Tuesday 29 January 2013

Conservation technologies for archaeological sites and artifacts


  Conservation technologies for archaeological sites and artifacts

 Conservation of archaeological sites
Excavation and conservation technology              
 Archaeological sites which have been excavated are usually backfilled for preservation. Structural components which are difficult to conserve in their original, unearthed state when using the backfilling method, such as pillar bases and platform exteriors made of tuff, are subjected to preservation treatment after removal from the site. However, the ideal situation would be to preserve the excavation site as is, with the entire site exposed, without backfilling or removing site components.
   When an excavation is carried out with a view to preserve and organize the site post-excavation,
conservation technology becomes involved in a variety of forms. Investigating the material and
structure of unearthed artifacts and remains yields important information in determining the
archaeological nature of the site. An environmental investigation is also needed to find out the
geographical conditions of the site as well as the state of preservation of the remains. Ultimately, it
becomes necessary to formulate a conservation plan which takes all of this information into account
in a comprehensive manner.
Conservation on siteRemains situated in dry soil can be impregnated with a material such as
synthetic resin to strengthen and stabilize the structures. However, in light of the weather resistance
of synthetic resins and the structure of the remains, it is not an easy matter to carry out conservation
in conditions exposed to direct sunlight and precipitation. Generally, a protective structure such as a
cover or roof is installed over such sites for display and conservation, even when they are hardened
with synthetic resin. In cases such as kiln sites, where the structure is three-dimensional and the
ceiling portion has collapsed, a partial restoration may be performed which also serves to support
and bolster the overhanging walls of the kiln. The ceiling portions are restored with hard urethane
foam, which is lightweight and can be shaped freely. By partially restoring the ceiling, the structure
of the kiln body can be more concretely presented for effective display and conservation.
   The conservation of remains made of rock, such as foundations and platform exteriors, is also
important. On the earth’s surface, rocks are vulnerable to accelerated weathering from physical,
chemical, and biological forces due to direct exposure to sunlight (temperature etc.), wind, rain,
weather damage (moisture, wind, sand, acid rain, etc.), and salts. Of course, it is often the case that
rocks which were underground for long periods have also deteriorated due to such effects as
moisture.
   There are several types of weathering depending on the type of rock. Plutonic rocks such as
 granite have large grain sizes and break up into fine gravel, granules, and sand due to the loss of
 cohesion among crystals with the disintegration of feldspars, micas, and, in some cases,
  hornblendes. Volcanic rocks such as andesite’s are relatively likely to retain their shape, but even so
  the substrate (glass) of the surface layers has often undergone degeneration from hydrolysis and the
  feldspars which are present as phenocrysts have dissolved and disappeared. In general, black
  colored andesite’s have become whitened. Moisture-logged portions may have turned into clay.
  Pyroclastic rock, such as tuff, have weak consolidation to begin with (welded tuff has strong
  consolidation) and is prone to weathering. Porous by nature, tuff develops more cavities and spaces
  when weathered and becomes more absorbent of water. Needless to say, when severely weathered
  it becomes argillaceous, or clay-like. Tuff with high moisture content when unearthed must be kept
  from rapid drying, as it will begin to crack when allowed to dry quickly. The same thing can be
  said for sedimentary rocks such as sandstone. Generally speaking, rock which has deteriorated and
  developed many spaces will absorb more moisture, and will undergo more damage from freezing
  and thawing. Therefore, when excavation is performed during the winter, there is a need to protect
  the structures from freezing by applying a sheet over a thick layer of protective material such as
  unwoven fabric.
    In performing conservation treatment, there is a need to strengthen the deteriorated rock and apply
a water repellant finish to decrease moisture absorption. However, when strengthening the rock, care
must be taken not to apply a coating which suffocates the rock. Impregnation is carried out with
synthetic resins or strengthening/water repellant impregnates such as alkyl silicate. There is a need
to devise ways to ensure sufficiently effective impregnation of the entire structure, as insufficient
impregnation of the agent into the interior of the structure results in unevenness of strength, cracking,
and separation of strata, and possible peeling of the surface in future. The dipping method, in which
the structural component is immersed directly into the impregnate, and the continuous spray method,
in which the impregnate solution is sprayed onto the rock, are some of the methods used to
impregnate the rock effectively with the preservative.
