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・ Valley Gang
・ Valley Gardens
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・ Valley Gardens (disambiguation)
・ Valley Gardens Middle School
・ Valley Gardens, Louisville
・ Valley girl
・ Valley Girl (disambiguation)
・ Valley Girl (film)
・ Valley Girl (song)
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Valley
・ Valley (disambiguation)
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・ Valley Acres, California
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・ Valley and ridge salamander
・ Valley and Siletz Railroad
・ Valley Apparel L.L.C.
・ Valley Arts Guitar
・ Valley Australian Football Club
・ Valley Bank of Kalispell
・ Valley Baseball League
・ Valley Bend Wildlife Management Area


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Valley : ウィキペディア英語版
A valley is a low area between hills, often with a river running through it.In geology, a valley or dale is a depression that is longer than it is wide. The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, (at least) with respect of the cross section of the slopes or hillsides.==Valley terminology==A valley in its broadest geographic sense is also known as a ''dale''. A valley through which a river runs may also be referred to as a vale. A small, secluded, and often wooded valley is known as a dell or in Scotland as a glen. A wide, flat valley through which a river runs is known in Scotland as a strath. A mountain cove is a small valley, closed at one or both ends, in the central or southern Appalachian Mountains which sometimes results from the erosion of a geologic window. A small valley surrounded by mountains or ridges is sometimes known as a hollow. A deep, narrow valley is known as a cwm (also spelled ''combe'' or ''coombe''). Similar geological structures, such as canyons, ravines, gorges, gullies, and kloofs, are not usually referred to as valleys. See also: "chine". A valley formed by erosion is called an erosional valley; a valley formed by geologic events such as drop faults or the rise of highlands is called a structural valley.==River valleys == River valley" -->:''For a comprehensive list of world wide river valleys see: ''A valley formed by flowing water, or ''river valley'', is usually V-shaped. The exact shape will depend on the characteristics of the stream flowing through it. Rivers with steep gradients, as in mountain ranges, produce steep walls and a bottom. Shallower slopes may produce broader and gentler valleys. However, in the lowest stretch of a river, where it approaches its base level, it begins to deposit sediment and the valley bottom becomes a floodplain.Some broad ''V'' examples are:* North America: Black Canyon of the Gunnison National Park, and others in Grand Canyon NP* Europe:** Austria: narrow passages of upper Inn valley (Inntal), affluents of Enns** Switzerland: Napf region, Zurich Oberland, Engadin** Germany: affluents to the middle reaches of Rhine and MoselSome of the first human complex societies originated in river valleys, such as that of the Nile, Tigris-Euphrates, Indus, Ganges, Yangtze, Huang He, Mississippi, and arguably Amazon. In prehistory, the rivers were used as a source of fresh water and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, stimulating the development of agriculture. Most of the first civilizations developed from these river valley communities. Another word for river valley is River phenomenon.

A valley is a low area between hills, often with a river running through it.
In geology, a valley or dale is a depression that is longer than it is wide. The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, (at least) with respect of the cross section of the slopes or hillsides.
==Valley terminology==
A valley in its broadest geographic sense is also known as a ''dale''. A valley through which a river runs may also be referred to as a vale. A small, secluded, and often wooded valley is known as a dell or in Scotland as a glen. A wide, flat valley through which a river runs is known in Scotland as a strath. A mountain cove is a small valley, closed at one or both ends, in the central or southern Appalachian Mountains which sometimes results from the erosion of a geologic window. A small valley surrounded by mountains or ridges is sometimes known as a hollow. A deep, narrow valley is known as a cwm (also spelled ''combe'' or ''coombe''). Similar geological structures, such as canyons, ravines, gorges, gullies, and kloofs, are not usually referred to as valleys. See also: "chine". A valley formed by erosion is called an erosional valley; a valley formed by geologic events such as drop faults or the rise of highlands is called a structural valley.
==River valleys ==
:''For a comprehensive list of world wide river valleys see: ''
A valley formed by flowing water, or ''river valley'', is usually V-shaped. The exact shape will depend on the characteristics of the stream flowing through it. Rivers with steep gradients, as in mountain ranges, produce steep walls and a bottom. Shallower slopes may produce broader and gentler valleys. However, in the lowest stretch of a river, where it approaches its base level, it begins to deposit sediment and the valley bottom becomes a floodplain.
Some broad ''V'' examples are:
* North America: Black Canyon of the Gunnison National Park, and others in Grand Canyon NP
* Europe:
*
* Austria: narrow passages of upper Inn valley (Inntal), affluents of Enns
*
* Switzerland: Napf region, Zurich Oberland, Engadin
*
* Germany: affluents to the middle reaches of Rhine and Mosel
Some of the first human complex societies originated in river valleys, such as that of the Nile, Tigris-Euphrates, Indus, Ganges, Yangtze, Huang He, Mississippi, and arguably Amazon. In prehistory, the rivers were used as a source of fresh water and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, stimulating the development of agriculture. Most of the first civilizations developed from these river valley communities. Another word for river valley is River phenomenon.

