Ghaggar-Hakra River (English Wikipedia)

Analysis of information sources in references of the Wikipedia article "Ghaggar-Hakra River" in English language version.

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  • "Hakra". Totally Explained. Archived from the original on 12 July 2012. Retrieved 20 August 2009.

books.google.com

breakthrough-india.org

currentscience.ac.in

dnaindia.com

doi.org

eurogenes.blogspot.nl

handle.net

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  • From Brooke (2015):[24] “The story in Harappan India was somewhat different (see Figure 111.3). The Bronze Age village and urban societies of the Indus Valley are some-thing of an anomaly, in that archaeologists have found little indication of local defence and regional warfare. It would seem that the bountiful monsoon rainfall of the Early to Mid-Holocene had forged a condition of plenty for all, and that competitive energies were channelled into commerce rather than conflict. Scholars have long argued that these rains shaped the origins of the urban Harappan societies, which emerged from Neolithic villages around 2600 BC. It now appears that this rainfall began to slowly taper off in the third millennium, at just the point that the Harappan cities began to develop. Thus it seems that this "first urbanization" in South Asia was the initial response of the Indus Valley peoples to the beginning of Late Holocene aridification. These cities were maintained for 300 to 400 years and then gradually abandoned as the Harappan peoples resettled in scattered villages in the eastern range of their territories, into the Punjab and the Ganges Valley ... .” — Brooke (2015)[24]: 17  (footnotes)
    (a) Giosan, Liviu; et al. (2012). "Fluvial landscapes of the Harappan Civilization". Proceedings of the National Academy of Sciences, USA. 102 (26): E1688–E1694. Bibcode:2012PNAS..109E1688G. doi:10.1073/pnas.1112743109. PMC 3387054. PMID 22645375;
    (b) Ponton, Camilo (2012). "Holocene aridification of India". Geophysical Research Letters. 39 (3): L03704. Bibcode:2012GeoRL..39.3704P. doi:10.1029/2011GL050722. hdl:1912/5100. S2CID 140604921;
    (c) Rashid, Harunur; et al. (2011). "Late glacial to Holocene Indian summer monsoon variability based upon sediment records taken from the Bay of Bengal" (PDF). Terrestrial, Atmospheric and Oceanic Sciences. 22 (2): 215–228. Bibcode:2011TAOS...22..215R. doi:10.3319/TAO.2010.09.17.02(TibXS);
    (d) Madella, Marco; Fuller, Dorian Q. (2006). "Palaeoecology and the Harappan civilisation of south Asia: A reconsideration". Quaternary Science Reviews. 25 (11–12): 1283–1301. Bibcode:2006QSRv...25.1283M. doi:10.1016/j.quascirev.2005.10.012.
    Compare with the very different interpretations in Possehl (2002),[25] and Staubwasser et al. (2003),[26] Bar-Matthews & Avner Ayalon (2015).[27]

