Understanding regional tectonics using beach balls Part I Remember b.pdf
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Understanding regional tectonics using beach balls Part I: Remember beach balls and fault types Figure 1 shows that we can distinguish the different types of faults (normal, reverse and strike- slip) using beach balls. Beach balls describe the focal mechanism occurring at a given fault. Figure 1: Different types of faults and associated focal mechanisms. The black parts are under compression and the white parts under tension. For the strike-slip faults, the circle with the cross means that the block is sliding further from you, while the dot inside the circle means that the block is sliding towards you. For all three cases, the direction of the fault is through the page. Part II: Using beach balls to understand the regional tectonics around Turkey Figure 2 shows the focal mechanisms for the eastern Mediterranean region. 1) Draw arrows showing the relative motion across some of the main fault zones (shown with eleven pairs of dots), using the beach balls on Figure 2 and help from Figure 1. Note that for strike-slip faults, there are usually two possibilities (e.g., left-lateral strike slip fault oriented N-S or right-lateral strike-slip fault oriented W-E). However, here, you already have the direction of the fault, so there is only one possibility. 2) Draw arrows showing the motion of the three southern plates relative to Eurasia. That means that Eurasia, in this exercise, is not moving. Motion of the three southern plates are shown with four boxes. A good way to work this problem is to imagine cutting the map on the next page map into pieces along the plate-bounding faults, tape Eurasian to a table, and try sliding the blocks to see if you can find a way to move them that is consistent with the focal mechanisms. Figure 2, next page: (top). Focal mechanisms for the eastern Mediterranean region. (bottom) Topographic and bathymetric maps to be completed with relative motions of the plates. Eurasian Plate African Plate Eurasian Plate 3) There are volcanoes on near the west-most box. Why is this? 4) Compare the African and Arabian arrows (i.e., velocity vectors). Which is larger? 5) There are large mountains in Iran and the Caucuses (in the NE portion of the map, see also name of countries on Figure 4). Why is this? 6) There are elongated islands, peninsulas and inlets in Greece that trend SE-NW to E-W. Why is this? .
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Understanding regional tectonics using beach balls Part I Remember b.pdf
Understanding regional tectonics using beach balls Part I: Remember beach balls and fault types
Figure 1 shows that we can distinguish the different types of faults (normal, reverse and strike-
slip) using beach balls. Beach balls describe the focal mechanism occurring at a given fault.
Figure 1: Different types of faults and associated focal mechanisms. The black parts are under
compression and the white parts under tension. For the strike-slip faults, the circle with the cross
means that the block is sliding further from you, while the dot inside the circle means that the
block is sliding towards you. For all three cases, the direction of the fault is through the page.
Part II: Using beach balls to understand the regional tectonics around Turkey Figure 2 shows the
focal mechanisms for the eastern Mediterranean region. 1) Draw arrows showing the relative
motion across some of the main fault zones (shown with eleven pairs of dots), using the beach
balls on Figure 2 and help from Figure 1 . Note that for strike-slip faults, there are usually two
possibilities (eg., left-lateral strike slip fault oriented N-S or right-lateral strike-slip fault oriented
W-E). However, here, you already have the direction of the fault, so there is only one possibility.
2) Draw arrows showing the motion of the three southern plates relative to Eurasia. That means
that Eurasia, in this exercise, is not moving Motion of the three southern plates are shown with
four boxes. A good way to work this problem is to imagine cutting the map on the next page map
into pieces along the plate-bounding faults, tape Eurasian to a table, and try sliding the blocks to
see if you can find a way to move them that is consistent with the focal mechanisms. Figure 2,
next page: (top). Focal mechanisms for the eastern Mediterranean region. (bottom) Topographic
and bathymetric maps to be completed with relative motions of the plates.
There are volcanoes on near the west-most box. Why is this? 4) Compare the African and
Arabian arrows (i.e, velocity vectors). Which is larger? 5) There are large mountains in Iran and
the Caucuses (in the NE portion of the map, see also name of countries on Figure 4). Why is
this? 6) There are elongated islands, peninsulas and inlets in Greece that trend SE-NW to E-W.
Why is this?
Figure 3: Major faults in the Mediterranean region..
