Erosional and Depositional Textures and Structures in Coastal Karst Landscapes

Taboroši, Danko; Kázmér, Miklós

doi:10.1007/978-94-007-5016-6_2

Cited by 27 publications

(16 citation statements)

References 115 publications

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“…They develop parallel to sea level by a combination of physical and biological abrasion and biological and chemical dissolution (e.g., Focke, 1978;Kázmér and Taboroši, 2012;Neumann, 1966;Pirazzoli et al, 1994;Pirazzoli, Laborel, and Stiros, 1996;Taboroši and Ká zmér, 2012). Marine notches will form in the tidal zone under quiet and moderate conditions, whereas wave-stressed coasts usually lack them, wave undercutting and cliff collapse being faster than notch formation (Sunamura, 1992;Trenhaile, 1987).…”

Section: Discussion Why Measure Notches?mentioning

confidence: 99%

Rapid Profiling of Marine Notches Using a Handheld Laser Distance Meter

Kázmér

Taboroši

2012

Journal of Coastal Research

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A rapid, single-user profiling method for rocky shores is described. The Leica Disto D8 handheld laser distance meter measures distance up to 100 m and inclination in 360u. It automatically calculates horizontal distance and vertical elevation. Memory storage accommodates data for 30 measurement points, allowing easy plotting of shore profiles. This technique allows even inaccessible, dangerous, and overhanging cliff faces to be evaluated faithfully and within minutes. It is a major improvement over standard methods that often involve risky coasteering and climbing. Examples are given from marine notches in Thailand. ADDITIONAL INDEX WORDS:Rocky coast, active tectonics, Thailand.

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Section: Discussion Why Measure Notches?mentioning

confidence: 99%

Rapid Profiling of Marine Notches Using a Handheld Laser Distance Meter

Kázmér

Taboroši

2012

Journal of Coastal Research

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“…At any rate, microscopic bioerosional features can only be noted in places where they are not immediately overprinted by eroding activities of larger organisms. In tropical regions, microbial effects on coastal rocks are most evident in the form of ubiquitous 'phytokarst' -highly irregular and extraordinarily jagged type of karren that develops in eogenetic limestones attacked by boring cyanobacteria (Jones 1989;Taboroši & Kázmér 2013).…”

Section: Bioerodersmentioning

confidence: 99%

“…Pulau Langgun cooling by seawater. That may lead to significant corrosion (Moses 2003;Taboroši & Kázmér 2013). Furthermore, cyanobacteria, other microbes and fungi tend to be the only organisms adapted to life in these chemically and thermally extreme environments and their bioerosional activity contributes to the overall geomorphic shaping.…”

Section: Spraymentioning

confidence: 99%

“…Some of them appear to be capable of scratching the rock with their radulas and consuming endolithic organisms as well. Though they do not leave bioerosional traces visible to the naked eye, they do contribute to the overall bioerosional process and lowering of the bedrock surface (Taboroši & Kázmér 2013). …”

Section: Littorinid Snailsmentioning

confidence: 99%

“…Distribution is delimited upwards by their (in) tolerance to desiccation and downwards by the presence of seastars that predate on newly settled juveniles (Shumway 1996). Oysters can form a horizontal ledge (corniche of Pirazzoli 1996: 44), up to 1 m wide (Taboroši & Kázmér 2013, Figure 2.9h).…”

Section: Oystersmentioning

confidence: 99%

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Features of Intertidal Bioerosion and Bioconstruction on Limestone Coasts of Langkawi Islands, Malaysia

Kázmér¹,

Leman²,

Mohamed³

et al. 2015

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A review of the rock art of Palau, Micronesia in local and regional contexts

Liston

Hoerman

Sasao³

et al. 2021

Archaeology in Oceania

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The style and iconography of the ten rock art sites known so far in Palau, Micronesia, including two newly discovered rock painting sites, are described and linked to their geographic locations, archaeological associations, oral traditions and local iconographies. Following a brief review of rock art in Micronesia and parts of Island Southeast Asia and New Guinea, Palau's eight rock painting sites and two rock engraving sites are regionally contextualized. We found no apparent relationships with rock art elsewhere in Micronesia but stylistic similarities with eastern Indonesia and West Papua painting traditions are clear. This may suggest the Palau paintings were created early in the archipelago's cultural sequence. Palau's rock paintings are clearly within the Austronesian painting tradition while the single well‐recorded carving site does not conform with the Austronesian engraving style. Palau's rock art is also closely aligned to the Oceanic Rock Art Tradition.

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Erosional and Depositional Textures and Structures in Coastal Karst Landscapes

Cited by 27 publications

References 115 publications

Rapid Profiling of Marine Notches Using a Handheld Laser Distance Meter

Rapid Profiling of Marine Notches Using a Handheld Laser Distance Meter

Features of Intertidal Bioerosion and Bioconstruction on Limestone Coasts of Langkawi Islands, Malaysia

A review of the rock art of Palau, Micronesia in local and regional contexts

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