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Egypt
Civilization and Geology
Hassan Z. Harraz
hharraz2006@yahoo.com
TYPES OF ROCKS - The Rock Cycle
The
Geologic
Time
Scale
EGYPT
BEDROCK
BEDROCK OF
EGYPT
Top Layer
Limestones
Intermediate Layer
Sandstone
The Basement Complex
Igneous Rocks
And
Metamorphic
BEDROCK OF
EGYPT
Top Layer
Limestones
Intermediate Layer
Sandstone
The Basement Complex
Igneous Rocks
And
Metamorphic
BEDROCK OF
EGYPT
Top Layer
Limestones
Intermediate Layer
Sandstone
The Basement Complex
Igneous Rocks
And
Metamorphic
BEDROCK OF
EGYPT
Top Layer
Limestones
Intermediate Layer
Sandstone
The Basement Complex
Igneous Rocks
And
Metamorphic
BEDROCK OF
EGYPT
Top Layer
Limestones
Intermediate Layer
Sandstone
The Basement Complex
Igneous Rocks
And
Metamorphic
According to the “Rock Cycle,”
New IGNEOUS ROCK can be made from:
A.) Sedimentary Rock
B.) Metamorphic Rock
C.) Older Igneous Rock
D.) All of the Above
E.) Only A and B
F.) None of the Above –
It Only Comes from the Mantle
The
Geologic
Time
Scale
Precambrian
0.59 billion
(590 million)
to
4.6 billion
years ago
SW (West Nile Craton)
2 billion years ago
Eastern Desert and Sinai
0.5 to 1 billion years ago
The
BASEMENT
COMPLEX
The Past
THE BASEMENT COMPLEX
Continuous Beneath The Entire Country
Southwest at
Gebel Uweinat
THE BASEMENT COMPLEX
Continuous Beneath The Entire Country
Southwest at
Gebel Uweinat
Scattered southern
portions of the
Western Desert
THE BASEMENT COMPLEX
Continuous Beneath The Entire Country
Southern
Portion of
the Sinai
Southwest at
Gebel Uweinat
Scattered southern
portions of the
Western Desert
THE BASEMENT COMPLEX
Continuous Beneath The Entire Country
High
Mountains
Eastern
Desert
Southern
Portion of
the Sinai
Southwest at
Gebel Uweinat
Scattered southern
portions of the
Western Desert
THE BASEMENT COMPLEX
Continuous Beneath The Entire Country
High
Mountains
Eastern
Desert
Southern
Portion of
the Sinai
Aswan at the
First Nile Cataract
Southwest at
Gebel Uweinat
Scattered southern
portions of the
Western Desert
BASEMENT COMPLEX
Sinai Area
Metamorphic Rocks Cut
by Igneous Intrusions
Photos by: Alan Kehew
THE PRECAMBRIAN ROCKS OF EGYPT
ARE COMPOSED OF:
A.) Igneous Rocks
B.) Metamorphic Rocks
C.) Sedimentary Rocks
D.) All of the Above
E.) Only A and B
INTERMEDIATE ROCK UNITS
Paleocene – 55 to 65 million years ago
Shale (mud)
Late Cretaceous – 80 to 90 million years ago
Fine, White Limestone (often called Chalk)
Shale (mud)
Nubian Sandstone
The Past
Figure 3-39ACONTINENTAL DRIFT Late Paleozoic
Tethys Sea
Late Paleozoic
INTERMEDIATE ROCK UNITS
Paleocene – 55 to 65 million years ago
Shale (mud)
Late Cretaceous – 80 to 90 million years ago
Fine, White Limestone (often called Chalk)
Shale (mud)
Nubian Sandstone
The
Geologic
Time
Scale
late Cretaceous
80 million
to
90 million
years ago
INTERMEDIATE
ROCK UNITS
Nubian Sandstone
INTERMEDIATE ROCK UNITS
Nubian Sandstone
• medium-sized silica gains
• loosely cemented with quartz and iron oxide
(ferruginous) cements and chlorite clays
• highly porous and friable
easy to quarry and carve
• strength – sparse
but always present due to quartz cement
• iron produces yellow-red-brown color
• manganese sometimes present produces
purple to black color
EGYPT
BEDROCK
Nubian Sandstone
exposed in southern Egypt (1/3 of country)
and in northern Nubia (Sudan)
THE NUBIAN SANDSTONE OF EGYPT IS:
A.) Well Cemented, Very Dense and Hard
B.) Moderately Cemented and Reasonably
Durable due to Quartz Cement
C.) Poorly Cemented and NO Use
as a Building Stone
D.) Only Found as Loose Sand in Wide-spread
Sand Sheets throughout the Western Desert
