scispace - formally typeset
Book ChapterDOI

Notable Glaciokarsts of the World

Reads0
Chats0
TLDR
In this paper, notable glaciokarsts of the world are presented, where geographical location, geologic and tectonic settings, climatic conditions, glaciation phases as well as surface and underground karst landforms are presented about each selected region.
Abstract
In this chapter, notable glaciokarsts of the world are presented. Geographical location, geologic and tectonic settings, climatic conditions, glaciation phases as well as surface and underground karst landforms are presented about each selected region. Obviously, the areal extent, the degree of exploration and the amount of publicly available information are different in each case. Historically, the first glaciokarst studies were based on the Alps, the Pyrenees, the Dinaric Alps and the British Isles, and they have remained in the focus since then. Hence, these regions are presented here in more detail, but even these presentations can be considered only short overviews. Some other glaciokarst terrains, such as Scandinavia or the Rocky Mountains, have also been thoroughly studied but later in history; nevertheless, there are abundant internationally available publications about them. Certain parts of the Balkan Peninsula, the Apennines or even Anatolia received high attention more recently and novel methods have been used to investigate their glaciokarst terrains. The Carpathians and the Appalachians, which are also discussed in this chapter, are extensively studied mountains in general, but glaciokarsts occupy a relatively small proportion in them. On the other hand, there are still regions, which are difficult to access, where glaciokarsts are poorly explored, and/or the available literature is limited (or the publications are only in Russian, for instance). Some of them, namely, the Altai Mountains, the Greater Caucasus, the Tian Shan, the Pamir and the Patagonian archipelago, are also briefly presented here. Finally, it is noted that our selection does not contain all glaciokarsts of the world because it is beyond the scope of this chapter.

read more

Citations
More filters

Mantle dynamics in the Mediterranean

TL;DR: In this paper, a conceptual and quantitative framework for the causes of surface deformation in the Mediterranean is discussed, which can be outlined by two, almost symmetric, upper mantle convection cells.
Journal ArticleDOI

First 36Cl cosmogenic moraine geochronology of the Dinaric mountain karst: Velež and Crvanj Mountains of Bosnia and Herzegovina

TL;DR: In this paper, the authors presented the first attempt to date moraines in the Dinaric mountain karst using cosmogenic 36Cl surface exposure dating technique, which yielded 36Cl ages spanning from Oldest Dryas for Velež (14.9 ± 1.1 ka) to Younger Dryas (11.9Õ± 0.9 ka), considering the average age of the two oldest samples from each lateral moraine as the most representative time of moraine emplacement.
Journal ArticleDOI

Testing the uniqueness of deep terrestrial life.

TL;DR: It is proposed that the idea of a unique deep terrestrial fauna akin to deep oceanic life is unsupported by data and unwarranted by ecological considerations, and the BFN hypothesis and local ecological and structural factors sufficiently explain the distribution of subterranean terrestrial life even in the deepest karst massifs.
References
More filters
Book

Karst Hydrogeology and Geomorphology

TL;DR: In this article, the authors discuss the relationship between Karst and general geomorphology and Hydrogeology and discuss the development of Karst underground systems, and present a detailed analysis of these systems.
Book ChapterDOI

An outline of North American deglaciation with emphasis on central and northern Canada

TL;DR: In this paper, the authors present revised maps of North American deglaciation at 500-year and finer resolution, which represent an updating of a series prepared nearly two decades ago for the INQUA 1987 Congress.
Journal ArticleDOI

Origin and morphology of limestone caves

TL;DR: The time required to reach the maximum rate is nearly independent of kinetics and varies directly with flow distance and temperature and inversely with initial fracture width, discharge, gradient, and PCO2 as mentioned in this paper.
Journal ArticleDOI

Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites

TL;DR: In this paper, the eustatic component of relative sea-level change provides a measure of the amount of ice transferred between the continents and oceans during glacial cycles, which has been quantified for the period since the last glacial maximum by correcting observed sea level change for the glacio-hydro-isostatic contributions using realistic ice distribution and earth models.