.wikipedia.org/wiki/Basin_and_range_topography

    This results in block faulting, where the blocks of rock between the normal faults either subside, uplift, or tilt. The movement of these blocks results in the alternating valleys and mountains. As the crust thins, it also allows heat from the mantle to more easily melt rock and form magma, resulting in increased volcanic activity. [3]

  6. Rift lake - Wikipedia

    en.wikipedia.org/wiki/Rift_lake

    Faulted southeastern side of Svyatoy Nos peninsula, Lake Baikal – active faulting shown by faceted spurs. Artificial rendering of the Albertine Rift showing four of its rift lakes A rift lake is a lake formed as a result of subsidence related to movement on faults within a rift zone, an area of extensional tectonics in the continental crust .

  7. Graben - Wikipedia

    en.wikipedia.org/wiki/Graben

    The exception is at any major offset in the bounding fault, where a relay ramp may provide an important sediment input point. Most of the sediment will enter the half-graben down the unfaulted hanging wall side (e.g., Lake Baikal). [4] Rima Ariadaeus on the Moon is thought to be a graben. The lack of erosion on the Moon makes its structure with ...

  8. Underground lake - Wikipedia

    en.wikipedia.org/wiki/Underground_lake

    Underground lake within Cross Cave in Slovenia, one of 22 such lakes. An underground lake (also known as a subterranean lake) is a lake underneath the surface of the Earth. . Most naturally occurring underground lakes are found in areas of karst topography, [1] [2] where limestone or other soluble rock has been weathered away, leaving a cave where water can flow and accumu

  9. Lake Turkana - Wikipedia

    en.wikipedia.org/wiki/Lake_Turkana

    The Lake Turkana drainage basin draws its waters mainly from Kenya Highlands and Ethiopian Highlands. A map of lake turkana. The basement rocks of the region have been dated by two analytical determinations to 522 and 510 million years ago (mya). No rift was in the offing at that time. A rift is signalled by volcanic activity through the ...