Geomorphology of Uluṟu

Posted on June 9, 2010 - Filed Under General

Oz! Uluru_sunset I came across an article discussing how Uluru (Maybe we can see that another visit?) came into form.
He hypothesizes that the relief of the ancestral Uluṟu was brought into existence by an initial cataclysmic depositional marine transgression and a subsequent erosional regression. Following this event, perhaps only tens of years, or maybe hundreds of years later, huge amounts of precipitation began to weather the newly formed and fresh relief, leaving a record of vast holes, ribs, and numerous other features found all over Uluṟu’s surface. As the precipitation continued, a huge inland lake formed and filled the area to a depth of tens of meters. Water sapping eventually caused the arkose to weather at and around a linear horizon 35 m above ground level, producing huge open-mouthed caves. As the process of equilibrium began to set in, a more permanent lake depth of around 3–6 m was established. Since the area all around Uluṟu is quite flat, potential energy in the form of large waves easily etch out the flared, concave-out slopes in the same manner as the flared slopes found at Fort Rock (Oregon). Wave attack is also responsible for the undermining of rock at Uluṟu’s base and may have been a catalyst for the wave-like features themselves. At a later stage still, the climate changed so dramatically, that the once humid, tropical climate of central Australia became a dry arid desert with limited rainfall. As a result, the lake eventually dried up, but not without leaving its permanent reminder both on the face of Uluṟu, and under the ground in terms of huge clay deposits.
Read more how he came to this conclusion, HERE

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