Deadline is on Tuesday ,September 16 th2014I would like to .docx
Deadline is on Tuesday ,September 16 th/2014
I would like to have a design of the four broadcast protocols using a written description with the graphic representation showing how the design looks like and how information/communication happen between nodes beside the details explanation using scenarios to estimate the complexity.
Each of the designs should have an evaluation of the efficiency in the context of message complexity and round complexity.
The design should be based on a cube system with 8 nodes using
1. message-passing model
2. shared-memory model
3. mobile agent communication model
So the final work will have a total of 4 graphic designs with use case scenarios for each design to explain and calculate the complexity and efficiently of each design. The efficiency would be calculated for each design in term of message complexity and round complexity. Then decide on the best protocol among the proposed designs based on the efficiency.
geology2.pdf
geology1.pdf
1
Plate Tectonics Name: ________________
INTRODUCTION
Plate tectonics is a well established theory that unifies and provides a framework for
all geologic observations. Most geologic phenomenon observed near the Earth’s
surface are linked in some way to plate tectonic processes. The theory states that the
outer 60-100 km of the Earth is divided into slabs of rigid rock (the lithosphere). These
slabs (the plates) rest upon a semi-viscous layer of easily deformable rock (the
asthenosphere). Thermal convection within the asthenosphere pushes the plates in
horizontal directions at rates ranging from 1 cm to 12 cm/year. This causes the plates
to move in relation to one another. Boundaries between the 8 principle plates and
several smaller plates are zones of rock deformation, earthquakes and volcanism.
This lab utilizes real data that demonstrates and/or validates the theory of Plate
Tectonics. Four exercises, modified from Jones and Jones (2003), follow.
o Part A examines global maps of tectonic plate boundaries and earthquake data
to identify plate boundary locations and assess relative motion between the
plates.
o Part B uses maps of the ocean floor to calculate spreading rates across a mid-
oceanic ridge in the South Pacific.
o Part C interprets maps and utilizes geologic ages for Hawaiian Islands to better
understand movement of the underlying Pacific plate over a “hot spot”.
o Part D examines a geologic map along a portion of the San Andreas Fault to
evaluate the direction and rate of plate movement.
OBJECTIVES
Upon completion of this exercise, you will be able to understand:
1. basic differences between major types of plate boundaries.
2. magnetic stripping and use it to calculate spreading rates
3. the concept of “hot spots” and use this understanding to determine the speed
and direction of movement of plates
4. how to interpret a geological map of the San Andreas Fault and calculate the
rate of movement al.
Geologic maps show the distribution of rock units at the sur.pdf
Geologic maps show the distribution of rock units at the surface as well as structural features,
such as faults and folds. A geologic map is usually printed on top of a regular topographic map
(the base map) to help you locate yourself on the map. The base map is printed with light colors,
so it doesn't interfere with seeing the geologic features on the map. The geology is represented by
colors, lines, and symbols unique to geologic maps. Each color used on a geologic map
represents a different geologic unit. A unit is a specific type of rock of a specific age range (for
example, a Permian limestone, a contact late Triassic sandstone, etc). All exposures of rocks of
the same age and type are shown with the same color and are separated from other rocks by a
line representing the contact between them. The two main types of contacts shown on most
geologic maps are depositional contacts and faults. Where the original depositional contact
between geologic units is preserved, it is shown on the geologic map as a thin line. If the rocks are
in contact because of a fault, a thicker line is used to represent the fault, and the relative motion
along the fault, if known, is indicated by labeling the upthrown side and downthrown side of the
fault. For low angle (thrust) faults the teeth are on the upthrown (hanging wall) block. Each
geologic unit is assigned a set of letters to symbolize it on the map. Usually the symbol is the
combination of a capital letter followed by one or more small letters. The capital letter represents
the age (geologic period) of the unit. Examples include Q (Quaternary), K (Cretaceous), and C
(Cambrian). The small letters indicate either the name of the unit, if it has one, or the type of rock,
if the unit has no name. Many geologic units are named based on where their characteristics are
bestdisplayed, or where they were first studied. For example, Jm is the map symbol for the
Morrison formation, a stratigraphic unit of Jurassic age first studied near Morrison, Colorado but
exposed throughout Colorado, Wyoming, and Utah (the Morrison formation is the source of many
dinosaur fossils). Js would be unnamed shale (s for shale) that is Jurassic in age. Sedimentary
rocks form in broad, flat layers (beds) that may later be tilted or bent by tectonic forces. The spatial
orientation of tilted rock layers is described in terms of strike and dip. Strike is the compass
direction of a line formed by the intersection of a horizontal plane (the surface of the Earth) and an
inclined surface (the titled rock layer). Dip is the angle between a horizontal plane and the inclined
surface and is always measured perpendicular to strike. On geologic maps " T " shaped-symbols
are used show the strike and dip of each rock unit. The top of the "T" is the line of strike and the
short arm of the " T " illustrates the dip direction in degrees. The higher the number, the steeper
the bed with 90 being perpendicular to the surface (vertical). In the example h.