harvard.edu

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hillsofmorni.com

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ncbi.nlm.nih.gov

  • From Brooke (2015):[24] “The story in Harappan India was somewhat different (see Figure 111.3). The Bronze Age village and urban societies of the Indus Valley are some-thing of an anomaly, in that archaeologists have found little indication of local defence and regional warfare. It would seem that the bountiful monsoon rainfall of the Early to Mid-Holocene had forged a condition of plenty for all, and that competitive energies were channelled into commerce rather than conflict. Scholars have long argued that these rains shaped the origins of the urban Harappan societies, which emerged from Neolithic villages around 2600 BC. It now appears that this rainfall began to slowly taper off in the third millennium, at just the point that the Harappan cities began to develop. Thus it seems that this "first urbanization" in South Asia was the initial response of the Indus Valley peoples to the beginning of Late Holocene aridification. These cities were maintained for 300 to 400 years and then gradually abandoned as the Harappan peoples resettled in scattered villages in the eastern range of their territories, into the Punjab and the Ganges Valley ... .” — Brooke (2015)[24]: 17  (footnotes)
    (a) Giosan, Liviu; et al. (2012). "Fluvial landscapes of the Harappan Civilization". Proceedings of the National Academy of Sciences, USA. 102 (26): E1688–E1694. Bibcode:2012PNAS..109E1688G. doi:10.1073/pnas.1112743109. PMC 3387054. PMID 22645375;
    (b) Ponton, Camilo (2012). "Holocene aridification of India". Geophysical Research Letters. 39 (3): L03704. Bibcode:2012GeoRL..39.3704P. doi:10.1029/2011GL050722. hdl:1912/5100. S2CID 140604921;
    (c) Rashid, Harunur; et al. (2011). "Late glacial to Holocene Indian summer monsoon variability based upon sediment records taken from the Bay of Bengal" (PDF). Terrestrial, Atmospheric and Oceanic Sciences. 22 (2): 215–228. Bibcode:2011TAOS...22..215R. doi:10.3319/TAO.2010.09.17.02(TibXS);
    (d) Madella, Marco; Fuller, Dorian Q. (2006). "Palaeoecology and the Harappan civilisation of south Asia: A reconsideration". Quaternary Science Reviews. 25 (11–12): 1283–1301. Bibcode:2006QSRv...25.1283M. doi:10.1016/j.quascirev.2005.10.012.
    Compare with the very different interpretations in Possehl (2002),[25] and Staubwasser et al. (2003),[26] Bar-Matthews & Avner Ayalon (2015).[27]
  • Singh et al. 2017. Singh, Ajit; Thomsen, Kristina J.; Sinha, Rajiv; Buylaert, Jan-Pieter; Carter, Andrew; Mark, Darren F.; Mason, Philippa J.; Densmore, Alexander L.; Murray, Andrew S. (28 November 2017). "Counter-intuitive influence of Himalayan river morphodynamics on Indus Civilisation urban settlements". Nature Communications. 8 (1): 1617. Bibcode:2017NatCo...8.1617S. doi:10.1038/s41467-017-01643-9. ISSN 2041-1723. PMC 5705636. PMID 29184098.
  • Khonde et al. 2017. Khonde, Nitesh; Kumar Singh, Sunil; Maur, D. M.; Rai, Vinai K.; Chamyal, L. S.; Giosan, Liviu (2017), "Tracing the Vedic Saraswati River in the Great Rann of Kachchh", Scientific Reports, 7 (1): 5476, Bibcode:2017NatSR...7.5476K, doi:10.1038/s41598-017-05745-8, PMC 5511136, PMID 28710495
  • Giosan et al. 2012. Giosan; et al. (2012), "Fluvial landscapes of the Harappan civilization", PNAS, 109 (26): E1688–E1694, Bibcode:2012PNAS..109E1688G, doi:10.1073/pnas.1112743109, PMC 3387054, PMID 22645375
  • Chatterjee et al. 2019. Chatterjee, Anirban; Ray, Jyotiranjan S.; Shukla, Anil D.; Pande, Kanchan (20 November 2019). "On the existence of a perennial river in the Harappan heartland". Scientific Reports. 9 (1): 17221. Bibcode:2019NatSR...917221C. doi:10.1038/s41598-019-53489-4. ISSN 2045-2322. PMC 6868222. PMID 31748611.
  • Giosan et al. 2012, p. 1693. Giosan; et al. (2012), "Fluvial landscapes of the Harappan civilization", PNAS, 109 (26): E1688–E1694, Bibcode:2012PNAS..109E1688G, doi:10.1073/pnas.1112743109, PMC 3387054, PMID 22645375

