The process of transportation of petroleum from its place of origin, the source rock, to its place of accumulation into the reservoir up to the trap is termed as Migration.
This is my presentation on the tectonic control of sediments.
It includes the effects of tectonics either direct or indirect on sediments and sedimentation.
Sedimentation along various plate boundaries.
Few examples as evidence from Pakistan (the Siwalik Group) and Argentina (Fiambala Basin)
The process of transportation of petroleum from its place of origin, the source rock, to its place of accumulation into the reservoir up to the trap is termed as Migration.
This is my presentation on the tectonic control of sediments.
It includes the effects of tectonics either direct or indirect on sediments and sedimentation.
Sedimentation along various plate boundaries.
Few examples as evidence from Pakistan (the Siwalik Group) and Argentina (Fiambala Basin)
Origin and Abundance of elements in the Solar system and in the Earth and its...AkshayRaut51
Definition of Elements and atom
Origin of Universe
Theories of origin of Solar system and Earth
Chemical Composition of Planets
Chemical Composition of Earth
Chemical composition of Meteorites
Abundance of Elements
THE PRESENCE AND VARIETY OF A PARTICULAR PLANTS
SPECIES IN THE AREA OF MINERALISATION HAVE BEEN RECOGNISED AS A GUIDE TO LOCATING ORE, METHOD,UNIVERSAL INDICATORS , UNIVERSAL INDICATOR ,LOCAL INDICATOR
Mineral deposits known to occur in Egypt; Classification of mineral deposit in Egypt, Possible Areas for Investment in Mineral Industry in Egypt, Mineral Commodities
Limestone;Industrial Uses of Limestone ; Lime; Lime Cycle; Production of Lime; Classification of Hydrated Lime IS 712-1973; Purposes for the Utilize of Lime; Soda Ash;Solvay process for the manufacture of Soda Ash; Purposes for the Utilize of Soda Ash; Gypsum; Calcination of Gypsum; Hardening of Plaster; Magnesium; Production Of Magnesium from seawater and dolomite; Process for production Magnesium hydroxide and Calcium chloride from Dolomite ; Process for production Magnesium and Calcium chloride
Beneficiation and Mineral Processing of Sand and Silica Sand; Sand and Silica Sand; Processing Sand; Sand into Silicon-Silicon carbide ; Heavy Mineral Sand; Separation of Heavy Minerals from Black Sand/Sand; Zircon to Zirconium; Ti-Bearing Minerals
Origin and Abundance of elements in the Solar system and in the Earth and its...AkshayRaut51
Definition of Elements and atom
Origin of Universe
Theories of origin of Solar system and Earth
Chemical Composition of Planets
Chemical Composition of Earth
Chemical composition of Meteorites
Abundance of Elements
THE PRESENCE AND VARIETY OF A PARTICULAR PLANTS
SPECIES IN THE AREA OF MINERALISATION HAVE BEEN RECOGNISED AS A GUIDE TO LOCATING ORE, METHOD,UNIVERSAL INDICATORS , UNIVERSAL INDICATOR ,LOCAL INDICATOR
Mineral deposits known to occur in Egypt; Classification of mineral deposit in Egypt, Possible Areas for Investment in Mineral Industry in Egypt, Mineral Commodities
Limestone;Industrial Uses of Limestone ; Lime; Lime Cycle; Production of Lime; Classification of Hydrated Lime IS 712-1973; Purposes for the Utilize of Lime; Soda Ash;Solvay process for the manufacture of Soda Ash; Purposes for the Utilize of Soda Ash; Gypsum; Calcination of Gypsum; Hardening of Plaster; Magnesium; Production Of Magnesium from seawater and dolomite; Process for production Magnesium hydroxide and Calcium chloride from Dolomite ; Process for production Magnesium and Calcium chloride
Beneficiation and Mineral Processing of Sand and Silica Sand; Sand and Silica Sand; Processing Sand; Sand into Silicon-Silicon carbide ; Heavy Mineral Sand; Separation of Heavy Minerals from Black Sand/Sand; Zircon to Zirconium; Ti-Bearing Minerals
zeolites, types, nature, synthetic, processes, Deposits and properties;Physical characteristics of some naturally occurring zeolites; molecular sieves;Adsorption and related molecular sieving; zeolite catalysts
SUPERGENE ENRICHMENT; Definition; Zones; Morphology of Zoning; Oxidized zone ; Supergene zone ; Gossans and Cappings; Chemical Changes Involved; Electrowinning; Formation of Copper Oxides
Earth Resources
Reserves and resources
Nonrenewable Mineral Resources
What are industrial minerals?