An Integrated Study of Gravity and Magnetic Data to Determine Subsurface Stru...
:The present study wascarried out to delineate the location, extension, trend and depth of subsurface
structures of Alamein area. To achieve this aim, the gravity and aeromagnetic data have been subjected to
different analytical techniques. The Fast Fourier Transform technique was used to separatethe residual
components from the regional ones. The resulted maps showed that the area was affected mainly bytheENE, EW,
WNWand NWtectonic trends. In addition, spectral analysis technique was applied on magnetic anomalies to
estimate the depth to basement surface, which varies from 3.03 in southern part to 7.24 Km in northern part.3DEulerdeconvloution
and tilt angle derivative techniques were carried out to detect the edges of magnetic sources
and to determine their depths.Correlation between them shows acoincidence between Euler solution and zero
lines of tilt angle map. A tentative basement structure map is constructed from the integration of these results
and geological information. This map shows alternative uplifted and downfaulted structure trending in the ENE,
NE and E-W directions. In addition, the NNW to NW strike-slip faults intersected them in later events. Finally,
2-D modeling technique was run on three gravity and magnetic profiles in the same location. Different drilled
wells and the constructed basement structure map support these modeled profiles. Theyshow an acidic basement
rocks. A general decreasing of Conrad discontinuity depths from about 20.5 km at southern part to 17.9 km at
northern part can be noticed. Moreover, the crustal thickness (depth to Moho discontinuity), varies between
31.5 and 28.5 km revealing visibly crustal stretching and thinning northerly
Recommended
Understanding regional tectonics using beach balls Part I Remember b.pdf
Understanding regional tectonics using beach balls Part I: Remember beach balls and fault types
Figure 1 shows that we can distinguish the different types of faults (normal, reverse and strike-
slip) using beach balls. Beach balls describe the focal mechanism occurring at a given fault.
Figure 1: Different types of faults and associated focal mechanisms. The black parts are under
compression and the white parts under tension. For the strike-slip faults, the circle with the cross
means that the block is sliding further from you, while the dot inside the circle means that the
block is sliding towards you. For all three cases, the direction of the fault is through the page.
Part II: Using beach balls to understand the regional tectonics around Turkey Figure 2 shows the
focal mechanisms for the eastern Mediterranean region. 1) Draw arrows showing the relative
motion across some of the main fault zones (shown with eleven pairs of dots), using the beach
balls on Figure 2 and help from Figure 1 . Note that for strike-slip faults, there are usually two
possibilities (eg., left-lateral strike slip fault oriented N-S or right-lateral strike-slip fault oriented
W-E). However, here, you already have the direction of the fault, so there is only one possibility.
2) Draw arrows showing the motion of the three southern plates relative to Eurasia. That means
that Eurasia, in this exercise, is not moving Motion of the three southern plates are shown with
four boxes. A good way to work this problem is to imagine cutting the map on the next page map
into pieces along the plate-bounding faults, tape Eurasian to a table, and try sliding the blocks to
see if you can find a way to move them that is consistent with the focal mechanisms. Figure 2,
next page: (top). Focal mechanisms for the eastern Mediterranean region. (bottom) Topographic
and bathymetric maps to be completed with relative motions of the plates.
