Since the greenhouse effect emerged as a predictable threat, necessitating the evalu ation of its future impact on the environment in the various parts of the globe, interest in the climate changes during the Holocene has gained momentum. The background can be summarized by the sentence: The past is a key to the future. As a matter of fact, this sentence is in the opposite direction, on the dimension of time, to the principle adopted by the founders of the science of geology. They proposed that geological processes in the present should be used as a key for understanding the past. Another reason for the interest in the history of the climate of the Holocene can be described as the renaissance of a modified deterministic approach to the inter relation between physical and human geography. This relates in the first place to the fact that various investigations, especially as carried out by Hubert Lamb, showed that the sequence of climate changes previously suggested by Blytt and Sernander for Europe and adopted by most Holocene climatologists was far too general, and that there were more climate changes during recent history than previously taken account of. In the second place it was found out that these changes had had an impact on the history of human communities. Thus, one can conclude that once the taboo on geographical determinism (i. e."

This survey of the ancient levels of lakes, rivers and the sea, as well as changes in the compositions of stalagmites and sediments reveals an astonishing correlation of climate changes with the emergence and collapse of civilizations in the Middle East. The authors conclude that climate change has been the decisive factor in the history surrounding the origins of the "cradle of civilization."

Arid and semi-arid regions can be defined as environments in which water is the limit ing factor for bio-systems. This means that survival of life in these regions involves a constant struggle to obtain this limited commodity and draw the maximum benefit out of it. However, despite the difficulties for plants, animals, and man to live in, these regions, they are being utilized more and more because of the pressure of world population growth. This is expressed in the expansion of agricultural activities in desert lands as well as by the formation and rapid growth of urban and industrial centers. These trends result in a growing demand for water on the one hand, and the disposal of vast amounts of waste water, as well as other types of refuse, on the other. Meeting the first demand, namely, supplying water to the agricultural communities and urban centers, involves, in many instances, the over-exploitation and misuse of nat ural water resources. The surplus of waste water, sometimes highly loaded with toxic compounds, is likely to cause irreversible damage to the environment. The geoscientists and engineers face a challenge on two conflicting fronts. Success on one front, namely, in answering the full demand for water, may lead to an increase in the pollution of the environment by waste water."

The book is based on the results of the investigations of the authors in the semi-arid and arid regions (ASAR) of the globe. These investigations brought to the conclusion that the warming climate will cause the drying up of the water resources in these regions. In this case the principles of Sustainable Development will not be able to avert forthcoming catastrophes. These conclusions brought to the compilation of the policy of "Progressive Development," emphasising investment in the development of new water resources and changing the natural environments while advancing the local populations on the dimension of knowledge by education.

Since the beginning of man's existence on Earth, the adequacy of available water has been as important as any other factor for man's survival and prosperity.
The volume comprises comprehensive reviews on: Paleoenvironments of arid land, climate-water-man interactions, water resources in the Minoan era, ancient Greek examples of avoiding water shortages, climatic changes in the eastern Mediterranean region since 5000 B.C., climatic evolution in ancient civilizations based on fossil studies, impact of climatic changes on groundwater and Mediterranean wetlands.
The book is written for civil and agricultural engineers, hydrologists, geologists, environmental scientists and researchers. It is also useful as a reference to consulting engineers, agriculturists, environmentalists and students.

This book presents an update and revision of the book Water Shall Flow from the Rock - Hydrogeology and Climate in the Lands of the Bible by A. Issar, published by Springer-Verlag in 1990. The enormous quantity and quality of new data added since 1990 called for a thorough update. Another reason for this work is the better understanding achieved since the initial book was published about the role which climate plays in shaping the history of the Lands of the Bible. Albeit the fact that the impact of climate change was touched upon rather widely in the first book, still, without interweaving the new data and understanding, the picture would have remained partial.

The book is based on the results of the investigations of the authors in the semi-arid and arid regions (ASAR) of the globe. These investigations brought to the conclusion that the warming climate will cause the drying up of the water resources in these regions. In this case the principles of Sustainable Development will not be able to avert forthcoming catastrophes. These conclusions brought to the compilation of the policy of "Progressive Development," emphasising investment in the development of new water resources and changing the natural environments while advancing the local populations on the dimension of knowledge by education.