pubmed.ncbi.nlm.nih.gov

  • From Brooke (2015):[24] “The story in Harappan India was somewhat different (see Figure 111.3). The Bronze Age village and urban societies of the Indus Valley are some-thing of an anomaly, in that archaeologists have found little indication of local defence and regional warfare. It would seem that the bountiful monsoon rainfall of the Early to Mid-Holocene had forged a condition of plenty for all, and that competitive energies were channelled into commerce rather than conflict. Scholars have long argued that these rains shaped the origins of the urban Harappan societies, which emerged from Neolithic villages around 2600 BC. It now appears that this rainfall began to slowly taper off in the third millennium, at just the point that the Harappan cities began to develop. Thus it seems that this "first urbanization" in South Asia was the initial response of the Indus Valley peoples to the beginning of Late Holocene aridification. These cities were maintained for 300 to 400 years and then gradually abandoned as the Harappan peoples resettled in scattered villages in the eastern range of their territories, into the Punjab and the Ganges Valley ... .” — Brooke (2015)[24]: 17  (footnotes)
    (a) Giosan, Liviu; et al. (2012). "Fluvial landscapes of the Harappan Civilization". Proceedings of the National Academy of Sciences, USA. 102 (26): E1688–E1694. Bibcode:2012PNAS..109E1688G. doi:10.1073/pnas.1112743109. PMC 3387054. PMID 22645375;
    (b) Ponton, Camilo (2012). "Holocene aridification of India". Geophysical Research Letters. 39 (3): L03704. Bibcode:2012GeoRL..39.3704P. doi:10.1029/2011GL050722. hdl:1912/5100. S2CID 140604921;
    (c) Rashid, Harunur; et al. (2011). "Late glacial to Holocene Indian summer monsoon variability based upon sediment records taken from the Bay of Bengal" (PDF). Terrestrial, Atmospheric and Oceanic Sciences. 22 (2): 215–228. Bibcode:2011TAOS...22..215R. doi:10.3319/TAO.2010.09.17.02(TibXS);
    (d) Madella, Marco; Fuller, Dorian Q. (2006). "Palaeoecology and the Harappan civilisation of south Asia: A reconsideration". Quaternary Science Reviews. 25 (11–12): 1283–1301. Bibcode:2006QSRv...25.1283M. doi:10.1016/j.quascirev.2005.10.012.
    Compare with the very different interpretations in Possehl (2002),[25] and Staubwasser et al. (2003),[26] Bar-Matthews & Avner Ayalon (2015).[27]
  • Singh et al. 2017. Singh, Ajit; Thomsen, Kristina J.; Sinha, Rajiv; Buylaert, Jan-Pieter; Carter, Andrew; Mark, Darren F.; Mason, Philippa J.; Densmore, Alexander L.; Murray, Andrew S. (28 November 2017). "Counter-intuitive influence of Himalayan river morphodynamics on Indus Civilisation urban settlements". Nature Communications. 8 (1): 1617. Bibcode:2017NatCo...8.1617S. doi:10.1038/s41467-017-01643-9. ISSN 2041-1723. PMC 5705636. PMID 29184098.
  • Khonde et al. 2017. Khonde, Nitesh; Kumar Singh, Sunil; Maur, D. M.; Rai, Vinai K.; Chamyal, L. S.; Giosan, Liviu (2017), "Tracing the Vedic Saraswati River in the Great Rann of Kachchh", Scientific Reports, 7 (1): 5476, Bibcode:2017NatSR...7.5476K, doi:10.1038/s41598-017-05745-8, PMC 5511136, PMID 28710495
  • Giosan et al. 2012. Giosan; et al. (2012), "Fluvial landscapes of the Harappan civilization", PNAS, 109 (26): E1688–E1694, Bibcode:2012PNAS..109E1688G, doi:10.1073/pnas.1112743109, PMC 3387054, PMID 22645375
  • Chatterjee et al. 2019. Chatterjee, Anirban; Ray, Jyotiranjan S.; Shukla, Anil D.; Pande, Kanchan (20 November 2019). "On the existence of a perennial river in the Harappan heartland". Scientific Reports. 9 (1): 17221. Bibcode:2019NatSR...917221C. doi:10.1038/s41598-019-53489-4. ISSN 2045-2322. PMC 6868222. PMID 31748611.
  • Giosan et al. 2012, p. 1693. Giosan; et al. (2012), "Fluvial landscapes of the Harappan civilization", PNAS, 109 (26): E1688–E1694, Bibcode:2012PNAS..109E1688G, doi:10.1073/pnas.1112743109, PMC 3387054, PMID 22645375