Why are industrial minerals so important?
Geology of Industrial Minerals Deposits
Classification of industrial minerals
General characteristics of Non-metallic Deposits
Factors important in evaluating an industrial minerals deposit
Selected industrial rocks and minerals
ABRASIVES MINERALS
OLIVINE
GYPSUM
CLAY MINERALS
FLUORITE
PERLITE
BUILDING STONES and Rip-rap
CALCIUM CARBONATE DEPOSITS
SULFUR ORE DEPOSITS
CHERT DEPOSITS
PHOSPHATE ORE DEPOSITS
EVAPORITE DEPOSITS
SELECTED SOME NON-METALLIC METAMORPHIC DEPOSITS
Asbestos Deposits
Graphite Deposits
Talc, Soapstone, and Pyrophyllite
Selected Some Ornamental Metamorphic Stones
Marble
Quartzite
Serpentinite
Study of plate tectonics of the earth, or plate movement, Jahangir Alam
a) Wegener’s Evidence (Continental Drift)
b) History of Plate Tectonics
c) Breakup and Appearence of Pangea
WHAT IS A PLATE?
Major continental and oceanic plates include:
Types of Earth’s Crust:
Plate tectonics (from the Late Latin tectonicus) is a scientific theory which describes the large scale motions of Earth's lithosphere.
THE DYNAMIC EARTH:
The earth is a dynamic planet, continuously changing both externally and internally. The earth’s surface is constantly being changed by endo-genetic processes resulting in volcanism and tectonism, and exogenetic processes such as erosion and deposition. These processes have been active throughout geological history. The processes that change the surface feature are normally very slow (erosion and deposition) except some catastrophic changes that occur instantaneously as in the case of volcanism or earthquakes. The interior of the earth is also in motion. Deeper inside the earth, the liquid core probably flows at a geologically rapid rate of a few tenths of mm/s. Several hypotheses attempted to explain the dynamism of the earth.
+ Horizontal movement hypothesis
+ Continental drift, displacement hypothesis
Development of the plate tectonic theory.
Plate tectonic theory arose out of the hypothesis of continental drift proposed by Alfred Wegener in 1912. He suggested that the present continents once formed a single land mass that drifted apart, thus releasing the continents from the Earth's core and likening them to "icebergs" of low density granite floating on a sea of denser basalt.
Seafloor Spreading
The first evidence that the lithospheric plates did move came with the discovery of variable magnetic field direction in rocks of differing ages.
The earliest (Precambrian) history of the earth's crustDhanBahadurkhatri
The duration of the Precambrian era and the earliest known state of the crust, Development of Archean Cratons, the Precambrian shield rocks, Paleogeography during Precambrian, and Precambrian glaciations.
Khatatba Formation
• Geological formation in the Shoushan
Basin, North Western Desert, Egypt
• Middle Jurassic formation, dating back
approximately 174 to 163 million years ago
• Contains organic
-rich shale and coaly shale
• Important source rocks for hydrocarbons • Significant target for oil and gas exploration
in the region
• Extensively studied with organic
geochemical, petrographic, and
petrophysical analyses
• Studies helped identify essential elements
of the petroleum system in the area.
Written information are rightfully gathered from the internet. Kindly, use this properly including proper citation. This is a presentation made during our high school days.
The objectives of this course in iron ore Resources and iron industry are:
i) acquainting students (majors and non-majors) with the basic tools necessary for studying iron ore deposits and processes,
ii) different processes for phosphorus removal from iron ore
iii) beneficiation processes of iron ore deposits.
iv) different processes and techniques that used to enrichment low-grade iron ore resources
v) understanding the different ironwork processes and technology,
vi) understanding the different types of iron ore products,
vii) prominent routes for steelmaking
viii) understanding the relationship between the distribution of iron ore and scrap, as well as steelmarkets,
ix) steel industry in Egypt , and
x) gaining some knowledge of the global iron ore as well as environmental problems associated with the extraction and utilization of iron ore resources.
There are plenty of hard-to-beneficiate iron ores and high-grade tailings in India and all over the world; As the volume of high-grade iron ores declines.
Minerals phase transformation by hydrogen reduction (MPTH) can efficiently revitalize hard-to-beneficiate iron ore resources and tailings, turning the waste into profitable products. It may also improve the concentrate quality comparing to that from the previous method. From the economic and environmental aspects, MPTH is the most effective method to recover iron oxides.
