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Chartership Interview - partial portfolio
presentation For the
Geological Society of London
By –
Dr. Ram BEN-DAVID
March 30th 2016
Presentation Overview
 Mining projects
a. The on-going gold exploration project of
Sakassou, Cote d’Ivoire;
b. The Shefa Yamim Ltd. Exploration project,
Northern Israel.
 Geo-engineering projects
a. Coastal cliffs stability – the geological
problems and engineering solutions;
b. Tunneling – rock strength and geo-
engineering supervision in Jerusalem.
The Sakassou project, Cote d’Ivoire
1. Points on the geology of Cote d’Ivoire geology
• Paleoproterozoic Birimian Supergroup (~2.15-2.2 Ga) – extensive
sediments and volcanics (‘green stone’) ~10,000 m thick section;
• Forming NE-SW structures or belts;
• The metamorphism, deformation and extensive intrusive activity are
part of the Eburnean thermo-tectonic event (orogenic cycle, ~2.1 Ga);
Yamoussoukro
permit
2. Zoom from the Cote d’Ivoire geology to the
Sakassou framework
1st. Phase –
Soil Sampling –
1: 1009
2nd. Phase –
Soil Sampling –
2: ~6000
Local mining
activities
Geological Map of
Cote d’Ivoire
Regional topo-map of
Bouake area
Generalized geological map of the
Sakassou Permit
3. First results and further exploration steps
Structure A1
Structure A2
Structure B
helicopter-borne
geophysical survey for
approximately 1,944 line-
kms of VTEM Plus and
magnetics
The suggested Birimian
structure Coincides with soil
sampling results
Soil sampling results of 1st
sampling stage
Trenching program
4. Some field observations
Altered yel/red
schist, sometimes
greenish
+ qtz. veins.
Mineralizations in
all directions.
9 m
Sample n° TSG-14 From pit base
Sulfidic schist
Iron Oxide schist
Pit N° 17
laterite
The Shefa Yamim Ltd. exploration
project, Israel
1. General overview -
• Some evidences indicate kimberlite potential along the Mount
Carmel Ridge;
• Sediments derived from the Carmel, and maybe from the Lower
Galilee may suggest the existence of precious minerals in the
alluvial deposits of the Yizre’el and Zevulun valleys;
• Shefa Yamim Ltd., has received renewable exploration/prospection
licenses since 1999;
• The company had already raised >15M $ in the Israeli Stock
Exchange, promising huge revenues when discovering the main
sources.
2. My role –
• I was appointed as Chief geologist (on a retainer basis) on June
2013;
• My main tasks were: (1) To develop exploration programs, (2)
produce geological reports for the state officials as well as to the Tel
Aviv Stock Exchange.
Source: Segev, 2009, Cretaceous Research
~100 Ma Volcanic activities of basic
pyroclastics and few lava flows
represent the 4th tecto-volcanic
event of the Levant.
The Shefa Yamim claim: the close to
kimberlite composition may produce
diamonds.
3. Some geological background
PERMIT
206
PERMIT 221
PERMIT 222
4. The exploration permits projected on
geological maps
**
*
*
*
**
*
*
*
*
*
**
*
*
5. Difference perspective of the prospection programs
Coastal cliff stability along the
Mediterranean Sea – Geological problems
and Engineering Solutions
1. The problem
• The friable geological section retreats in rates of 20-
50 cm/y.
• The sea level rise and the urbanization stress create
the need for comprehensive and durable solutions.
2. The project
10 km The Israeli government has decided to
stabilize several sections along the Israeli
coast
 The sections were defined in the National
Master Plan no. 13.
 A budget of 0.5 billion NIS (>90,000,000 £)
was defined–
- To plan in detail each of the 6 major
zones shown on the map;
- To concretize the projects in terms of
architecture and engineering;
 Our role –
- Geological mapping of many of the
different segments (in red);
- Define the geotechnical problems;
- Advise on optimal solutions.