E.) Never Exposed at the Surface
The
Geologic
Time
Scale
late Cretaceous
80 million
to
90 million
years ago
INTERMEDIATE
ROCK UNITS
Nubian Sandstone
Basement Complex
UNCONFORMITY
(MISSING ROCK)
Basement Complex
Uplifted, Weathered
and Eroded Away
INTERMEDIATE ROCK UNITS
Paleocene – 55 to 65 million years ago
Shale (mud)
Late Cretaceous – 80 to 90 million years ago
Fine, White Limestone (often called Chalk)
Shale (mud)
Nubian Sandstone
INTERMEDIATE ROCK UNITS
Paleocene – 55 to 65 million years ago
Shale (mud)
Late Cretaceous – 80 to 90 million years ago
Fine, White Limestone (often called Chalk)
Shale (mud)
Nubian Sandstone
The
Geologic
Time
Scale
late Cretaceous
80 million
to
90 million
years ago
INTERMEDIATE
ROCK UNITS
Fine, White Limestone
(often called Chalk)
overlays a layer of
Shale
Nubian Sandstone
Facies Development
Marine Transgressions
and Regressions
General Model
INTERMEDIATE ROCK UNITS
Paleocene – 55 to 65 million years ago
Shale (mud)
Late Cretaceous – 80 to 90 million years ago
Fine, White Limestone (often called Chalk)
Shale (mud)
Nubian Sandstone
INTERMEDIATE ROCK UNITS
Paleocene – 55 to 65 million years ago
Shale (mud)
Late Cretaceous – 80 to 90 million years ago
Fine, White Limestone (often called Chalk)
Shale (mud)
Nubian Sandstone
The
Geologic
Time
Scale
Paleocene
55 million
to
65 million
years ago
INTERMEDIATE
ROCK UNITS
Paleocene Shale
(Text book refers to this
as part of the Cretaceous
Limestone and Shale Package)
Facies Development
Marine Transgressions
and Regressions
General Model
EGYPT
BEDROCK
Paleocene Shale
Cretaceous Shale
and Limestone
UPPER ROCK UNITS
Present
• Alluvium deposited in Nile River Valley, Sand Sheets and
Dunes in the Western Desert and Sinai
Pliocene 5.1 to 2 million years ago
• Seas retreat - Erosion and Denudation
Miocene 24.6 to 5.1 million years ago
• Limestones
Oligocene 38 to 24.6 million years ago
• Regional Tectonics as Red Sea begins to open
• Basalt sheet flows
• Conglomerates along coast
Eocene – 38 million to 55 million years ago
• Limestone
UPPER ROCK UNITS
Present
• Alluvium deposited in Nile River Valley, Sand Sheets and
Dunes in the Western Desert and Sinai
Pliocene 5.1 to 2 million years ago
• Seas retreat - Erosion and Denudation
Miocene 24.6 to 5.1 million years ago
• Limestones
Oligocene 38 to 24.6 million years ago
• Regional Tectonics as Red Sea begins to open
• Basalt sheet flows
Conglomerates along coast
Eocene – 38 million to 55 million years ago
• Limestone
The
Geologic
Time
Scale
Eocene
38 million
to
55 million
years ago
UPPER
ROCK UNITS
Eocene
Limestone
Giza Plateau and
Pyramids are composed
of Eocene Limestone
UPPER ROCK UNITS
Eocene – 38 million to 55 million years ago
Limestone
• thickness varies due to deposition on folded
substrate (north-south compression at end of
Cretaceous Period)
• composition varies due to deposition during
transgression of Tethys Sea
• various members (sub-layers) can be distinguished
• units become thicker basinward toward the north
due to that portion always being covered by
the transgressing Tethys Sea
• units dip gently to the north due to
post-depositional tectonic uplift
EGYPT
BEDROCK
Eocene Limestone exposed in
central Egypt north to Cairo
LIMESTONE WOULD BE EXPECTED TO
OCCUR ______________ THE ROCK
SEQUENCE DUE TO A TRANSGRESSIVE
EVENT (RISE IN SEA LEVEL)
A.) at the Top of
B.) at the Bottom of
C.) at the Middle of
D.) Throughout
E.) Nowhere in
UPPER ROCK UNITS
Present
• Alluvium deposited in Nile River Valley, Sand Sheets and
Dunes in the Western Desert and Sinai
Pliocene 5.1 to 2 million years ago
