Israel 2002
"Geology of the Land of Israel"
Issue Date |
18.06.2002 |
ID |
Michel: Bl. 66 (1690-1692) ;
Scott: 1483a-c;
Stanley Gibbons: MS1612;
Yvert et Tellier: BF 67 (1622-1624);
Category: pF |
Design |
Designer: M. Pereg,
Photograph: Dr. David Darom (Hebrew University) |
Stamps in set |
3 |
Value |
NIS 4.40 - ammonite, Proeucalycoceras haugi
NIS 3.40 - Blue-green stone, Elat Stone
NIS 2.20 - fossil fish, Aipichthyoides galeatus
Geological Map of Israel at MS background
|
Emission/Type |
commemorative
|
Issue places |
Mizpe Ramon |
Size (width x height) |
stamps: 26.0mm x 34.5 mm,
Mini-Sheet: 115mm x 70mm
|
Layout |
Mini-Sheet of 3 stamps |
Products |
FDC x1 |
Paper |
|
Perforation |
14 x 14 |
Print Technique |
Offset lithography, multi-color |
Printed by |
Government Printers |
Quantity |
|
Issuing Authority |
Israel Post |
On June 18
th, 2002, the Post Authority of Israel issued the set
of three stamps "Geology of the Land of Israel".
These stamps were printed as a Mini-Sheet with Geological Map of Israel on the
margins.
The following text was written by Dr. Zeev Levy fom Geological Survey of Israel
for these stamps press release, in 2002.
During ancient geological times, the land of Israel was situated
on the north-eastern margins of a continent comprising Africa and Arabia.
An ocean named Tethys extended to the north, periodically
inundating the region.
Terrestrial sandstone, soil and marsh deposits accumulated on the
exposed land of Israel.
When the sea flooded the region, it deposited limestone and chalk
with fossils, bearing evidence of the shallow to deep marine settings.
As part of the global plate tectonic system, the Africa-Arabia continent
moved north-eastward and collided with the European-Asian continent.
The resulting faulting and folding of the sedimentary strata in the land
of Israel further intensified during the younger faulting event along
the Dead Sea- Red Sea Rift Valley.
These processes shaped the topography of the country and are still active
as indicated by earthquakes in the region.
Of particular morphological and geological interest is
Makhtesh Ramon, the
largest of the Negev erosion valleys cut into an upward-folded
geological structure.
These valleys are entirely surrounded by cliffs, comprising a single narrow
outlet to the southeast, thus recalling a crater (mortar), called in Hebrew, Makhtesh.
The elongated erosion valley of Makhtesh Ramon exposes ancient marine and terrestrial strata,
intrusive magmatic and volcanic rocks and other remarkable geological
phenomena.
Makhtesh Ramon is thus a huge Natural History Museum, which became an official
Geological Park under the initiative of Prof. Emmanuel Mazor of
the Weizmann Institute of Science.
The souvenir sheet illustrates samples from the collections of
the Geological Survey of Israel and the Hebrew University, photographed
by Dr. David Darom (Hebrew University).The geological map of Makhtesh
Ramon area illustrates the first day cover.
A reduced geological map of Israel is in the center of the souvenir sheet and
a view of sedimentary layers in Nahal Ardon in east
Makhtesh Ramon intruded by a vertical dyke, is on the left.
- The fossil fish, Aipichthyoides galeatus, is one of many
vertebrate remains of great scientific significance, found in the
country.
- The ammonite Proeucalycoceras haugi is a mollusk-conch fill of
an extinct nature, related to extant octopods and squids.
Ammonites are among the important fossils, defining geological periods.
- The blue green Elat Stone, frequently incorporated in Israeli
jewellery, consists of some of the copper minerals mined in the Timna
area (north of Elat) since about six centuries ago.The modern Timna
mine was active between 1958 and 1976.
The souvenir sheet was prepared in collaboration with the
Geological Survey of Israel, which is the governmental institution
investigating the country's infrastructure, natural resources
(including water) and evaluating geological and ecological hazards.
Products
FDC |
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|
|
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References:
Acknowledgements:
- Many thanks to Dr. Peter Voice, PhD Department of Geological and Environmental Sciences, Western Michigan University, USA,
for his help in finding information and for review of a draft of this article.