There are volcanoes on near the west-most box. Why is this? 4) Compare the African and
Arabian arrows (i.e, velocity vectors). Which is larger? 5) There are large mountains in Iran and
the Caucuses (in the NE portion of the map, see also name of countries on Figure 4). Why is
this? 6) There are elongated islands, peninsulas and inlets in Greece that trend SE-NW to E-W.
Why is this?
Figure 3: Major faults in the Mediterranean region..
Deadline is on Tuesday ,September 16 th2014I would like to .docx
Deadline is on Tuesday ,September 16 th/2014
I would like to have a design of the four broadcast protocols using a written description with the graphic representation showing how the design looks like and how information/communication happen between nodes beside the details explanation using scenarios to estimate the complexity.
Each of the designs should have an evaluation of the efficiency in the context of message complexity and round complexity.
The design should be based on a cube system with 8 nodes using
1. message-passing model
2. shared-memory model
3. mobile agent communication model
So the final work will have a total of 4 graphic designs with use case scenarios for each design to explain and calculate the complexity and efficiently of each design. The efficiency would be calculated for each design in term of message complexity and round complexity. Then decide on the best protocol among the proposed designs based on the efficiency.
geology2.pdf
geology1.pdf
1
Plate Tectonics Name: ________________
INTRODUCTION
Plate tectonics is a well established theory that unifies and provides a framework for
all geologic observations. Most geologic phenomenon observed near the Earth’s
surface are linked in some way to plate tectonic processes. The theory states that the
outer 60-100 km of the Earth is divided into slabs of rigid rock (the lithosphere). These
slabs (the plates) rest upon a semi-viscous layer of easily deformable rock (the
asthenosphere). Thermal convection within the asthenosphere pushes the plates in
horizontal directions at rates ranging from 1 cm to 12 cm/year. This causes the plates
to move in relation to one another. Boundaries between the 8 principle plates and
several smaller plates are zones of rock deformation, earthquakes and volcanism.
This lab utilizes real data that demonstrates and/or validates the theory of Plate
Tectonics. Four exercises, modified from Jones and Jones (2003), follow.
o Part A examines global maps of tectonic plate boundaries and earthquake data
to identify plate boundary locations and assess relative motion between the
plates.
o Part B uses maps of the ocean floor to calculate spreading rates across a mid-
oceanic ridge in the South Pacific.
o Part C interprets maps and utilizes geologic ages for Hawaiian Islands to better
understand movement of the underlying Pacific plate over a “hot spot”.
o Part D examines a geologic map along a portion of the San Andreas Fault to
evaluate the direction and rate of plate movement.
OBJECTIVES
Upon completion of this exercise, you will be able to understand:
1. basic differences between major types of plate boundaries.
2. magnetic stripping and use it to calculate spreading rates
3. the concept of “hot spots” and use this understanding to determine the speed
and direction of movement of plates
4. how to interpret a geological map of the San Andreas Fault and calculate the
rate of movement al.
Geologic maps show the distribution of rock units at the sur.pdf
Geologic maps show the distribution of rock units at the surface as well as structural features,
such as faults and folds. A geologic map is usually printed on top of a regular topographic map
(the base map) to help you locate yourself on the map. The base map is printed with light colors,
so it doesn't interfere with seeing the geologic features on the map. The geology is represented by
colors, lines, and symbols unique to geologic maps. Each color used on a geologic map
represents a different geologic unit. A unit is a specific type of rock of a specific age range (for
example, a Permian limestone, a contact late Triassic sandstone, etc). All exposures of rocks of
the same age and type are shown with the same color and are separated from other rocks by a
line representing the contact between them. The two main types of contacts shown on most
geologic maps are depositional contacts and faults. Where the original depositional contact
between geologic units is preserved, it is shown on the geologic map as a thin line. If the rocks are
in contact because of a fault, a thicker line is used to represent the fault, and the relative motion
along the fault, if known, is indicated by labeling the upthrown side and downthrown side of the
fault. For low angle (thrust) faults the teeth are on the upthrown (hanging wall) block. Each
geologic unit is assigned a set of letters to symbolize it on the map. Usually the symbol is the
combination of a capital letter followed by one or more small letters. The capital letter represents
the age (geologic period) of the unit. Examples include Q (Quaternary), K (Cretaceous), and C
(Cambrian). The small letters indicate either the name of the unit, if it has one, or the type of rock,
if the unit has no name. Many geologic units are named based on where their characteristics are
bestdisplayed, or where they were first studied. For example, Jm is the map symbol for the
Morrison formation, a stratigraphic unit of Jurassic age first studied near Morrison, Colorado but
exposed throughout Colorado, Wyoming, and Utah (the Morrison formation is the source of many
dinosaur fossils). Js would be unnamed shale (s for shale) that is Jurassic in age. Sedimentary
rocks form in broad, flat layers (beds) that may later be tilted or bent by tectonic forces. The spatial
orientation of tilted rock layers is described in terms of strike and dip. Strike is the compass
direction of a line formed by the intersection of a horizontal plane (the surface of the Earth) and an
inclined surface (the titled rock layer). Dip is the angle between a horizontal plane and the inclined
surface and is always measured perpendicular to strike. On geologic maps " T " shaped-symbols
are used show the strike and dip of each rock unit. The top of the "T" is the line of strike and the
short arm of the " T " illustrates the dip direction in degrees. The higher the number, the steeper
the bed with 90 being perpendicular to the surface (vertical). In the example h.