Conservation through relocation etc.  In not a few cases, important archaeological structures
found through excavation cannot be preserved on site. Or, in many cases a portion of the cultural
layer or shell midden must be cut out and transported indoors for close inspection. Archaeological
structures thus removed can be utilized as effective displays in museums and resource centers. In
such cases, hard urethane foam can be used to package the structure for removal and transportation.
There are a variety of types of urethane foam. The type used for the removal of archaeological
artifacts and structures is the kind where two liquids are combined and mixed together to create foam.
It is capable of filling narrow, confined, irregular spaces completely with foam, allowing for
complete on-site wrapping of intricately configured archaeological structures.
    Recording the horizon of the geologic strata is also important in the disciplines of geology,
prehistory, archaeology, and soil science. In Europe, methods of taking thin film cross-sections of
sedimentary strata for the purpose of preserving profiles of geologic strata have been studied and
developed over a long period of time. There are two types of resin which have been developed for
the purpose of collecting thin layers of soil strata in archaeological excavations: epoxy resin and
polyurethane resin. Epoxy resin can be used for dry soil, and is characterized by its high strength and
for having virtually no shrinkage during hardening. Polyurethane resin, on the other hand, is
advantageous in that it can be used for damp soil strata, and has an extremely wide range of
application. When used for soil stratum transcription, the resin is applied to the surface to be
transcribed, to which gauze or other backing material is made to adhere to, and over which the resin
is applied again. When the resin is completely hardened, it is rolled up and peeled off the soil strata.
After the transcription is washed with water, it is subjected to surface treatment with resin, and
affixed to a panel or similar backing for display and/or conservation.
        Conservation of archaeological artifacts
Investigation of the excavation environment Prior to subjecting an archaeological artifact to
conservation treatment, it is important to investigate the kind of environment it was unearthed in, so
as to consider what kind of conservation treatment to carry out, as well as the environment in which
to conserve it prior to and following such treatment. That is, by investigating the underground
environment of the artifact, we can explore the factors behind its deterioration and/or weathering,
and use the information to identify the state of deterioration or to consider methods of conservation.
Furthermore, this information is utilized when designing programs for the storage and display of
cultural properties: conditions such as the appropriate temperature, humidity, and lighting, as well as
the structural design of air conditioning equipment and storage facilities.
   Specifically, measurements are taken of the temperature and humidity, and analyses are performed
of the soil and water quality, to determine whether the artifact had always been kept in dry
conditions, whether there were great fluctuations in temperature, the characteristics of the soil, etc.
When handling metal artifacts, the chlorine concentration in the soil provides a wealth of
information in regard to how to carry out the subsequent conservation treatment.
Removal of the artifact    Archaeological artifacts which have remained relatively strong can be
removed as is, without any special measures, as long as care is taken. However, in many cases the
artifacts are in an advanced stage of corrosion and/or deterioration, and any attempts to remove them
as they are may result in damage to the artifact’s shape. Materials used for the removal of such
fragile artifacts include hard urethane foam, mentioned above in the description of transporting
archaeological structures, liquid nitrogen, or resin.
   Dry artifacts are brushed with alcohol to remove the sand and soil on the surface to the degree to
which it is possible. On-site cleaning should be kept to a minimum to avoid any loss of information
that the artifact may hold. After drying, acrylic resin is applied to the artifact to strengthen it
temporarily. When the use of acrylic resin alone is not sufficient, or when the artifact is broken into
many fragments, several sheets of finely cut up gauze are pasted together and backed with resin
before removal of the artifact. After taking the artifact indoors, a solvent (acetone, toluene, xylene,
etc.) can be used to take the gauze off, little by little.
   Particularly special care must be taken when performing on-site cleaning of artifacts which are
moist, as there is a possibility that the soil around it also contains textiles or other organic artifacts. If
alcohol dehydration or air drying is possible; the aforementioned treatment can be carried out. When
drying is not possible, water soluble acrylic resin may be used for treatment, or hard urethane foam
may be utilized to cut out the artifact complete with the surrounding soil, and wrap it for removal.