Tel-Aviv
3. Points on the geology of the East Mediterranean
sea-shore
 The geology of the cliff section is composed mainly of Upper
Pleistocene sandstone units (locally called Kurkar) which were
deposited as near-shore dunes and clayey-sand soils (locally
called Hamra);
 Their age ranges, by OSL dates, from ~60 KaBP to ~5KaBP;
 The extensive weathering of the cliffs occurring along the coast
are due to the ingression of the Mediterranean Sea since the
Late Pleistocene glacial;
 The seashore is covered by yellowish quartz sand which
accumulates due to northward and north-eastward flowing sea
currents transporting sand from the Nile cone;
4. The five geological units recognised in the cliff
succession, their geotechnical properties and few
observations
Apolonia park
north
TE
NE
DO
NA
RA
Angle of
internal
friction
Cohesi
on
(Kpa)
Humidity
before/after
rain
)%(
Porosity
)%(
Textur
e
Age
(KA)
OSL
Slope
angle
(degrees
)
Thick
ness
Geol. unit
S---------0-5
Ta’arukha &
Hadera
38-45
170-
600
0.530-50S5-1080-901-5Tel Aviv
35102/8-23-------CL10-2020-902-8Netanya
35-3700-3/84-32S48-5330-503-10Dor
55-901.5--------SL50-5760-850-5Nachsholim
33-43300-2/7.52-23S59-6460-9016-22Ramat Gan
‫מל‬698
2000
PS3
1944
Retreat rates of the Apolonia cliffs: 1944-2000
Apolonia
Castle
notch
notch
5. Some architectural and engineering solutions
The great Jerusalem underground
parking project
1. The project
 The Jerusalem new entrance is undergoing a large scale development
processes including –
- New underground railroad station (80 m below surface);
- A new CBD;
- A new underground “Park & Go” parking zone - our project.
 The Underground Parking project includes –
- The major part - 2 spaces of 250(L) X 16(W) X 26(H) m;
- Rock cover – 6-10 m;
- Distance between the 2 spaces sides – 6 m;
- Secondary part – entrance/exit accesses tunnels of 90 X 2 m.
 Our role –
- Intensive supervision of tunneling processes;
- Rock quality description and designation;
- Providing real-time tools for the engineer for supporting requirements.
Main underground space
Project layout
Longitudinal section
Main underground space
Max – 10 m
2. Geological background
Kuw(y)
1 km
The project (approx.)
Main phenomena:
Dolomite
And karst
3. Geoengineering escort of tunnel construction
Time and age enhance my curiosity and
my willing as a geologist to explore the
world in general and earth in particular.
The experience of some 30 years just gives
wider and modest perspective of life.

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Chartership_Interview. LinkedIn

  • 1. Chartership Interview - partial portfolio presentation For the Geological Society of London By – Dr. Ram BEN-DAVID March 30th 2016
  • 2. Presentation Overview  Mining projects a. The on-going gold exploration project of Sakassou, Cote d’Ivoire; b. The Shefa Yamim Ltd. Exploration project, Northern Israel.  Geo-engineering projects a. Coastal cliffs stability – the geological problems and engineering solutions; b. Tunneling – rock strength and geo- engineering supervision in Jerusalem.
  • 3. The Sakassou project, Cote d’Ivoire 1. Points on the geology of Cote d’Ivoire geology • Paleoproterozoic Birimian Supergroup (~2.15-2.2 Ga) – extensive sediments and volcanics (‘green stone’) ~10,000 m thick section; • Forming NE-SW structures or belts; • The metamorphism, deformation and extensive intrusive activity are part of the Eburnean thermo-tectonic event (orogenic cycle, ~2.1 Ga); Yamoussoukro permit
  • 4. 2. Zoom from the Cote d’Ivoire geology to the Sakassou framework 1st. Phase – Soil Sampling – 1: 1009 2nd. Phase – Soil Sampling – 2: ~6000 Local mining activities Geological Map of Cote d’Ivoire Regional topo-map of Bouake area Generalized geological map of the Sakassou Permit
  • 5. 3. First results and further exploration steps Structure A1 Structure A2 Structure B helicopter-borne geophysical survey for approximately 1,944 line- kms of VTEM Plus and magnetics The suggested Birimian structure Coincides with soil sampling results Soil sampling results of 1st sampling stage Trenching program
  • 6. 4. Some field observations Altered yel/red schist, sometimes greenish + qtz. veins. Mineralizations in all directions. 9 m Sample n° TSG-14 From pit base Sulfidic schist Iron Oxide schist Pit N° 17 laterite
  • 7. The Shefa Yamim Ltd. exploration project, Israel 1. General overview - • Some evidences indicate kimberlite potential along the Mount Carmel Ridge; • Sediments derived from the Carmel, and maybe from the Lower Galilee may suggest the existence of precious minerals in the alluvial deposits of the Yizre’el and Zevulun valleys; • Shefa Yamim Ltd., has received renewable exploration/prospection licenses since 1999; • The company had already raised >15M $ in the Israeli Stock Exchange, promising huge revenues when discovering the main sources. 2. My role – • I was appointed as Chief geologist (on a retainer basis) on June 2013; • My main tasks were: (1) To develop exploration programs, (2) produce geological reports for the state officials as well as to the Tel Aviv Stock Exchange.