An Integrated Study of Gravity and Magnetic Data to Determine Subsurface Stru...
:The present study wascarried out to delineate the location, extension, trend and depth of subsurface
structures of Alamein area. To achieve this aim, the gravity and aeromagnetic data have been subjected to
different analytical techniques. The Fast Fourier Transform technique was used to separatethe residual
components from the regional ones. The resulted maps showed that the area was affected mainly bytheENE, EW,
WNWand NWtectonic trends. In addition, spectral analysis technique was applied on magnetic anomalies to
estimate the depth to basement surface, which varies from 3.03 in southern part to 7.24 Km in northern part.3DEulerdeconvloution
and tilt angle derivative techniques were carried out to detect the edges of magnetic sources
and to determine their depths.Correlation between them shows acoincidence between Euler solution and zero
lines of tilt angle map. A tentative basement structure map is constructed from the integration of these results
and geological information. This map shows alternative uplifted and downfaulted structure trending in the ENE,
NE and E-W directions. In addition, the NNW to NW strike-slip faults intersected them in later events. Finally,
2-D modeling technique was run on three gravity and magnetic profiles in the same location. Different drilled
wells and the constructed basement structure map support these modeled profiles. Theyshow an acidic basement
rocks. A general decreasing of Conrad discontinuity depths from about 20.5 km at southern part to 17.9 km at
northern part can be noticed. Moreover, the crustal thickness (depth to Moho discontinuity), varies between
31.5 and 28.5 km revealing visibly crustal stretching and thinning northerly
Structural Analysis and Tectonic Evolution based on Seismic Interpretation in...
the subsurface tectonic evolution of the East of Nile valley (EON) of the Beni Suef basin, Egypt, were
studied using twenty seismic profiles representing the desired structural framework of the EON - four of these
were selected for illustration - supported by the vertical seismic profile (VSP) logs of three deep wells drilled in
the study area. In addition, the analysis encompasses the detailed investigation of two (TWT) two way time
structure-contour maps and the rose diagrams representing the general trends of the recorded fault systems.
The study proved that the Upper Cretaceous rocks were dissected by systems of normal faults, trending in
WNW-ESE, NW-SE. These fault systems were originated in association to Cretaceous-Early Tertiary tectonic
deformations related to the Tethyan plate tectonics.
1 How does a topographic map show the shape of the land sur.pdf
1. How does a topographic map show the shape of the land surface? For example, how do
topographic maps indicate steeper slopes? How are gentler slopes portrayed? How can you
identify
stream or river valleys on maps?
2. What are contour lines? What is an index contour?
3. Define contour interval.
4. What does a fractional scale of 1:48,000 mean?
5. What is a bar scale and how is it used?
6. The basic unit of latitude and longitude is the degree. How is the degree subdivided?
7. Latitude is measured in degrees N or S of what line? What is the range of possible values (in
degrees) for latitude?
8. Longitude is measured in degrees W or E of what line? Where is that line located? What is the
range
of possible values (in degrees) for longitude?