抄文引用元・出典: フリー百科事典『 :''For a comprehensive list of world wide river valleys see: ''A valley formed by flowing water, or ''river valley'', is usually V-shaped. The exact shape will depend on the characteristics of the stream flowing through it. Rivers with steep gradients, as in mountain ranges, produce steep walls and a bottom. Shallower slopes may produce broader and gentler valleys. However, in the lowest stretch of a river, where it approaches its base level, it begins to deposit sediment and the valley bottom becomes a floodplain.Some broad ''V'' examples are:* North America: Black Canyon of the Gunnison National Park, and others in Grand Canyon NP* Europe:** Austria: narrow passages of upper Inn valley (Inntal), affluents of Enns** Switzerland: Napf region, Zurich Oberland, Engadin** Germany: affluents to the middle reaches of Rhine and MoselSome of the first human complex societies originated in river valleys, such as that of the Nile, Tigris-Euphrates, Indus, Ganges, Yangtze, Huang He, Mississippi, and arguably Amazon. In prehistory, the rivers were used as a source of fresh water and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, stimulating the development of agriculture. Most of the first civilizations developed from these river valley communities. Another word for river valley is River phenomenon.">ウィキペディア(Wikipedia)
:''For a comprehensive list of world wide river valleys see: ''A valley formed by flowing water, or ''river valley'', is usually V-shaped. The exact shape will depend on the characteristics of the stream flowing through it. Rivers with steep gradients, as in mountain ranges, produce steep walls and a bottom. Shallower slopes may produce broader and gentler valleys. However, in the lowest stretch of a river, where it approaches its base level, it begins to deposit sediment and the valley bottom becomes a floodplain.Some broad ''V'' examples are:* North America: Black Canyon of the Gunnison National Park, and others in Grand Canyon NP* Europe:** Austria: narrow passages of upper Inn valley (Inntal), affluents of Enns** Switzerland: Napf region, Zurich Oberland, Engadin** Germany: affluents to the middle reaches of Rhine and MoselSome of the first human complex societies originated in river valleys, such as that of the Nile, Tigris-Euphrates, Indus, Ganges, Yangtze, Huang He, Mississippi, and arguably Amazon. In prehistory, the rivers were used as a source of fresh water and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, stimulating the development of agriculture. Most of the first civilizations developed from these river valley communities. Another word for river valley is River phenomenon.">ウィキペディアで「A valley is a low area between hills, often with a river running through it.In geology, a valley or dale is a depression that is longer than it is wide. The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, (at least) with respect of the cross section of the slopes or hillsides.==Valley terminology==A valley in its broadest geographic sense is also known as a ''dale''. A valley through which a river runs may also be referred to as a vale. A small, secluded, and often wooded valley is known as a dell or in Scotland as a glen. A wide, flat valley through which a river runs is known in Scotland as a strath. A mountain cove is a small valley, closed at one or both ends, in the central or southern Appalachian Mountains which sometimes results from the erosion of a geologic window. A small valley surrounded by mountains or ridges is sometimes known as a hollow. A deep, narrow valley is known as a cwm (also spelled ''combe'' or ''coombe''). Similar geological structures, such as canyons, ravines, gorges, gullies, and kloofs, are not usually referred to as valleys. See also: "chine". A valley formed by erosion is called an erosional valley; a valley formed by geologic events such as drop faults or the rise of highlands is called a structural valley.==River valleys == River valley" -->:''For a comprehensive list of world wide river valleys see: ''A valley formed by flowing water, or ''river valley'', is usually V-shaped. The exact shape will depend on the characteristics of the stream flowing through it. Rivers with steep gradients, as in mountain ranges, produce steep walls and a bottom. Shallower slopes may produce broader and gentler valleys. However, in the lowest stretch of a river, where it approaches its base level, it begins to deposit sediment and the valley bottom becomes a floodplain.Some broad ''V'' examples are:* North America: Black Canyon of the Gunnison National Park, and others in Grand Canyon NP* Europe:** Austria: narrow passages of upper Inn valley (Inntal), affluents of Enns** Switzerland: Napf region, Zurich Oberland, Engadin** Germany: affluents to the middle reaches of Rhine and MoselSome of the first human complex societies originated in river valleys, such as that of the Nile, Tigris-Euphrates, Indus, Ganges, Yangtze, Huang He, Mississippi, and arguably Amazon. In prehistory, the rivers were used as a source of fresh water and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation, stimulating the development of agriculture. Most of the first civilizations developed from these river valley communities. Another word for river valley is River phenomenon.」の詳細全文を読む



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