Skip to main content

Saudi Arabia, Persian Gulf Coast

  • Reference work entry
Encyclopedia of the World's Coastal Landforms
  • 209 Accesses

Introduction

The Kingdom of Saudi Arabia has an Persian Gulf coast about 700 km long. The Arabian Peninsula has a steep western escarpment rising to 1,500–3,000 m at the edge of a plateau that declines gradually eastward, flattening to a broad coastal plain. Longer watercourses run eastward, but there are no permanent rivers, and the landscape is largely desert.

The climate is hot and arid. The Persian Gulf has summer temperatures ranging from 32°C in the south to 20°C in the north, falling to between 22 and 16°C in winter. Salinity is about 40 parts per thousand (ppt) in the south, but diminishes off the inflowing rivers in the north. Coral reefs are extensive in the southern part of the Persian Gulf, but become sparse in the cooler and more turbid northern regions. Mangroves are found in sheltered sites behind fringing reefs and beside inlets.

On the Persian Gulf coast the mean spring tide range is about 1.5 m and a sandy shore is exposed at low tide. Seas in the Persian Gulf are...

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 999.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Hardcover Book
USD 549.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

References

  • Al-Sayari SS, Zotl JG (eds) (1978) The quaternary period in Saudi Arabia. Springer-Verlag, New York

    Google Scholar 

  • Behairy AKA (1983) Marine transgressions in the west coast of Saudi Arabia (Red Sea) between mid-Pleistocene and Present. Marine Geol. 52:M25–M31

    Article  Google Scholar 

  • Fryberger SG, Al-Sari AM, Clisham TJ (1983) Eolian dune, interdune, sand sheet and siliciclastic sabkha sediment of an offshore prograding sand sea, Dharan area, Saudi Arabia. Bull Am Assoc Petrol Geol 67:280–312

    Google Scholar 

  • Gvirtzman G (1977) Morphology of the Red Sea fringing reefs. Memoirs, Bureau of Geological and Mining Research, Paris, 89:480–491

    Google Scholar 

  • Johnson DH, Kamal MR, Pierson GO, Ramsay JB (1978) Sabkhas of eastern Saudi Arabia. In: Al-Sayari SS and Zotl JG (eds) The quaternary period in Saudi Arabia. Springer-Verlag, New York, pp 84–93

    Google Scholar 

  • McClure HA, Vita-Finzi C (1982) Holocene shorelines and tectonic movements in eastern Saudi Arabia. Tectonophysics 85:T37–T43

    Article  Google Scholar 

  • Shinn EA (1969) Submarine lithification of Holocene carbonate sediment in the Persian Gulf. Sedimentology 12:109–144

    Article  Google Scholar 

  • Sugden W (1963) Some aspects of sedimentation in the Persian Gulf. J Sediment Petrol 33:355–364

    Google Scholar 

  • Vita-Finzi C (1991) Dating of an uplifted shoreline in eastern Saudi Arabia. Tectonomorphology 194:197–201

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2010 Springer Science+Business Media B.V.

About this entry

Cite this entry

Bird, E. (2010). Saudi Arabia, Persian Gulf Coast. In: Bird, E.C.F. (eds) Encyclopedia of the World's Coastal Landforms. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-8639-7_194

Download citation

Publish with us

Policies and ethics