The clean minerals phase transformation by hydrogen reduction (MPTH) was proposed.
Industrial utilization of limonite/goethite, limonite-hematite, sulfur-bearing refractory iron ore was achieved, where Sulfur-bearing minerals decomposed or formed sulfate after oxidation roasting.
Sulfur content of iron ore concentrate was significantly reduced to 0.038 %.
Improving utilization efficiency of refractory iron ore resources is a common theme for the sustainable development of the world’s steel and iron industry.
Magnetization Roasting is considered as an effective and typical method for the beneficiation of refractory iron ores.
After magnetization roasting, the weakly magnetic iron minerals, including hematite, limonite and siderite, are selectively reduced or oxidized to ferromagnetic magnetite, which is relatively easier to enrich by Magnetic Separation after liberation pretreatments.
The Primary Magnetization Roasting Methods include: Shaft Furnace Roasting, Rotary Kiln Roasting, Fluidized Bed Roasting, and Microwave assisted roasting. The developments in magnetization roasting of difficult to treat iron ores, including: Shaft Furnace Roasting, Rotary Kiln Roasting, Fluidized Bed Roasting, and Microwave Assisted Roasting in the Past Decade.
Shaft Furnace Roasting is gradually eliminated due to its high energy consumption and low industrial processing capacity, and the primary problem for rotary kiln roasting is the kiln coating which affects the yield of iron resource and its industrial application.
Fluidized Bed Roasting and Microwave assisted roasting are considered as the most effective and promising methods.
Suspension (Fluidized) Magnetization Roasting is recognized as the most effective and promising technology due to its high reaction efficiency, low energy consumption and large processing capacity. Moreover, an industrial production line with a throughput of 1.65 million t/a for beneficiation of a specularite ore has been built.
Microwave Assisted Roasting is a potential alternative technology for magnetizing iron ores. However, it is currently limited to laboratory research and has no industrial application. Forwarding microwave assisted magnetization roasting methods into industrial applications needs long way and time to achieve.
Furthermore, using biomass, H2 or siderite as a reducing agent in the magnetic reduction roasting of iron ores is a beneficial way to reduce carbon emissions, which can be called clean and green magnetization roasting technology.
In the future, technical research on clean and green magnetization roasting should be strengthened. Maybe microwave magnetization roasting using biomass/H2/siderite as reductant can be further studied for a more effective and greener magnetization of iron ores.
WORLD RESOURCES IRON DEPOSITS
Iron Ore Pellets Market Industry Trends
Scope and Market Size
Market Analysis and Insights
DRI Production in Plants Using Merchant Iron Ore
Outlook for DR grade pellet supply‐demand out to 2030
DRI and the pathway to carbon‐neutral steelmaking
Supply‐side challenges for the steel & iron ore industries
scrap is the main raw material, is growing in the structure of global steelmaking capacities; SCARP/ RECYCLING IRON ; EAF steel production method in the world; Scrap for Stock; A Global Scrap Shortage;Availability of Ferrous Scrap Resources; EGYPT IRON SCRAP IMPORTS.
The iron ore production has significantly expanded in recent years, owing to increasing steel demands in developing countries.
However, the content of iron in ore deposits has deteriorated and low-grade iron ore has been processed.
The fine ores resulting from the concentration process must be agglomerated for use in iron and steelmaking.
Bentonite is the most used binder due to favorable mechanical and metallurgical pellet properties, but it contains impurities especially silica and alumina.
Better quality wet, dry, preheated, and fired pellets can be produced with combined binders, such as organic and inorganic salts, when compared with bentonite-bonded pellets.
While organic binders provide sufficient wet and dry pellet strengths, inorganic salts provide the required preheated and fired pellet strengths.
The industrial development program of any country, by and large, is based on its natural resources.
Currently the majority of the world’s steel is produced through either one of the two main routes: i) the integrated Blast Furnace – Basic Oxygen Furnace (BF – BOF) route or ii) the Direct Reduced Iron - Electric Arc Furnace (DRI - EAF) route.
Depleting resources of coking coal, the world over, is posing a threat to the conventional (Blast Furnace [Bf]–Basic Oxygen Furnace [BOF]) route of iron and steelmaking.
During the last four decades, a new route of ironmaking has rapidly developed for Direct Reduction (DR) of iron ore to metallic iron by using noncoking coal/natural gas.
This product is known as Direct Reduced Iron (DRI) or Sponge Iron.
