مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

2,271
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

4

Information Journal Paper

Title

CHARACTERISTIC OF KAFST LANDSCAPE OF WATERSHED BASIN OF KARDEH-RIVER (EAST OF KOPEH-DAGH ZONE)

Pages

  1-16

Abstract

 There are relative many learst massive in the Kopeh-dagh mountains. Every learst geomorphological research about these learstterrain, learstaquifer, relationship between korst forms, hydraulic learst system, land use and management of environment can be usefull. The learstmassive of leardehis a typefrom the semi-and arid- mountains kind. In the lower part of the watershed basin there are five wells that have been drilled in limestone and the drink water of west of Mashhad is supplied by the water resourvier of the leardeh-dam.About the 80 percent of watersupply for the people from the watershed basin is supplied by the springs and the other 20 percent by the rivers. From this reason the identificatiorl of learstic land forms, vulnerability of hydraulic system and finally the correct land use planning and management of water resources in this learsticterritory is necessary. The main carbonate and carbonate-dolomite of the Kardeh-watershed basin are the jurassic formations of Marzdaran (JMZ1) and Marzdaran (JMZ2) which have thick massive limestone beds. The development of the secQndarypermeable of the limestone (in forms of a networkof joints andfaultings) and the learstification processes are the most important factors of learstification of stones. The karstic forms that are made in these stones are: microkarren, learren,dolines,sinkholes, caves and other learsticforms.

Cites

References

  • No record.
  • Cite

    APA: Copy

    ESHGHI, ALI REZA, & SERVATI, M.R.. (2004). CHARACTERISTIC OF KAFST LANDSCAPE OF WATERSHED BASIN OF KARDEH-RIVER (EAST OF KOPEH-DAGH ZONE). GEOGRAPHICAL RESEARCH QUARTERLY, 36(48), 1-16. SID. https://sid.ir/paper/5479/en

    Vancouver: Copy

    ESHGHI ALI REZA, SERVATI M.R.. CHARACTERISTIC OF KAFST LANDSCAPE OF WATERSHED BASIN OF KARDEH-RIVER (EAST OF KOPEH-DAGH ZONE). GEOGRAPHICAL RESEARCH QUARTERLY[Internet]. 2004;36(48):1-16. Available from: https://sid.ir/paper/5479/en

    IEEE: Copy

    ALI REZA ESHGHI, and M.R. SERVATI, “CHARACTERISTIC OF KAFST LANDSCAPE OF WATERSHED BASIN OF KARDEH-RIVER (EAST OF KOPEH-DAGH ZONE),” GEOGRAPHICAL RESEARCH QUARTERLY, vol. 36, no. 48, pp. 1–16, 2004, [Online]. Available: https://sid.ir/paper/5479/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top
    telegram sharing button
    whatsapp sharing button
    linkedin sharing button
    twitter sharing button
    email sharing button
    email sharing button
    email sharing button
    sharethis sharing button