Relief Inversion

Inverted relief, inverted topography, or topographic inversion refers to landscape features that have reversed their elevation relative to other features. It most often occurs when low areas of a landscape become filled with lava or sediment that hardens into material that is more resistant to erosion than the material that surrounds it. ''Differential erosion'' then removes the less resistant surrounding material, leaving behind the younger resistant material, which may then appear as a ridge where previously there was a valley. Terms such as "inverted valley" or "inverted channel" are used to describe such features.Pain, C.F., and C.D. Ollier, 1995, ''Inversion of relief - a component of landscape evolution.'' Geomorphology. 12(2):151-165. Inverted relief has been observed on the surfaces of other planets as well as on Earth. For example, well-documented inverted topographies have been discovered on Mars.Pain, C.F., J.D.A. Clarke, and M. Thomas, 2007, ''Inversion of relief on Mars.'' Icarus. 190(2):478–491.

Formation

Several processes can cause the floor of a depression to become more resistant to erosion than its surrounding slopes and uplands:
*First, coarse-grained sediment, such as gravel, accumulates in the depression, i.e., a stream valley or lake basin. Next, wind erosion removes fine-grained sediments in areas adjacent to the depression. This leaves behind the more resistant coarse-grained sediments as a hill or ridge, while the channel switches to a lower lying area.
*A fluvial valley might fill with volcanic material such as lava or welded tuff pouring into it. This would resist erosion while the surrounding surface is eroded away to create a ridge.
* Cementation of underlying sediments by minerals dissolved in water may occur in a depression. On Earth, this often happens in stream valleys as the result of the formation of duricrusts, i.e., silcrete or ferricrete, by pedogenesis. Minerals for cementation can come from groundwater. It is thought that a low point like a valley focuses groundflow, so more water and cements move into it, and this results in a greater degree of cementation. Again, the cemented sediments would resist erosion while the surrounding terrain is eroded away to create a ridge or hill.
*Erosion of the resistant upper strata of the anticlines of a folded region, exposing less resistant underlying strata, which then erode relatively rapidly leaving the syncline as the top of a mesa or ridge.

An example

A classic example of inverted relief is Table Mountain, Tuolumne County, California. Multiple lava flows filled an ancient fluvial valley that cut westward through the central Sierra Nevada range to the Central Valley about 10.5 million years ago. These Miocene lava flows filled this ancient river valley with a thick sequence of potassium-rich trachyandesite lavas that are significantly more resistant to erosion than the Mesozoic siltstone and other rock in which the valley was cut. Thus, subsequent differential erosion left these volcanic rocks as a sinuous ridge, which now stands well above landscape underlain by more deeply eroded Mesozoic rocks.Gornya, C., C. Busbya, C.J. Pluhar, J. Hagana and K. Putirkab, 2009, ''An in-depth look at distal Sierra Nevada palaeochannel fill: drill cores through the Table Mountain Latite near Knights Ferry.'' International Geology Review. 51(9–11):824–842.

Another example is Table Mountain, Cape Town, where the original high ridges of resistant quartzitic sandstone of the Cape Fold Belt were eroded away first, exposing less resistant rock, which eroded faster, leaving the original valley bottom at the top of the residual mountain.

On Mars

Inverted relief in the form of sinuous and meandering ridges, which are indicative of ancient, inverted fluvial channels, is argued to be evidence of water channels on the Martian surface in the past.HiRISE, 2010a
''Inverted Channels North of Juventae Chasma (PSP_006770_1760).''
Operations Center, Department of Planetary Sciences, Lunar and Planetary Laboratory, Tucson, Arizona.Williams, R.M.E., T.C. Chidsey, Jr., and D.E. Eby, D.E., 2007, ''Exhumed paleochannels in central Utah - analogs for raised curvilinear features on Mars'', in G.C. Willis M.D. Hylland, D.L. Clark, and T.C. Chidsey, Jr., eds., pp. 220-235, Central Utah - diverse geology of a dynamic landscape. Publication 36, Utah Geological Association, Salt Lake City, Utah. An example is Miyamoto Crater, which was proposed in 2010 as a potential location to be searched for evidence of life on Mars.Newsom, H.E., N.L. Lanza, A.M. Ollila, S.M. Wiseman, T.L. Roush, G.A. Marzo, L.L. Tornabene, C.H. Okubo, M.M. Osterloo, V.E. Hamilton, and L.S. Crumpler, 2010, ''Inverted channel deposits on the floor of Miyamoto crater, Mars.'' Icarus. 205(1):64-72.