Processes that produce iron by reduction of iron ore (in solid state) below the melting point are generally classified as DR processes.
Based on the types of reductant used, DR processes can be broadly classified into two groups: (1) coal-based DR process and (2) gas-based DR process.
Details of DR processes, reoxidation, storage, transportation, and application of DRI are discussed in this presentation.
This presentation reviews the different DR processes used to produce Direct Reduced Iron (DRI), providing an analysis on the quality requirements of iron-bearing ores for use in these processes. The presentation also discusses the environmental sustainability of such processes. DR processes reduce iron ore in its solid state by the use of either natural gas or coal as reducing agents, and they have a comparative advantage of low capital costs, low emissions and production flexibility over the BF process.
Currently the majority of the world’s steel is produced through either one of the two main routes: i) the integrated Blast Furnace – Basic Oxygen Furnace (BF – BOF) route or ii) the Direct Reduced Iron - Electric Arc Furnace (DRI - EAF) route.
In the former, the blast furnace uses iron ore, scrap metal, coke and pulverized coal as raw materials to produce hot metal for conversion in the BOF. Although it is still the prevalent process, blast furnace hot metal production has declined over the years due to diminishing quality of metallurgical coke, low supply of scrap metal and environmental problems associated with the process. These factors have contributed to the development of alternative technologies of ironmaking, of which Direct Reduction (DR) processes are expected to emerge as preferred alternatives in the future.
This presentation reviews the different DR processes used to produce Direct Reduced Iron (DRI), providing an analysis on the quality requirements of iron-bearing ores for use in these processes. The presentation also discusses the environmental sustainability of such processes. DR processes reduce iron ore in its solid state by the use of either natural gas or coal as reducing agents, and they have a comparative advantage of low capital costs, low emissions and production flexibility over the BF process.
Ironmaking represents the first step in steelmaking.
The iron and steel industry is the most energy-intensive and capital-intensive manufacturing sector in the world (Strezov, 2006).
Steelmaking processes depend on different forms of iron as primary feed material. Traditionally, the main sources of iron for making steel were Blast Furnace hot metal and recycled steel in the form of scrap.
The Blast Furnace (BF) has remained the workhorse of worldwide virgin iron production (i.e., hot metal) for more than 200 years. Over the years, BFs have evolved into highly efficient chemical reactors, capable of providing stable operation with a wide range of feed materials.
However, operation of modern efficient BFs normally involves sintering and coke making and their associated environmental problems.
More than 90% of iron is currently produced via the BF process, while the rest is coming from Direct Reduction (DR) processes, Mini Blast Furnaces (MBFs), Corex, Finex, Ausmelt, etc. Additionally, the severe shortage of good-quality metallurgical coal has remained an additional constraint all over the world. In view of this, there is an increasing awareness that the BF route needs to be supplemented with alternative ironmaking processes that are more environment friendly and less dependent on metallurgical coal.
Because of the rapid depletion of easily processed iron ores, the utilization of refractory ores has attracted increasing attention .
There several billion tonnes iron deposits, and most are refractory ores, which are difficult to process by conventional methods because of the low iron grade, fine grain size and complex mineralogy.
The beneficiation of low-grade iron ores to meet the growing demand for iron and steel is an important research topic.
At present, magnetization roasting followed by magnetic separation is one of the most effective technologies for the beneficiation of refractory iron ores.
However, certain ores do not qualify to be treated in physical separation processes, and hence, alternative strategies are being looked into for upgrading their iron content.
Reduction roasting has many advantages over the physical beneficiation process, such as enhanced iron recovery and processing of complex and poorly liberated iron ores.
The objective of this presentation is to compile and amalgamate the crucial information regarding the beneficiation of low-grade iron ores using carbothermic reduction followed by magnetic separation, which is a promising technique to treat iron ores with complex mineralogy and liberation issues.
Reduction roasting studies done for different types low-grade iron ores including oolitic iron ores, banded iron ores, iron ore slimes and tailings, and industrial wastes have been discussed.
Reduction roasting followed by magnetic separation is a promising method to recover the iron values from low-grade iron ores.
The process involves the reduction of the goethite and hematite phases to magnetite, which can subsequently be recovered using a low-intensity magnetic separation unit.
The large-scale technological advancements in reduction roasting and the possibilities of the application of alternative reductants as substitutes for coal have also been highlighted.
This presentation aims at insight light on the occurrence of phosphorus in iron ores from the mines around the world.
The presentation extends to the phosphorus removal processes of this mineral to meet the specifications of the steel industry.