Plaster of Paris was often used in the past for the removal of fragile artifacts. However, because it is
laborious and time-consuming to remove the plaster afterward, and in order to avoid inadvertent
shaking etc. of the artifact, it is advisable to avoid the use of plaster. Also, when the artifact has a
high moisture content making the above-mentioned work difficult, it may be possible to use liquid
nitrogen to freeze the entire artifact with the soil around it for removal. However, it will thaw in a
short time and there must be steps taken to ensure the shape can be maintained, by the use of
urethane foam for example.
Materials analysis          The conservation science of cultural properties begins with the analysis of
its material. Materials analysis is performed first through observation with the naked eye and the
microscope, with instrumental analysis carried out as necessary. However, when analyzing valuable
cultural properties, it is preferable to do so without taking samples, that is, non-destructively. Even
in the rare case when sampling is allowed, it is needless to say that the samples must be in very
minute quantities.
   Furthermore, the conservation science of archaeological artifacts demands an accurate grasp of the
interior of the article, which cannot be seen. This is essential to elucidate the method of manufacture,
and also provides information that is important for cleaning, restoration, and other processes of
conservation. The most widely used method for investigating the interior structure of artifacts has
been x-ray radiography. In recent years, researchers have been using technologies where data is
directly digitized from images taken using imaging plates with a wide dynamic range. With this
method, it is easy to perform computerized image analysis which is difficult with film photography.
Furthermore, it is possible to extract the microstructure. At the same time, the technology of x-ray
computer tomography, wherein the interior structure can be shown three-dimensionally, has also
been introduced into the field of cultural properties, making it possible to obtain more detailed
information. Neutron radiography is also being studied and put to practical use as a method for
obtaining information that is different from that obtained through x-ray imaging.
   Another method of analysis, which is most important and has become widely used, is the
deciphering of characters written in ink on wooden strips and lacquered paper. This is performed
through the combined use of infrared TV camera and image enhancement devices to decipher
writing which is beyond the visible range of the naked eye. These devices are used to decipher
writing and drawings done in ink on pottery and metal articles in addition to those made of wood and
paper.
Conservation treatment:            Traditional methods and techniques have always been valued for the
conservation and repair of cultural properties, and the materials and technologies for conservation
have been selected with care. In particular, the conservation of artwork, handicrafts, and architecture
has relied heavily on traditional materials and methods.
   However, most artifacts unearthed in archaeological excavations do not even have known methods
of manufacture, not to mention traditional methods of restoration. These artifacts have already
undergone physical and chemical changes and are in varying degrees of degeneration, necessitating a
program of conservation treatment which makes full use of modern science.
Conservation treatment for organic artifacts :           Organic artifacts include those made of wood,
fiber, and paper, out of which wooden articles are unearthed in the highest quantities. Wooden
articles range from structural components such as pillars to containers, tools, and ornaments
including bowls and pedestal tables, not much different from the modern day. In some cases, the
wooden articles have been lacquered with urushi or bear writing done in ink (such as in the case of
wooden strips). The wooden articles unearthed in Japan are usually very fragile, with the cellulose
component largely reduced and displaced with large quantities of water. Some broadleaf materials in
severe stages of deterioration have a moisture content of 1500%. This means one kilogram of the
wood contains 15 kilograms of water. Such a piece of wood, when allowed to air dry, will undergo
such pronounced shrinkage and deformation it will no longer be possible to restore it to its original
shape.
   The most important thing in the conservation treatment of unearthed organic artifacts is to bring
them to a dry state which can withstand display and storage, without causing shrinkage or
deformation. Many methods of conservation treatment have been devised and implemented to date,
and they all have one thing in common. That is that the treatment is done in two processes:
“impregnation with a chemical agent,” and “drying/hardening with a chemical agent.”
