Kali Sindu: Béda antara owahan
Konten dihapus Konten ditambahkan
c éjaan using AWB |
c yaiku -> ya iku, miturut Bausastra Jawa Balai Bahasa Yogyakarta, replaced: yaiku → ya iku (7) using AWB |
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Larik 94:
Miwiti saka panggonan kang dhuwur ing donya kanthi lèlèhan ès ([[glaciers]]), kali iki mènèhi warna tumrap ékosistem kang arupa alas kanthi hawa kang sedhengan, [[dhataran]] lan laladan kang gersang. Bebarengan karo kali [[Kali Chenab|Chenab]], [[Kali Ravi|Ravi]], [[Kali Sutlej|Sutlej]], [[Kali Jhelum|Jhelum]], [[Kali Beas|Beas]] lan kali mati [[Kali Sarasvati|Sarasvati]], kali Sindu maujud dadi delta ''[[Sapta Sindhu]]'' ("Kali Pitu") ing provinsi [[Sindh]] ing Pakistan. Kali iki nduwèni 20 anak kali utama.
Kali Sindu nyadiakaké sumber wigati banyu tumrap ékonomi Pakistan - utamané lumbung pangan {''breadbasket'')
Sumber utama banyu Kali Sindu
Kali Sindu iku salah siji saka sethithik kali ing donya kang duwé arus pasang surut ombak (''tidal bore''). Sistem Kali Indus iku olèh sumber banyu saka salju lan lèlèhan ès (glacier) saka Karakoram, [[Hindu Kush]] lan pagunungan Himalaya ing Tibet, Kashmir lan [[Pakistan]] sisih lor. Ilèné kali uga ditentokaké déning mangsa - kurang banget banyuné jroning mangsa anyep winter, nanging banjir ing mangsa ketiga (''monsoon''),
== Sajarah ==
Larik 151:
<!-- Image with unknown copyright status removed: [[Image:IndusMap.jpg|thumb|200px|Map showing the change experienced in the drainage of the Indus River after five million year ago when the tributaries of the Indus flowing from the Punjab were captured from the Ganges.]] -->
Kali Sindu ngisi dhasar muara (''submarine fan'') kang dumunung ing [[Segara Arabia]], kang dadi endhapan lumpur nomer loro paling gedhé ing donya, watara 5 yuta km<sup>3</sup> material kang dilorod saka tlatah pagunungan. Studi bab endhapan ing kali nuduhaké yèn [[Karakoram|gunung-gunung Karakoram]] ing Pakistan lor minangka sumber utama material endhapan, lan pagunungan Himalaya nomer panyumbang loro, akèh-akèhé liwat ilèn kali-kali ing Punjab (
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The delta of this proto-Indus river has subsequently been found in the Katawaz Basin, on the Afghan-Pakistan border. Most recently the Indus was paralleled by the ancient [[Saraswati River]], which the [[Rigveda]] suggests flowed from the [[Himalaya]] between the [[Sutlej]] and the [[Yamuna]] Rivers, close to modern day [[Chandigarh]]. Reportedly the [[Saraswati River]] was totally dried by 1900 BCE as confirmed by archaeological hydrological radiocarbon dating {{Fact|date=March 2007}}.
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