Phosphorus is a contaminant that can be hard to remove, especially when one does not know its mode of occurrence in the ores.
Phosphorus can be removed from iron ore by very different routes of treatment. The genesis of the reserve, the mineralogy, the cost and sustainability define the technology to be applied.
The presentations surveyed cite removal by physical processes (flotation and selective agglomeration), chemical (leaching), thermal and bioleaching processes.
Removal results of above 90% and less than 0.05% residual phosphorus are noticed, which is the maximum value required in most of the products generated in the processing of iron ore.
Chinese studies show that the direct reduction roasting of high phosphorus oolitic hematite followed by magnetic separation is reality technical solutions to improve the recovery of metallic iron and dephosphorization rate.
For ores with widespread phosphorus in the iron matrix and low release, thermal or mixed processes are closer to reality technical solutions. Due to their higher operating costs, it will be necessary to rethink the processes of sintering and pelletizing, such that these operations also become phosphorus removal steps.
With the exhaustive processing of the known reserves of hematite from Iron Ore Quadrangle (Minas Gerais-Brazil), there will be no shortage of granules in the not too distant future. THEREFORE, THERE IS AN EXPECTATION THAT THE ORE MINED WILL HAVE HIGHER LEVELS OF PHOSPHORUS.
Overview of IRON TYPES: Pig Iron, Direct Reduced Iron (DRI), Hot Briquetted Iron (HBI), Cold Briquetted Iron (CBI) and Cold Briquetted Iron and Carbon (CBIC) Specifications .
Comparison of Pig Iron and DRI
Properties; Manufacturing Process; Uses; Largest producers and markets
Iron ore mining plays a critical role in supplying the raw material necessary for steel production, supporting various industries and economic development worldwide.
From the extraction of iron ore to its processing and eventual export, each stage of the mining process requires careful planning, technological advancements, and environmental considerations.
By adopting sustainable mining practices and mitigating environmental impacts, the future of iron ore mining can be aligned with the principles of responsible resource utilization and environmental stewardship
The Egyptian steel sector is the second largest steel market in the Middle East and North Africa region in terms of production and third largest in terms of consumption.
Egypt was the third-ranked producer of Direct-Reduced Iron (DRI) in the Middle east and North Africa region after Iran and Saudi Arabia and accounted for 5.4% of the world’s total output
The Egyptian steel industry represents one of the cornerstones of Egypt’s economic growth and development, due to its linkages to almost all other industries that stimulate economic expansion, such as construction, housing, infrastructure, consumer goods and automotive. All these industries rely heavily on steel industry and so, the importance and development of the steel sector is significant for the progress of the Egyptian economy in general.
The Egyptian market has many companies that produce different steel products.
Geological consultant, working in a range of roles from project development/feasibility study programs and advanced exploration roles. Contracts in a variety of global locations including Egypt, Saudi Arab, and the Middle East. Commodities including Gold, base metal sulfide, Gossan/Supergene, heavy mineral sands, clay/kaolin, Silica Sand, and iron ore.
Exploration in Deep Weathering Profiles, Supergene, R-mode factor analysis; Multi-element association geochemistry; Assessment of Au-Zn potentiality in Gossan; Rodruin-Egypt
Mineral Processing: Crusher and Crushing; Secondary and Tertiary Crushing Circuits; Types of Crusher; Types of Crushing; Types of Jaw Crushers; Impact Crusher; Types of Cone Crushers; Ball Mill; BEST STONE MANUFACTURERS; Local Quality and High quality ; International and Country/Hand made
Classification Equipment
Introduction; Chemical composition of garnet; Structure; Classification; Physical properties; Optical properties; Occurrences; Gem variety; and Uses
Garnet group of minerals is one of the important group of minerals.
Since they are found in wide variety of colours, they are also used as gemstones.
Garnet group of minerals are also abrasives and thus have various industrial applications.
Welcome to TechSoup New Member Orientation and Q&A (May 2024).pdfTechSoup
In this webinar you will learn how your organization can access TechSoup's wide variety of product discount and donation programs. From hardware to software, we'll give you a tour of the tools available to help your nonprofit with productivity, collaboration, financial management, donor tracking, security, and more.
Model Attribute Check Company Auto PropertyCeline George
In Odoo, the multi-company feature allows you to manage multiple companies within a single Odoo database instance. Each company can have its own configurations while still sharing common resources such as products, customers, and suppliers.
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
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
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
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
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
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
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
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
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
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
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
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
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)
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
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