   Impregnation with a chemical agent can be done in one of two ways. One is to take a
water-steeped article and impregnate it directly with a water soluble chemical agent. The other is to
replace the water in the artifact with an organic solvent before impregnating the artifact with a water
soluble chemical agent. When using water insoluble chemical agent for impregnation, the procedure
of replacing the water within the artifact with an organic solvent becomes necessary as a
preprocessing step. The primary objective of impregnation with a chemical agent is to strengthen the
artifact and give it dimensional stability. When replacing the water in the artifact with the
impregnating chemical agent, the impregnation step itself becomes the dehydrating process. In this
process, the important point is the osmosis and diffusion of the chemical into the artifact. Generally
speaking, when a high density solution is added to a low density solution, there is movement of
solute and solvent in an effort to make the overall density uniform. For instance, in the case of
impregnation with polyethylene glycol, the solute is polyethylene glycol and the solvent is water.
That is, the water within the artifact gradually works it way out while the polyethylene glycol or
other impregnating agent seeps and diffuses its way in as the solute and solvent attempt to equalize
the density inside and outside the artifact, and the water is progressively replaced with the chemical
agent. The troublesome thing about the process of impregnation with a chemical agent is that the
osmosis and diffusion of the chemical agent is not only dependent on the nature of the chemical but
also greatly influenced by the properties of the archaeological artifact, such as the type of artifact,
the species of wood, and the state of deterioration.
   Once the impregnating step is complete, the artifact proceeds to the “drying/hardening with a
chemical agent” step. When replacing the entire water content of the artifact with a water-soluble
chemical agent, the final step is heating the artifact to melt the chemical impregnate and make it a
liquid of 100% concentration. Nonsalable agents which when heated become liquids of 100%
concentration can also be used to ultimately replace all of the organic solvent within the artifact.
When an artifact which has thus had all of its solvent (water or organic solvent) replaced with
chemical impregnate is taken out of the processing tank and cooled, the impregnate becomes a solid
and the artifact has been strengthened in a dry state. Or, in some cases the artifact is taken out of the
tank at an impregnate concentration of 70-80% instead of bringing it to 100%. In such cases the
20-30% water or organic solvent remaining within the solution composition of the artifact is
removed through air drying or by using part of the water as water of hydration for the crystallization
of the chemical agent and allowing the rest to evaporate. In another method, freeze drying, the
impregnation process is completed with the artifact still containing a significant amount of water or
organic solvent, and the artifact undergoes drying under special conditions. The pronounced
shrinkage and deformation of an organic archaeological artifact is largely due to the surface tension
of water. When liquid water is heated, it boils at 100°C and turns to steam. However, when water is
placed in a cup and allowed to stand, the amount gradually decreases until the cup is finally empty.
As can be seen from this phenomenon, water molecules are always escaping from the surface of
liquid water in an effort to maintain constant vapor pressure, even when the water is not heated to
100°C. When this liquid water becomes water vapor, significant pull strength is generated.
   As can be seen in the everyday phenomenon of cut-up vegetables drying out when left in the
freezer, water molecules are also escaping from the surface of solids as well. The phenomenon of
solid ice turning into water vapor without first becoming liquid water is called sublimation. In
sublimation, surface tension is negligible. Freeze drying makes use of this phenomenon. In reality,
the water in the artifact is sometimes replaced with tertiary butyl alcohol for the purpose of
enhancing drying efficiency and to minimize shrinkage and deformation.
Conservation of inorganic artifacts :  Inorganic artifacts are made of a wide range of materials:
earthenware, tile, stone, glass, ceramic, porcelain, metal, etc. Out of these, metal articles are
especially prone to corrosion while buried and pose problems for conservation.
   Ancient metal articles are made of various materials. Some are made from a single material such
as iron, copper, silver, tin, or lead, while others are made of a combination of materials, such as
copper-tin alloys or copper-plated iron, where iron was covered with copper plating. In any case, all
metals except gold undergo some degree of corrosion while buried. The causes of corrosion are
oxygen, moisture, and dissolved ions, with chloride ions believed to play a particularly major role.
Such unearthed metal archaeological artifacts are subjected to scientific investigations relating to
their structure and material, and are made to undergo conservation treatment before being displayed
in public or put in storage.