• Seas retreat - Erosion and Denudation
Miocene 24.6 to 5.1 million years ago
• Limestones
Oligocene 38 to 24.6 million years ago
• Regional Tectonics as Red Sea begins to open
• Basalt sheet flows
• Conglomerates along coast
Eocene – 38 million to 55 million years ago
• Limestone
The
Geologic
Time
Scale
Oligocene
38 to 24.6 million
years ago
UPPER
ROCK UNITS
• Regional Tectonics as Red
Sea begins to open
• Basalt sheet flows in SW
near Gebel Uweinat,
Gilf Kebir, north of
Fayum to NE of Cairo
• Tethys Sea coast-latitude of
Fayum Depression &
Cairo
• Conglomerates with land
animal fossils and large
tree trunks deposited in
streams along coast
EGYPT
BEDROCK
Basalt sheet
flows in SW near
Gebel Uweinat
EGYPT
BEDROCK
Basalt sheet flows
near Gilf Kebir
Basalt sheet
flows in SW near
Gebel Uweinat
EGYPT
BEDROCK
Basalt sheet flows
near Gilf Kebir
Basalt sheet
flows in SW near
Gebel Uweinat
Basalt sheet flows
north of Fayum to
NE of Cairo
EGYPT
BEDROCK
Tethys Sea coast at
latitude of Fayum
Depression & Cairo
Conglomerates with
land animal fossils
and large tree trunks
deposited in streams
along coast
UPPER ROCK UNITS
Present
• Alluvium deposited in Nile River Valley, Sand Sheets and
Dunes in the Western Desert and Sinai
Pliocene 5.1 to 2 million years ago
• Seas retreat - Erosion and Denudation
Miocene 24.6 to 5.1 million years ago
• Limestones
Oligocene 38 to 24.6 million years ago
• Regional Tectonics as Red Sea begins to open
• Basalt sheet flows
• Conglomerates along coast
Eocene – 38 million to 55 million years ago
• Limestone
The
Geologic
Time
Scale
Miocene
24.6 to 5.1 million
years ago
UPPER
ROCK UNITS
Limestones deposited south
of modern Mediterranean
Sea coast and Gulf of Suez
coast (early-mid Miocene)
EGYPT
BEDROCK
Limestones deposited south of modern
Mediterranean Sea coast and Gulf of
Suez coast (early-mid Miocene)
UPPER ROCK UNITS
Present
• Alluvium deposited in Nile River Valley, Sand Sheets and
Dunes in the Western Desert and Sinai
Pliocene 5.1 to 2 million years ago
• Seas retreat - Erosion and Denudation
Miocene 24.6 to 5.1 million years ago
• Limestones
Oligocene 38 to 24.6 million years ago
• Regional Tectonics as Red Sea begins to open
• Basalt sheet flows
• Conglomerates along coast
Eocene – 38 million to 55 million years ago
• Limestone
TRUE or FLASE
Extensive, area-wide erosion took place during
the Pliocene due to a regression (relative drop in
sea level or tectonic rise in land elevation)
The
Geologic
Time
Scale
Pliocene
5.1 to 2 million
years ago
UPPER
ROCK UNITS
• Seas retreated
probably land uplifted
• Erosion and denudation
variable throughout
Egypt
• Bedrock exposed as
erosion proceeded
UPPER ROCK UNITS
Present
• Alluvium deposited in Nile River Valley, Sand Sheets and
Dunes in the Western Desert and Sinai
Pliocene 5.1 to 2 million years ago
• Seas retreat - Erosion and Denudation
Miocene 24.6 to 5.1 million years ago
• Limestones
Oligocene 38 to 24.6 million years ago
• Regional Tectonics as Red Sea begins to open
• Basalt sheet flows
• Conglomerates along coast
Eocene – 38 million to 55 million years ago
• Limestone
The
Geologic
Time
Scale
Present
UPPER
ROCK UNITS
Alluvium deposited in Nile
River Valley, Sand Sheets
and Dunes in the Western
Desert and Sinai
EGYPT
BEDROCK
Alluvium deposited
in Nile River Valley
Sand Sheets and
Dunes deposited
in the Western
Desert
Sand Sheets
and Dunes
deposited in
the Sinai
Delta Growth
Egypt
Civilization and Geology

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Egypt Civilization and Geology

  • 1. Egypt Civilization and Geology Hassan Z. Harraz hharraz2006@yahoo.com