osu.edu

research.bpcrc.osu.edu

  • From Brooke (2015):[24] “The story in Harappan India was somewhat different (see Figure 111.3). The Bronze Age village and urban societies of the Indus Valley are some-thing of an anomaly, in that archaeologists have found little indication of local defence and regional warfare. It would seem that the bountiful monsoon rainfall of the Early to Mid-Holocene had forged a condition of plenty for all, and that competitive energies were channelled into commerce rather than conflict. Scholars have long argued that these rains shaped the origins of the urban Harappan societies, which emerged from Neolithic villages around 2600 BC. It now appears that this rainfall began to slowly taper off in the third millennium, at just the point that the Harappan cities began to develop. Thus it seems that this "first urbanization" in South Asia was the initial response of the Indus Valley peoples to the beginning of Late Holocene aridification. These cities were maintained for 300 to 400 years and then gradually abandoned as the Harappan peoples resettled in scattered villages in the eastern range of their territories, into the Punjab and the Ganges Valley ... .” — Brooke (2015)[24]: 17  (footnotes)
    (a) Giosan, Liviu; et al. (2012). "Fluvial landscapes of the Harappan Civilization". Proceedings of the National Academy of Sciences, USA. 102 (26): E1688–E1694. Bibcode:2012PNAS..109E1688G. doi:10.1073/pnas.1112743109. PMC 3387054. PMID 22645375;
    (b) Ponton, Camilo (2012). "Holocene aridification of India". Geophysical Research Letters. 39 (3): L03704. Bibcode:2012GeoRL..39.3704P. doi:10.1029/2011GL050722. hdl:1912/5100. S2CID 140604921;
    (c) Rashid, Harunur; et al. (2011). "Late glacial to Holocene Indian summer monsoon variability based upon sediment records taken from the Bay of Bengal" (PDF). Terrestrial, Atmospheric and Oceanic Sciences. 22 (2): 215–228. Bibcode:2011TAOS...22..215R. doi:10.3319/TAO.2010.09.17.02(TibXS);
    (d) Madella, Marco; Fuller, Dorian Q. (2006). "Palaeoecology and the Harappan civilisation of south Asia: A reconsideration". Quaternary Science Reviews. 25 (11–12): 1283–1301. Bibcode:2006QSRv...25.1283M. doi:10.1016/j.quascirev.2005.10.012.
    Compare with the very different interpretations in Possehl (2002),[25] and Staubwasser et al. (2003),[26] Bar-Matthews & Avner Ayalon (2015).[27]