   In general, unearthed metal artifacts are covered with some type of rust. The covering of rust may
have inhibited corrosion in some cases, while it may have accelerated it in other cases. In order to
control the progression of rust after unearthing a metal artifact, it is important to identify the cause of
the rust and eliminate as many causative factors as possible. Generally speaking, the causative
factors of rust in metals are oxygen and moisture as external factors and soluble salts contained in
the rust as an internal factor. Through the analysis of secondary matter, including rust, it is possible
to determine from the artifact’s history as to whether the rust will continue to progress in that
particular artifact.
   Many iron artifacts are covered with iron oxyhydroxide. There are three types of iron
oxyhydroxide known to be found on unearthed iron artifacts: alpha-, beta-, and gamma-FeOOH.
Beta-FeOOH (mineral name: akaganeite) is produced in the presence of chloride ions and
accelerates corrosion, thereby posing problems for conservation. At present, conservation treatment
is preceded by x-ray diffractometry to identify the type of rust, and by ion chromatography to
determine the quantities of anions such as sulfate ions, fluoride ions, and nitrate ions, to formulate a
program for conservation. In Japan, with its climate of high relative humidity, chloride ions are a
significant causative factor for corrosion. Desalination treatment is therefore performed to remove
these ions as much as possible. Various types of desalination processes, dry and wet (solution
method), have been devised for iron artifacts, out of which the solution method is generally used in
Japan. In recent years, methods have been developed involving the use of high-temperature,
high-pressure chambers for the extraction chloride and sulfate ions from unearthed artifacts. After
completing these types of chemical desalination steps, the artifact ultimately undergoes impregnation
with acrylic resin to strengthen it.
   Chloride ions are similarly associated with the corrosion of copper and bronze artifacts. The
presence of these ions exacerbates corrosion and destroys the artifacts. Bronze mirrors, which
appeared stable at the time of unearthing, have been known to succumb to general disintegration
after several to dozen years due to advanced pitting. This kind of phenomenon which occurs
especially in bronze artifacts is called “bronze disease.” Copper (I) chloride (mineral name:
nantokite) or hydrous copper chloride (mineral name: atacamite) is detected in the diseased parts. In
recent years, the development of the non-destructive parallel beam x-ray diffractometer has made it
possible to gain diffractometry data of rust without causing any damage to valuable cultural
properties, thereby contributing to the early detection of bronze disease.
   Bronze disease is sometimes treated by removing the causative chloride ions, but because bronze
is more prone to changes in color compared to iron, the method is difficult to employ for fear of
damaging the artifact. Therefore, methods have been developed and put into practice whereby a
protective film is generated on fresh metal parts to prevent corrosion from advancing, and to protect
the artifact from the forces of chloride ions. This is called the benzotriazole method and the principle
is a type of chemical conversion treatment. It is now used generally on unearthed copper and bronze
artifacts.
        The storage environment
   Conservation treatment does not ensure the prevention of further degradation of the archaeological
artifact. Instead, it is an attempt to inhibit further degradation as much as possible. For example,
even when a wooden artifact is successfully conserved with polyethylene glycol, placing that artifact
in high temperature and high humidity will cause the polyethylene glycol to absorb water and elute,
causing the deformation and shrinkage of the artifact as a result. Or, even when a metal artifact is
treated exactly according to theory, the rust may progress in reaction with moisture. In either case,
the problem is not about the treatment itself but is about the major influence of the storage
environment.
   In order to minimize these kinds of storage problems, there is a need to maintain the storage
environment in an optimal state. Notwithstanding the need to upgrade storage facilities so that they
can maintain a constant temperature and humidity, it is also important to deal with each artifact
individually. Generally speaking, oxygen and moisture are the environmental factors which are most
closely associated with the deterioration of artifacts during storage. Therefore, devising methods to
shield the artifact from oxygen and moisture will help to create significantly favorable conditions.