  • 2. TYPES OF ROCKS - The Rock Cycle
  • 5. BEDROCK OF EGYPT Top Layer Limestones Intermediate Layer Sandstone The Basement Complex Igneous Rocks And Metamorphic
  • 6. BEDROCK OF EGYPT Top Layer Limestones Intermediate Layer Sandstone The Basement Complex Igneous Rocks And Metamorphic
  • 7. BEDROCK OF EGYPT Top Layer Limestones Intermediate Layer Sandstone The Basement Complex Igneous Rocks And Metamorphic
  • 8. BEDROCK OF EGYPT Top Layer Limestones Intermediate Layer Sandstone The Basement Complex Igneous Rocks And Metamorphic
  • 9. BEDROCK OF EGYPT Top Layer Limestones Intermediate Layer Sandstone The Basement Complex Igneous Rocks And Metamorphic
  • 10. According to the “Rock Cycle,” New IGNEOUS ROCK can be made from: A.) Sedimentary Rock B.) Metamorphic Rock C.) Older Igneous Rock D.) All of the Above E.) Only A and B F.) None of the Above – It Only Comes from the Mantle
  • 11. The Geologic Time Scale Precambrian 0.59 billion (590 million) to 4.6 billion years ago SW (West Nile Craton) 2 billion years ago Eastern Desert and Sinai 0.5 to 1 billion years ago The BASEMENT COMPLEX
  • 13. THE BASEMENT COMPLEX Continuous Beneath The Entire Country Southwest at Gebel Uweinat
  • 14. THE BASEMENT COMPLEX Continuous Beneath The Entire Country Southwest at Gebel Uweinat Scattered southern portions of the Western Desert
  • 15. THE BASEMENT COMPLEX Continuous Beneath The Entire Country Southern Portion of the Sinai Southwest at Gebel Uweinat Scattered southern portions of the Western Desert
  • 16. THE BASEMENT COMPLEX Continuous Beneath The Entire Country High Mountains Eastern Desert Southern Portion of the Sinai Southwest at Gebel Uweinat Scattered southern portions of the Western Desert
  • 17. THE BASEMENT COMPLEX Continuous Beneath The Entire Country High Mountains Eastern Desert Southern Portion of the Sinai Aswan at the First Nile Cataract Southwest at Gebel Uweinat Scattered southern portions of the Western Desert
  • 18. BASEMENT COMPLEX Sinai Area Metamorphic Rocks Cut by Igneous Intrusions Photos by: Alan Kehew
  • 19.
  • 20.
  • 21.
  • 22.
  • 23.
  • 24. THE PRECAMBRIAN ROCKS OF EGYPT ARE COMPOSED OF: A.) Igneous Rocks B.) Metamorphic Rocks C.) Sedimentary Rocks D.) All of the Above E.) Only A and B
  • 25. INTERMEDIATE ROCK UNITS Paleocene – 55 to 65 million years ago Shale (mud) Late Cretaceous – 80 to 90 million years ago Fine, White Limestone (often called Chalk) Shale (mud) Nubian Sandstone
  • 27. Figure 3-39ACONTINENTAL DRIFT Late Paleozoic Tethys Sea Late Paleozoic
  • 28. INTERMEDIATE ROCK UNITS Paleocene – 55 to 65 million years ago Shale (mud) Late Cretaceous – 80 to 90 million years ago Fine, White Limestone (often called Chalk) Shale (mud) Nubian Sandstone
  • 29. The Geologic Time Scale late Cretaceous 80 million to 90 million years ago INTERMEDIATE ROCK UNITS Nubian Sandstone
  • 30. INTERMEDIATE ROCK UNITS Nubian Sandstone • medium-sized silica gains • loosely cemented with quartz and iron oxide (ferruginous) cements and chlorite clays • highly porous and friable easy to quarry and carve • strength – sparse but always present due to quartz cement • iron produces yellow-red-brown color • manganese sometimes present produces purple to black color
  • 31. EGYPT BEDROCK Nubian Sandstone exposed in southern Egypt (1/3 of country) and in northern Nubia (Sudan)
  • 32. THE NUBIAN SANDSTONE OF EGYPT IS: A.) Well Cemented, Very Dense and Hard B.) Moderately Cemented and Reasonably Durable due to Quartz Cement C.) Poorly Cemented and NO Use as a Building Stone D.) Only Found as Loose Sand in Wide-spread Sand Sheets throughout the Western Desert E.) Never Exposed at the Surface