Since the greenhouse effect emerged as a predictable threat, necessitating the evalu ation of its future impact on the environment in the various parts of the globe, interest in the climate changes during the Holocene has gained momentum. The background can be summarized by the sentence: The past is a key to the future. As a matter of fact, this sentence is in the opposite direction, on the dimension of time, to the principle adopted by the founders of the science of geology. They proposed that geological processes in the present should be used as a key for understanding the past. Another reason for the interest in the history of the climate of the Holocene can be described as the renaissance of a modified deterministic approach to the inter relation between physical and human geography. This relates in the first place to the fact that various investigations, especially as carried out by Hubert Lamb, showed that the sequence of climate changes previously suggested by Blytt and Sernander for Europe and adopted by most Holocene climatologists was far too general, and that there were more climate changes during recent history than previously taken account of. In the second place it was found out that these changes had had an impact on the history of human communities. Thus, one can conclude that once the taboo on geographical determinism (i. e."

Arid and semi-arid regions can be defined as environments in which water is the limit ing factor for bio-systems. This means that survival of life in these regions involves a constant struggle to obtain this limited commodity and draw the maximum benefit out of it. However, despite the difficulties for plants, animals, and man to live in, these regions, they are being utilized more and more because of the pressure of world population growth. This is expressed in the expansion of agricultural activities in desert lands as well as by the formation and rapid growth of urban and industrial centers. These trends result in a growing demand for water on the one hand, and the disposal of vast amounts of waste water, as well as other types of refuse, on the other. Meeting the first demand, namely, supplying water to the agricultural communities and urban centers, involves, in many instances, the over-exploitation and misuse of nat ural water resources. The surplus of waste water, sometimes highly loaded with toxic compounds, is likely to cause irreversible damage to the environment. The geoscientists and engineers face a challenge on two conflicting fronts. Success on one front, namely, in answering the full demand for water, may lead to an increase in the pollution of the environment by waste water."

This survey of the ancient levels of lakes, rivers and the sea, as well as changes in the compositions of stalagmites and sediments reveals an astonishing correlation of climate changes with the emergence and collapse of civilizations in the Middle East. The authors conclude that climate change has been the decisive factor in the history surrounding the origins of the "cradle of civilization."

It is now widely accepted that increasing concentrations of greenhouse gases in the atmosphere are causing higher global atmospheric temperatures. However, there is still a great deal of uncertainty about the likely effects of such a temperature rise on climate, and even more about the impacts of climate change and variability on the world's hydrological regimes and socio-economic systems. Studying the effects of climate variability in the past can give clues as to possible future effects. This volume provides a comprehensive review of the effects of climate variability on hydrological and human systems in the Holocene (the last 10,000 years), in various parts of the world. The book concentrates on the regions bordering the Mediterranean Sea, western and central Europe, China, Japan, West and South Africa and the southwestern USA. This book will be of value to researchers and professionals in hydrology, climatology, geology and historical geography.

Many times when the author saw the bedouins of southern Sinai excavate their wells in the crystalline rocks, from which this part of the peninsula is built, the story of Moses striking the rock to get water came to mind. The reader will, indeed, find in this book the description for a rather simple method by which to strike the rock to get water in the wilderness of Sinai. Yet this method was not invented by the author nor by any other modem hydrogeologist, but was a method that the author learned from the bedouins living in the crystalline mountains of southern Sinai. These bedouins, belonging to the tribe of the Gebelia (the "mountain people"), live around the monastery of Santa Katerina and, according to their tradition, which has been conftrmed by historical research, were once Christians who were brought by the Byzantine emperor, Justinian, from the Balkans in the 6th century A. D. to be servants to the priests of the monastery. They know how to discern places where veins of calcite fIlled the fractures of the granites; such places are a sign of an extinct spring. They also know how to distinguish an acid hard granite rock, and hard porphyry dike from a soft diabase dike. The latter indicated the location at which they should dig for water into the subsurface. In Chapter 9, the reader will ftnd a detailed description of how they used this knowledge to extract water from the rock.

It is now widely accepted that increasing concentrations of greenhouse gases in the atmosphere are causing higher global temperatures. This volume provides a comprehensive review of the effects of climate variability on hydrological and human systems in the Holocene (the last 10,000 years). The book concentrates on the regions bordering the Mediterranean Sea, western and central Europe, China, Japan, West and South Africa and southwestern U.S.A. It is intended for researchers and professionals in hydrology, climatology, geology and historical geography.