Introduction Topograpbic maps illustrate scale, width, length, and height of landforms. Geologic
maps show the distribution of different rock units and geologic features, such as faults, at the
surface of the Earth. In this lab you will become familiar with both types of maps which are
important tools for anyone studying the earth or its resources. Learning Outcomes - Explain how
contours are used to show elevation information and landforms on a map. (questions 13) -
Understand and explain different types of map scale, such as fractional scale and bar scale.
(questions 4-5) - Explain how latitude and longitude are used to describe location. (questions 6-8)
- Draw and use contours to visualize spatial data (such as spot elevations). (question 9) - Find the
latitude and longitude of a location on a map. (questions 10, 17, 18) - Read elevation data and
interpret contours on a topographic map.(questions 11, 12, 19) - Calculate elevation change and
gradient (slope) from topographic maps.(questions 13, 21) - Read distances on a map using a
ruler and bar scale.(questions 14-16; 20) - Interpret ages of rock units on a geologic map
(questions 22-23) - Identify geologic structures on a geologic map (questions 24-27) - Draw a
geologic cross section using locations of contacts and angles of dip on a geologic map (questions
28-30) - Identify types of folds or faults on a geologic cross section (questions 28-30) Map
Coordinate Systems A coordinate system allows us to describe the location of any point on the
surface of the Earth. Lines of latitude (also known as parallels) are the horizontal lines that circle
the globe. These lines are known as parallels because the run in the same direction as (are
parallel to) the Equator. The Equator is the imaginary line located at 0 latitude and is halfway
between the North Pole and the South Pole, which are 180 apart. This means the South Pole is 90
S and the North Pole is 90N. Lines that run from the North Pole to the South Pole are lines of
longitude (also known as meridians). The line at 0 longitude is the prime meridian and runs
through the Royal Observatory in Greenwich, England. Meridians are counted east and west from
the prime meridian up to a maximum of 180 longitude at the.
A research on resistivity measurements on wadi el nakhel
The aim of the study:- investigate the subsurface geological and hydrogeological conditions in
this area, Using Terrameter SAS A300 and made Schlumerger array to measure the apparent resistivity to get a 2D Electric Cross Section and determine the aquifer layer depth.
Toposheet indexing .
Indexing of toposheets, in Introduction to Million sheet, degree sheet, toposheet, and their scales.
Some practice questions based on toposheet indexing and map scale has also been given for best practice.
Two babies in a maternity ward have lost their identity bands and oth.pdf
Two babies in a maternity ward have lost their identity bands and other paperwork was lost.
Baby \#1 is type A and baby \#2 is type B. Betty is one of the mothers and she has type O. Which
of the following responses will you give to Betty based only on the blood types? The type B
baby belongs to Betty Either baby could belong to Betty The type A baby belongs to Betty.
Neither baby could be hers. Incorrect. Remember, her genotype is "ii".
Twenty-two true-false statements appear below. You must answer all of.pdf
Twenty-two true-false statements appear below. You must answer all of them. For each
statements you answer, insert "T" or "F" in the appropriate place on the separate answer sheet. 1.
Jury duty pay is excluded from gross income. 2. A item of small value, a Christmas ham for
example, given by an employer to an employee must be reported as gross income by the
recipient employee. 3. A compensatory damages payment received by a taxpayer as a lump sum
on account of sickness will be included in the taxpayer's gross income. 4. A disabled spouse, age
27 , is eligible to be a qualifying person under an employer maintained dependent care assistance
program. 5. If a dependent child receives Social Security benefits, the benefits, if taxable, will be
taxable to the taxpayer(s) claiming the dependency deduction. 6. Payments received under
workers' compensation acts are generally included in gross income. 7. Per the constructive
receipt doctrine, a cash basis taxpayer receives income when it is credited to a taxpayer's
account, or set apart for him/her, or otherwise made available for him/her to draw upon at any
time. 8. A tenant renting business-use property who reports on the cash basis of accounting is not
allowed to claim a deduction for a payment of rent in advance, but must wait until the year in
which the payment was due to claim the deduction. 9. Security deposits received by a landlord
from tenants are not picked up in the landlord's gross income unless they are to be returned to the
tenant upon termination of the lease. 10. An amount paid by the Veterans Administration to a
family member of a military disabled veteran as a subsistence allowance is excluded from gross
income. 11. An employee achievement award (under a nonqualified plan) in the amount of
$1,600 to employee Anne Able would not represent taxable gross income to Anne, 12. Gross
income may be received via cash, receivables, property, and land, but not any any other form of
economic benefit. 13. Payments received by a landlord from a tenant in exchange for a
modification of the lease are not included in the gross income of the landlord..