  • 33. The Geologic Time Scale late Cretaceous 80 million to 90 million years ago INTERMEDIATE ROCK UNITS Nubian Sandstone Basement Complex UNCONFORMITY (MISSING ROCK) Basement Complex Uplifted, Weathered and Eroded Away
  • 34. INTERMEDIATE ROCK UNITS Paleocene – 55 to 65 million years ago Shale (mud) Late Cretaceous – 80 to 90 million years ago Fine, White Limestone (often called Chalk) Shale (mud) Nubian Sandstone
  • 35. INTERMEDIATE ROCK UNITS Paleocene – 55 to 65 million years ago Shale (mud) Late Cretaceous – 80 to 90 million years ago Fine, White Limestone (often called Chalk) Shale (mud) Nubian Sandstone
  • 36. The Geologic Time Scale late Cretaceous 80 million to 90 million years ago INTERMEDIATE ROCK UNITS Fine, White Limestone (often called Chalk) overlays a layer of Shale Nubian Sandstone
  • 37. Facies Development Marine Transgressions and Regressions General Model
  • 38. INTERMEDIATE ROCK UNITS Paleocene – 55 to 65 million years ago Shale (mud) Late Cretaceous – 80 to 90 million years ago Fine, White Limestone (often called Chalk) Shale (mud) Nubian Sandstone
  • 39. INTERMEDIATE ROCK UNITS Paleocene – 55 to 65 million years ago Shale (mud) Late Cretaceous – 80 to 90 million years ago Fine, White Limestone (often called Chalk) Shale (mud) Nubian Sandstone
  • 40. The Geologic Time Scale Paleocene 55 million to 65 million years ago INTERMEDIATE ROCK UNITS Paleocene Shale (Text book refers to this as part of the Cretaceous Limestone and Shale Package)
  • 41. Facies Development Marine Transgressions and Regressions General Model
  • 43. UPPER ROCK UNITS Present • Alluvium deposited in Nile River Valley, Sand Sheets and Dunes in the Western Desert and Sinai Pliocene 5.1 to 2 million years ago • Seas retreat - Erosion and Denudation Miocene 24.6 to 5.1 million years ago • Limestones Oligocene 38 to 24.6 million years ago • Regional Tectonics as Red Sea begins to open • Basalt sheet flows • Conglomerates along coast Eocene – 38 million to 55 million years ago • Limestone
  • 44. UPPER ROCK UNITS Present • Alluvium deposited in Nile River Valley, Sand Sheets and Dunes in the Western Desert and Sinai Pliocene 5.1 to 2 million years ago • Seas retreat - Erosion and Denudation Miocene 24.6 to 5.1 million years ago • Limestones Oligocene 38 to 24.6 million years ago • Regional Tectonics as Red Sea begins to open • Basalt sheet flows Conglomerates along coast Eocene – 38 million to 55 million years ago • Limestone
  • 45. The Geologic Time Scale Eocene 38 million to 55 million years ago UPPER ROCK UNITS Eocene Limestone Giza Plateau and Pyramids are composed of Eocene Limestone
  • 46. UPPER ROCK UNITS Eocene – 38 million to 55 million years ago Limestone • thickness varies due to deposition on folded substrate (north-south compression at end of Cretaceous Period) • composition varies due to deposition during transgression of Tethys Sea • various members (sub-layers) can be distinguished • units become thicker basinward toward the north due to that portion always being covered by the transgressing Tethys Sea • units dip gently to the north due to post-depositional tectonic uplift
  • 47. EGYPT BEDROCK Eocene Limestone exposed in central Egypt north to Cairo
  • 48. LIMESTONE WOULD BE EXPECTED TO OCCUR ______________ THE ROCK SEQUENCE DUE TO A TRANSGRESSIVE EVENT (RISE IN SEA LEVEL) A.) at the Top of B.) at the Bottom of C.) at the Middle of D.) Throughout E.) Nowhere in