Other examples are shown in the photographs below.

Inverted terrain in Aeolis quadrangle

Image:Ridge in crater in Terra Sirenum.JPG, CTX image of craters in Aeolis quadrangle with black box in the large crater at lower right showing location of next image.
Image:Crater ridge in Aeolis.JPG, Image from previous photo of a curved ridge that may be an old stream that has become inverted. Illumination is from the NW. Image taken with HiRISE under the HiWish program.
Image:Meandering Ridges.JPG, Meandering Ridges that are probably inverted stream channels. Illumination is from the NW. Image taken with HiRISE.
Image:Sinuous Ridges in Medusae Formation.jpg, Sinuous Ridges within a branching fan in lower member of Medusae Fossae Formation,Grotzinger, J. and R. Milliken (eds.) 2012. Sedimentary Geology of Mars. SEPM as seen by HiRISE. Illumination is from the NW.

Inverted terrain in Syrtis Major quadrangle

Image:Inverted Streams in Juventae Chasma.jpg, Inverted Streams near Juventae Chasma, Syrtis Major quadrangle, as seen by Mars Global Surveyor. These streams begin at the top of a ridge then run together.
Image:Juventae Chasma Inverted Channels.JPG, Inverted Channels near Juventae Chasma, as seen by HiRISE. Channels were once regular stream channels. Image in Coprates quadrangle. Scale bar is 500 meters long.
Image:Inverted Channel 012435.jpg, Inverted Channel with many branches in Syrtis Major quadrangle.
Image:Antoniadi Crater Stream Channels.JPG, Inverted Stream Channels in Antoniadi Crater, as seen by HiRISE.

Inverted terrain in Margaritifer Sinus quadrangle

Image:Miyamoto Crater.JPG, Inverted Channel in Miyamoto Crater, Margaritifer Sinus quadrangle, as seen by HiRISE. Illumination is from the NW. The scale bar is 500 meters long.
Image:Inverted terrain context image.JPG, CTX context image for next image that was taken with HiRISE. Note long ridge going across image is probably an old stream. Box indicates area for HiRISE image.
Image:Inverted terrain in Parana Valles.JPG, Example of inverted terrain in Parana Valles region, as seen by HiRISE under the HiWish program. Illumination is from the NW.

Inverted terrain in Amazonis quadrangle

Image:ESP_024997ridges.jpg, Possible inverted stream channels, Amazonis quadrangle, as seen by HiRISE under HiWish program. The ridges were probably once stream valleys that have become full of sediment and cemented. So, they became hardened against erosion which removed surrounding material. Illumination is from the left (west).

References

External links

Everything2.com: Topographic Inversion
* ttps://archive.today/20130128111546/http://www.marstoday.com/news/viewsr.html?pid=21125 MarsToday.com: NASA Mars Picture of the Day: Inverted channelsbr>NASA: Inverted Topography, Patagonia, Argentina


*[https://web.archive.org/web/20080920225724/http://seis.natsci.csulb.edu/deptweb/SkinnyCalSites/bigpictext/TableMtn.html California State University Department of Geological Sciences: View of table mountain on eastern edge of the Sierra Nevada]

{{Geography of Mars, geology

Planetary geology
Surface features of Mars
Geomorphology
Mountain geomorphology
Erosion landforms