  • 8. Source: Segev, 2009, Cretaceous Research ~100 Ma Volcanic activities of basic pyroclastics and few lava flows represent the 4th tecto-volcanic event of the Levant. The Shefa Yamim claim: the close to kimberlite composition may produce diamonds. 3. Some geological background
  • 9. PERMIT 206 PERMIT 221 PERMIT 222 4. The exploration permits projected on geological maps
  • 11. Coastal cliff stability along the Mediterranean Sea – Geological problems and Engineering Solutions 1. The problem • The friable geological section retreats in rates of 20- 50 cm/y. • The sea level rise and the urbanization stress create the need for comprehensive and durable solutions.
  • 12. 2. The project 10 km The Israeli government has decided to stabilize several sections along the Israeli coast  The sections were defined in the National Master Plan no. 13.  A budget of 0.5 billion NIS (>90,000,000 £) was defined– - To plan in detail each of the 6 major zones shown on the map; - To concretize the projects in terms of architecture and engineering;  Our role – - Geological mapping of many of the different segments (in red); - Define the geotechnical problems; - Advise on optimal solutions. Tel-Aviv
  • 13. 3. Points on the geology of the East Mediterranean sea-shore  The geology of the cliff section is composed mainly of Upper Pleistocene sandstone units (locally called Kurkar) which were deposited as near-shore dunes and clayey-sand soils (locally called Hamra);  Their age ranges, by OSL dates, from ~60 KaBP to ~5KaBP;  The extensive weathering of the cliffs occurring along the coast are due to the ingression of the Mediterranean Sea since the Late Pleistocene glacial;  The seashore is covered by yellowish quartz sand which accumulates due to northward and north-eastward flowing sea currents transporting sand from the Nile cone;
  • 14. 4. The five geological units recognised in the cliff succession, their geotechnical properties and few observations Apolonia park north TE NE DO NA RA Angle of internal friction Cohesi on (Kpa) Humidity before/after rain )%( Porosity )%( Textur e Age (KA) OSL Slope angle (degrees ) Thick ness Geol. unit S---------0-5 Ta’arukha & Hadera 38-45 170- 600 0.530-50S5-1080-901-5Tel Aviv 35102/8-23-------CL10-2020-902-8Netanya 35-3700-3/84-32S48-5330-503-10Dor 55-901.5--------SL50-5760-850-5Nachsholim 33-43300-2/7.52-23S59-6460-9016-22Ramat Gan
  • 15. ‫מל‬698 2000 PS3 1944 Retreat rates of the Apolonia cliffs: 1944-2000 Apolonia Castle notch notch
  • 16. 5. Some architectural and engineering solutions
  • 17. The great Jerusalem underground parking project 1. The project  The Jerusalem new entrance is undergoing a large scale development processes including – - New underground railroad station (80 m below surface); - A new CBD; - A new underground “Park & Go” parking zone - our project.  The Underground Parking project includes – - The major part - 2 spaces of 250(L) X 16(W) X 26(H) m; - Rock cover – 6-10 m; - Distance between the 2 spaces sides – 6 m; - Secondary part – entrance/exit accesses tunnels of 90 X 2 m.  Our role – - Intensive supervision of tunneling processes; - Rock quality description and designation; - Providing real-time tools for the engineer for supporting requirements.
  • 20. 2. Geological background Kuw(y) 1 km The project (approx.) Main phenomena: Dolomite And karst
  • 21. 3. Geoengineering escort of tunnel construction
  • 22. Time and age enhance my curiosity and my willing as a geologist to explore the world in general and earth in particular. The experience of some 30 years just gives wider and modest perspective of life.