  • 49. UPPER ROCK UNITS Present • Alluvium deposited in Nile River Valley, Sand Sheets and Dunes in the Western Desert and Sinai Pliocene 5.1 to 2 million years ago • Seas retreat - Erosion and Denudation Miocene 24.6 to 5.1 million years ago • Limestones Oligocene 38 to 24.6 million years ago • Regional Tectonics as Red Sea begins to open • Basalt sheet flows • Conglomerates along coast Eocene – 38 million to 55 million years ago • Limestone
  • 50. The Geologic Time Scale Oligocene 38 to 24.6 million years ago UPPER ROCK UNITS • Regional Tectonics as Red Sea begins to open • Basalt sheet flows in SW near Gebel Uweinat, Gilf Kebir, north of Fayum to NE of Cairo • Tethys Sea coast-latitude of Fayum Depression & Cairo • Conglomerates with land animal fossils and large tree trunks deposited in streams along coast
  • 51. EGYPT BEDROCK Basalt sheet flows in SW near Gebel Uweinat
  • 52. EGYPT BEDROCK Basalt sheet flows near Gilf Kebir Basalt sheet flows in SW near Gebel Uweinat
  • 53. EGYPT BEDROCK Basalt sheet flows near Gilf Kebir Basalt sheet flows in SW near Gebel Uweinat Basalt sheet flows north of Fayum to NE of Cairo
  • 54. EGYPT BEDROCK Tethys Sea coast at latitude of Fayum Depression & Cairo Conglomerates with land animal fossils and large tree trunks deposited in streams along coast
  • 55. UPPER ROCK UNITS Present • Alluvium deposited in Nile River Valley, Sand Sheets and Dunes in the Western Desert and Sinai Pliocene 5.1 to 2 million years ago • Seas retreat - Erosion and Denudation Miocene 24.6 to 5.1 million years ago • Limestones Oligocene 38 to 24.6 million years ago • Regional Tectonics as Red Sea begins to open • Basalt sheet flows • Conglomerates along coast Eocene – 38 million to 55 million years ago • Limestone
  • 56. The Geologic Time Scale Miocene 24.6 to 5.1 million years ago UPPER ROCK UNITS Limestones deposited south of modern Mediterranean Sea coast and Gulf of Suez coast (early-mid Miocene)
  • 57. EGYPT BEDROCK Limestones deposited south of modern Mediterranean Sea coast and Gulf of Suez coast (early-mid Miocene)
  • 58. UPPER ROCK UNITS Present • Alluvium deposited in Nile River Valley, Sand Sheets and Dunes in the Western Desert and Sinai Pliocene 5.1 to 2 million years ago • Seas retreat - Erosion and Denudation Miocene 24.6 to 5.1 million years ago • Limestones Oligocene 38 to 24.6 million years ago • Regional Tectonics as Red Sea begins to open • Basalt sheet flows • Conglomerates along coast Eocene – 38 million to 55 million years ago • Limestone
  • 59. TRUE or FLASE Extensive, area-wide erosion took place during the Pliocene due to a regression (relative drop in sea level or tectonic rise in land elevation)
  • 60. The Geologic Time Scale Pliocene 5.1 to 2 million years ago UPPER ROCK UNITS • Seas retreated probably land uplifted • Erosion and denudation variable throughout Egypt • Bedrock exposed as erosion proceeded
  • 61. UPPER ROCK UNITS Present • Alluvium deposited in Nile River Valley, Sand Sheets and Dunes in the Western Desert and Sinai Pliocene 5.1 to 2 million years ago • Seas retreat - Erosion and Denudation Miocene 24.6 to 5.1 million years ago • Limestones Oligocene 38 to 24.6 million years ago • Regional Tectonics as Red Sea begins to open • Basalt sheet flows • Conglomerates along coast Eocene – 38 million to 55 million years ago • Limestone
  • 62. The Geologic Time Scale Present UPPER ROCK UNITS Alluvium deposited in Nile River Valley, Sand Sheets and Dunes in the Western Desert and Sinai
  • 63. EGYPT BEDROCK Alluvium deposited in Nile River Valley Sand Sheets and Dunes deposited in the Western Desert Sand Sheets and Dunes deposited in the Sinai Delta Growth