rajeshkochhar.com

researchgate.net

semanticscholar.org

api.semanticscholar.org

  • From Brooke (2015):[24] “The story in Harappan India was somewhat different (see Figure 111.3). The Bronze Age village and urban societies of the Indus Valley are some-thing of an anomaly, in that archaeologists have found little indication of local defence and regional warfare. It would seem that the bountiful monsoon rainfall of the Early to Mid-Holocene had forged a condition of plenty for all, and that competitive energies were channelled into commerce rather than conflict. Scholars have long argued that these rains shaped the origins of the urban Harappan societies, which emerged from Neolithic villages around 2600 BC. It now appears that this rainfall began to slowly taper off in the third millennium, at just the point that the Harappan cities began to develop. Thus it seems that this "first urbanization" in South Asia was the initial response of the Indus Valley peoples to the beginning of Late Holocene aridification. These cities were maintained for 300 to 400 years and then gradually abandoned as the Harappan peoples resettled in scattered villages in the eastern range of their territories, into the Punjab and the Ganges Valley ... .” — Brooke (2015)[24]: 17  (footnotes)
    (a) Giosan, Liviu; et al. (2012). "Fluvial landscapes of the Harappan Civilization". Proceedings of the National Academy of Sciences, USA. 102 (26): E1688–E1694. Bibcode:2012PNAS..109E1688G. doi:10.1073/pnas.1112743109. PMC 3387054. PMID 22645375;
    (b) Ponton, Camilo (2012). "Holocene aridification of India". Geophysical Research Letters. 39 (3): L03704. Bibcode:2012GeoRL..39.3704P. doi:10.1029/2011GL050722. hdl:1912/5100. S2CID 140604921;
    (c) Rashid, Harunur; et al. (2011). "Late glacial to Holocene Indian summer monsoon variability based upon sediment records taken from the Bay of Bengal" (PDF). Terrestrial, Atmospheric and Oceanic Sciences. 22 (2): 215–228. Bibcode:2011TAOS...22..215R. doi:10.3319/TAO.2010.09.17.02(TibXS);
    (d) Madella, Marco; Fuller, Dorian Q. (2006). "Palaeoecology and the Harappan civilisation of south Asia: A reconsideration". Quaternary Science Reviews. 25 (11–12): 1283–1301. Bibcode:2006QSRv...25.1283M. doi:10.1016/j.quascirev.2005.10.012.
    Compare with the very different interpretations in Possehl (2002),[25] and Staubwasser et al. (2003),[26] Bar-Matthews & Avner Ayalon (2015).[27]
  • Clift et al. 2012. Clift, Peter D.; Carter, Andrew; Giosan, Liviu; Durcan, Julie; et al. (2012), "U-Pb zircon dating evidence for a Pleistocene Sarasvati River and capture of the Yamuna River", Geology, 40 (3): 211–214, Bibcode:2012Geo....40..211C, doi:10.1130/g32840.1, S2CID 130765891
  • Dave et al. 2019. Dave, Aditi Krishna; Courty, Marie-Agnes; Fitzsimmons, Kathryn E.; Singhvia, Ashok Kumar (2019), "Revisiting the contemporaneity of a mighty river and the Harappans: Archaeological, stratigraphic and chronometric constraints", Quaternary Geochronology, 49: 230–235, Bibcode:2019QuGeo..49..230D, doi:10.1016/j.quageo.2018.05.002, S2CID 134501741
  • Sinha, Singh & Tandon 2020, p. 240. Sinha, Rajiv; Singh, Ajit; Tandon, Sampat K. (25 July 2020), "Fluvial archives of north and northwestern India as recorders of climatic signatures in the late Quaternary: review and assessment", Current Science, 119 (2): 232, doi:10.18520/cs/v119/i2/232-243, S2CID 239534661
  • Staubwasser, Michael; et al. (2003). "Climate change at the 4.2 ka BP termination of the Indus Valley Civilization and Holocene south Asian monsoon variability". Geophysical Research Letters. 30 (8): 1425. Bibcode:2003GeoRL..30.1425S. doi:10.1029/2002GL016822. S2CID 129178112.
  • Demkina 2017. Demkina, T.S. (2017), "Paleoecological crisis in the steppes of the Lower Volga region in the Middle of the Bronze Age (III–II centuries BC)", Eurasian Soil Science, 50 (7): 791–804, Bibcode:2017EurSS..50..791D, doi:10.1134/S1064229317070018, S2CID 133638705
  • Possehl 1997. Possehl, Gregory L. (December 1997). "The transformation of the Indus Civilization". Journal of World Prehistory. 11 (4): 425–472. doi:10.1007/bf02220556. JSTOR 25801118. S2CID 161129625.

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  • "Hakra". Totally Explained. Archived from the original on 12 July 2012. Retrieved 20 August 2009.

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