Coastal and Bottom Topography

Игнатов, Евгений

doi:10.1007/698_5_078

Cited by 5 publications

(1 citation statement)

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“…Morphometric characteristics and topography of the Black Sea bottom are described in detail in the geological literature and regional oceanographic research works (Arkhangel'sky & Strakhov 1938;Goncharov et al 1978;Shnyukov 1987;Simonov & Altman 1991;Ignatov 2008;Eremeev & Symonenko 2009). …”

Section: Modern Coastlinementioning

confidence: 99%

Geological and Geomorphological Factors and Marine Conditions of the Azov‐Black Sea Basin and Coastal Characteristics as They Determine Prospecting for Seabed Prehistoric Sites on the Continental Shelf

Yanko-Hombach

Schnyukov

Пасынков

et al. 2017

Submerged Landscapes of the European Continental Shelf

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Section: Modern Coastlinementioning

confidence: 99%

Geological and Geomorphological Factors and Marine Conditions of the Azov‐Black Sea Basin and Coastal Characteristics as They Determine Prospecting for Seabed Prehistoric Sites on the Continental Shelf

Yanko-Hombach

Schnyukov

Пасынков

et al. 2017

Submerged Landscapes of the European Continental Shelf

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Peculiarities of tsunamis generated by Asteroid impact or nuclear explosions in the northwest of Black Sea

Isvoranu

Badescu

2010

Nat Hazards

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Different models are used to evaluate the seashore effects of the tsunami generated by an asteroid impacting the shallow-water plateau in the northwest basin of the Black Sea. The shortest distance between the impact location and the coast is about 185 km. The tsunami's effects on the coastal regions depend on many factors among which the most important is asteroid size. The tsunami generated by a 250-m asteroid reaches the nearest dry land location in 35 min and needs about 2 h to arrive all over the Black Sea coast. The run-up value is about 2 m high on Turkish and Crimean coasts. In the western Black Sea regions, the wave height is about 3 m. The run-up values strongly depend on bathymetry and topography peculiarities. The run-up values in case of the tsunami generated by a 1,000-m-sized asteroid are up to five to six times larger than in case of the 250-m impactor, depending on location. Differences between the tsunami's dynamics on coastal regions situated in the proximity of deep water and shallow water, respectively, are outlined. Aspects concerning accidental or deliberate nuclear explosions are briefly referred. Possible social consequences and prevention are shortly discussed.

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Narrow shelf canyons vs. wide shelf canyons: Two distinct types of Black Sea submarine canyons

Jipa

Panin

2020

Quaternary International

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Coastal and Bottom Topography

Cited by 5 publications

References 0 publications

Geological and Geomorphological Factors and Marine Conditions of the Azov‐Black Sea Basin and Coastal Characteristics as They Determine Prospecting for Seabed Prehistoric Sites on the Continental Shelf

Geological and Geomorphological Factors and Marine Conditions of the Azov‐Black Sea Basin and Coastal Characteristics as They Determine Prospecting for Seabed Prehistoric Sites on the Continental Shelf

Peculiarities of tsunamis generated by Asteroid impact or nuclear explosions in the northwest of Black Sea

Narrow shelf canyons vs. wide shelf canyons: Two distinct types of Black Sea submarine canyons

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