One method devised from this standpoint is the use of deoxidizer and desiccant in a bag made of
special film with extremely low air permeability. Since this method can be applied to artifacts of
different types and sizes, it can be described as an excellent method of storage. However, it is not a
permanent method and must be checked on continuously. In any case, we must recognize that
artifacts which have undergone treatment are not stable in every kind of environment and that
storage must be undertaken by checking the status on a continuous, ongoing basis.

Research on Ranikot


        SPEECH OF M. H. PANHWAR AT SEMINAR ON
                                  RANIKOT.
1. Who so ever built Ranikot fort or when they built it, will remain disputed,
unless explored by Archaeologist, but it was never occupied and cannot be
occupied in future this will remain undisputed. Climatic conditions of Sindh
were not known to ancients. They neither had concepts nor had developed
instruments to collect climatic data. All this came up in at end of 16th and
early 17th century in Europe. Surprisingly Korean had developed rain gauge
around 1400 AD, but it was not put to any scientific use. The British collected
climatic data for each Taluka head quarters from 1904 onwards. For some
cities climatic data were available from 1870s and Department of
Meteorology, Government of India had issued a booklet “Climate and Indian
Farmer” in 1945. That publication laid down information on frequency of five
inches of rainfall in one day in different areas of undivided India. Further
work on climate of Sindh by the present author showed that there can be
possibility of 5 inches of rainfall twice in even 5 years in Ghorabari-Badin
area, once in 5 years in Hyderabad-Mirpurkhas area once in 10 years in
Sann-Sakrand-Nawabshah area, once in 20 years in Moro-Dadu-Johi area
and once 33 years in Rohri - Jacobabad area. Dadu - Johi - Gaj area had
more 5 inches rainfall three times in one day in past 50 years and the area,
has seen flooding of Dadu, Johi and Sehwan Talukas in 1956, 1977 and
1994. This type of rainfall caused LBOD to breach in 2003 and flooded vast
area. In the latter case it was 5 inch rainfall within a week in three districts,
Nawabshah – Sanghar and Mirpurkhas and combined waters caused flood.
This is known for past 50 years but none seems to be planning for it.
2. Now coming to Ranikot fort, it is close to Sann-Sakrand-Nawabshah and 5
inches rainfall can occur in one day, once in 10 years. The Ranikot Fort
having circumference of 20.5 miles and nearly rectangular in shape will have
an area of about 25 square miles within its boundaries i.e., 16,000 acres. Its
three gates to south, west and north, allow rain-fed streams to bring
additional water in side the fort. Maximum contribution is from Mohan Dhoro
of Mohan Nai, catchment of which is some 50 years miles, i.e., twice as much
as that of the fort itself and this water enters the fort at Mohan gate exactly
apposite to Sann gate. The catchment of those rains fed rivers is total of
more than 50 square miles, but needs to be verified. This makes total
catchment of more than 32,000 acres and if all that rain passes through the
main gate in 12 hours it would be 13,000 cosecs, almost one and half times
that of Rohri canal at Khairpur and the same as Nara canal. To allow this
water to pass, gates should have regulator gates bigger than Rohri canal and
same as Nara canal. Such rains are occurring regularly 6-7 times each
century and therefore Sann gate will be washed away if rebuilt from time to
time. The same will be the case at Mohan gate, but it has not been verified.
It seems that it was rebuilt a few times, only to frustrate the owners, within
Speech of M. H. PANHWAR at a seminar on Ranikot Copyright www.panhwar.com      1
shortest possible time. Time and rain waited for no man. The fort has
remained unoccupied since its construction.
3. We have records Nawab Wali Muhammad Leghari, who got main gate
repaired with strong steel hinges and when rains came, gates and steel gave
away as if the latter was made with wax. This is just an example.
4. That fort was never occupied is clear from the fact that there are no old
settlements inside the fort, no places of worship, no graveyards, no pottery
shreds and in brief no information on any settlement except fort walls
repaired and renovated according to weapon of war used over centuries.
5. Such fort though strategically important hide out, 36 miles (60 kms) to
the west of the river Indus which flowed near Shahdadpur, with half of
distance through hills and would be safe from any cavalry attack, as there is
no water in the last 18 miles for animals to drink. Fort could not be safe
heaven, due to periodic heavy rainfall floods, which destroyed its main gate.
