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Characterisation of potholes formed on bedrock sandstones at Loei Dun, Phetchabun Geopark, Thailand

Singtuen Vimoltip, Junjuer Thitaree

Geologos

2022

Vol. 28, No. 1

39--50

Phetchabun National Geopark comprises varied geosites; one of the fluvial bedrock landforms distinguished here is Loei Dun. This shows many potholes in Mesozoic sandstone of the Nam Phong Formation (Khorat Group). A genetic study of the occurrence of the Loei Dun potholes lends it a higher geoheritage value. For the present study we did fieldwork and carried out petrographical and geotechnical analyses so as to classify and characterise the potholes and consider geotourism potentials. Petrographically, the bedrock sandstone is a lithic arenite which consists of 82-96 percent very fine to coarse, well-sorted subangular sand with low sphericity and calcite cementation. Our geotechnical analysis of the bedrock sandstone suggests that pothole occurrence may be linked to low rock strength and slake durability index with high rock absorption and porosity at Loei Dun. Field studies confirmed the impact of other factors such as joints/faults, fluvial conditions and biological weathering. There are five types of pothole, viz., simple ones, potholes with external furrows, compound potholes, breached potholes and lateral ones. The present study adds educational value to the Loei Dun geosite at Phetchabun Geoparks and cultural and economic aspects can be further strengthened through the development of geotourism in the area.

Regiony hydrogeotermalne na Niżu Polskim

Nawrocki Jerzy, Socha Mariusz

Przegląd Geologiczny

2021

Vol. 69, nr 9

578--593

The paper provides a proprsal to divide the three main Mesozoic hydrogeothermal reservoirs of the Polish Lowlands into regions. The division is based primarily on reservoir efficacy in terms of using thermal waters for heating and recreation purposes. The presented validation of individual regions and sub-regions shows that only some parts of them have a medium or high heating potential. The heating and recreation potentials are limited in many places by the high mineralization of thermal waters.