More Related Content
Similar to Understanding regional tectonics using beach balls Part I Remember b.pdf
Structural Analysis and Tectonic Evolution based on Seismic Interpretation in...
the subsurface tectonic evolution of the East of Nile valley (EON) of the Beni Suef basin, Egypt, were
studied using twenty seismic profiles representing the desired structural framework of the EON - four of these
were selected for illustration - supported by the vertical seismic profile (VSP) logs of three deep wells drilled in
the study area. In addition, the analysis encompasses the detailed investigation of two (TWT) two way time
structure-contour maps and the rose diagrams representing the general trends of the recorded fault systems.
The study proved that the Upper Cretaceous rocks were dissected by systems of normal faults, trending in
WNW-ESE, NW-SE. These fault systems were originated in association to Cretaceous-Early Tertiary tectonic
deformations related to the Tethyan plate tectonics.
1 How does a topographic map show the shape of the land sur.pdf
1. How does a topographic map show the shape of the land surface? For example, how do
topographic maps indicate steeper slopes? How are gentler slopes portrayed? How can you
identify
stream or river valleys on maps?
2. What are contour lines? What is an index contour?
3. Define contour interval.
4. What does a fractional scale of 1:48,000 mean?
5. What is a bar scale and how is it used?
6. The basic unit of latitude and longitude is the degree. How is the degree subdivided?
7. Latitude is measured in degrees N or S of what line? What is the range of possible values (in
degrees) for latitude?
8. Longitude is measured in degrees W or E of what line? Where is that line located? What is the
range
of possible values (in degrees) for longitude?
Introduction Topograpbic maps illustrate scale, width, length, and height of landforms. Geologic
maps show the distribution of different rock units and geologic features, such as faults, at the
surface of the Earth. In this lab you will become familiar with both types of maps which are
important tools for anyone studying the earth or its resources. Learning Outcomes - Explain how
contours are used to show elevation information and landforms on a map. (questions 13) -
Understand and explain different types of map scale, such as fractional scale and bar scale.
(questions 4-5) - Explain how latitude and longitude are used to describe location. (questions 6-8)
- Draw and use contours to visualize spatial data (such as spot elevations). (question 9) - Find the
latitude and longitude of a location on a map. (questions 10, 17, 18) - Read elevation data and
interpret contours on a topographic map.(questions 11, 12, 19) - Calculate elevation change and
gradient (slope) from topographic maps.(questions 13, 21) - Read distances on a map using a
ruler and bar scale.(questions 14-16; 20) - Interpret ages of rock units on a geologic map
(questions 22-23) - Identify geologic structures on a geologic map (questions 24-27) - Draw a
geologic cross section using locations of contacts and angles of dip on a geologic map (questions
28-30) - Identify types of folds or faults on a geologic cross section (questions 28-30) Map
Coordinate Systems A coordinate system allows us to describe the location of any point on the
surface of the Earth. Lines of latitude (also known as parallels) are the horizontal lines that circle
the globe. These lines are known as parallels because the run in the same direction as (are
parallel to) the Equator. The Equator is the imaginary line located at 0 latitude and is halfway
between the North Pole and the South Pole, which are 180 apart. This means the South Pole is 90
S and the North Pole is 90N. Lines that run from the North Pole to the South Pole are lines of
longitude (also known as meridians). The line at 0 longitude is the prime meridian and runs
through the Royal Observatory in Greenwich, England. Meridians are counted east and west from
the prime meridian up to a maximum of 180 longitude at the.
A research on resistivity measurements on wadi el nakhel
The aim of the study:- investigate the subsurface geological and hydrogeological conditions in
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