There are periodic changes made to protect fort from guns. Originally it was
for bow and arrow offence and defence, next cross bow and then against
guns and finally against muskets. These changes are systematically visible in
periodic repairs.
6. Mr. Khursheed Hassan retired Director General Archaeology has written a
book on “Forts of Pakistan” and he presented me a copy, yesterday on
(February 25). It mentions a dome near the gate, similar to the one in a
mosque at Giri near Taxila, built by the later Ghaznavids who ruled west part
of Punjab from Lahore. The date can be 11th or 12th century. It is not
inferred that peacock and buffalo engraved on it. Lion was emblem of Seljuks
(12th - 13th century) and buffalo could be symbol of Sindhi buffalo breeders
(Jats of Southern Punjab or Meds of Sindh).
7. This only establishes antiquity of fort. My opinion is permission should be
taken from Shaikh Khursheed Hassan to print 30 pages from his book on
Sindh forts as that would also throw light on the other forts of Sindh. Some
additions also show floral patterns, most probably added after 10th century.
My previous thinking (1981) that fort belonged to Bactrian Greeks or
Parthians is changeable on the ground that from 600 BC – 400 AD, the rulers
could not have been powerful enough to spend on such elaborate fort, as it
was period of severe drought world over. There was favourable climate from
500 – 650 BC, the period of Rai Dynasty of Sindh. Rai rulers were Sudras
(lowest caste in Hindu hierarchy), but were fair and just to public and such
accepted as Rajputs (sons of kings). During their period a number of
monumental stupas were also build and fort could pertain to that period, but
this too is guess work. They were in conflict with Sassanians and may have
thought of such defence, but nothing is sure.
8. My other comments are that in Quetta region, Miri means fortress and has
nothing to do with Mirs of Sindh. Fossilised trees of fort and surroundings
belong to 53-62 million years ago when Ranikot series of mountains were
Speech of M. H. PANHWAR at a seminar on Ranikot Copyright www.panhwar.com    2
laid. In the fort British geologists Blanford and others lived and explored
geology of Western Sindh between 1865 and 1879 and produced two
monumental works namely “Geology of Western Sindh” by Blanford 1879 and
Duncan and Sladen, Mem. Ind. Geol. Sur. 1871. They are useful even today.
9. Hyderabad cannot be considered as Nerunkot as most of city has been
built in 20th century and no debris of any kind are found form the ground
there. In the 8th century river flowed from Brahmanabad and one branch of
it passed east of Tando Allahyar and another through present Fruit Research
Institute Mirpurkhas. Hyderabad was at higher level than the other two and
water could not be brought there from the river to Hyderabad. Ground water
around the city of Hyderabad is brackish within 10 miles (16 kilometers) in
each direction. Nerunkot may be at the foot of Ganjo Takar hills close to
Khathar as Henry Cousins had suspected.
10. There is talk about conservation. Einstein had said; “Best is enemy of
good”, Conservation to improve old monuments is science in itself. Present
renovation of Ranikot fort amounts to destroying it. Original stone is of dark
brown colour, set in lime mortar. This stone is very hard and lime turns into
stone as it ages. Tourism Development Corporation is restoring it with white
Laki lime stone, which is softer and it is being set in cement mortar. Cement
has life of about 100-150 years and then it turns into dry dust. Lime has
indefinite life. Thus best restoration has become worse archaeologically.
Restoration is not every body’s job. It is special branch of archaeology.
11. G. M. Sayed had invited Col. Rashid, Hassamuddin Rashdi, Rabani, and
Joyo Saheb and me and arranged our visit to the fort in February 1965. Then
he followed it by involving others. In 1981 Seminar G. M. Sayed should have
been invited, but sponsors did not thing it proper. In my speech on that
occasion, I had mentioned of G. M. Sayed’s initiative and knowledge of forts.
Some speakers were not ready to hear his contribution.
Speech of M. H. PANHWAR at a seminar on Ranikot Copyright www.panhwar.com   3