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Shouf Cedar Biosphere Reserve Limit地形図

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Shouf Cedar Biosphere Reserve Limit

Precipitation in the watershed is the source of both surface streamflow and groundwater. The major portion of this occurs as rain. Snowfall often occurs at the upper elevations but snow seldom persists more than a few days and disappears before the end of the rainy season. Normally snow has little overall direct effect on stream-flow within the watershed/ A large proportion of the exposed surface rock in the Barouk region is cavernous, fissured and broken limestone, and its porous condition makes it very permeable. This results in much of the precipitation infiltrating with minimum surface runoff despite the often-shallow soils and sparse vegetative cover. Water percolates downward through the various formations and feeds the springs found on lower slopes in the area. Surface water flows originating on the range are mostly seasonal but some are perennial. Underground water generates outflow rivers such as: - Al Awali River, more commonly known as Al-Barouk river - Damour River, known as Al-Safa river The summit of the range is considered as a divide between two hydrological systems because of the difference between the two slopes of the mountain. The rivers that flow in the valleys are the major source of agriculture irrigation and supply a dozen Shouf villages with domestic water and some of the western Bekaa villages.

Wikipedia (CC-BY-SA 3.0)

この地図について

名前Shouf Cedar Biosphere Reserve Limitの地形図、標高、地勢。

場所Shouf Cedar Biosphere Reserve Limit, Western Beqaa District, Beqaa Governorate, Lebanon (33.48771 35.57255 33.83497 35.83461)

平均標高:980 m

最低標高:9 m

最大標高:2,058 m

その他の地形図

地図をクリックすると、その地形、その標高、その地勢が表示されます。

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Lebanon > Beqaa Governorate

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次の冒険に備えよう:

❄️スパッツ(ゲイター) - 靴の中への雪や砂の侵入を防ぐレッグカバー
🧢登山用ハット・キャップ - 紫外線対策と蒸れ防止を両立した、折りたたみ可能な帽子
🎒軽量登山デイバッグ - 日帰り登山に最適な小型バックパック
🥾ハイキングスニーカー - 軽量で歩きやすく、日帰りハイキングに最適
🧴アウトドア虫除け - 登山やキャンプで蚊や虫から身を守る虫除けスプレー

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