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Changunarayan Hill is Cracking: Is Anyone Listening? By HARI K. SHRESTHA Cultural Heritage and Changunarayan Hill :
UNECSO defines cultural heritage as the entire spirit of people in terms of values,
action, works, institutions, monuments and sites. A designated cultural heritage site
provides a reference to understand peoples value system. The cultural heritages also
contribute to establishing and maintaining peace among people of various cultural
backgrounds. As such, the value of such heritage is not limited to a single nation or
people; it must be viewed as the global property. Recognizing the enormous cultural and
architectural value of various structures in the Changunarayan Hill, UNESCO listed the
hill and other structures, including Changunarayan temple, in the hill as a World Heritage
Site in 1979. Located at an altitude of 1541 meters, on the western hillock of the
Dolagiri ridge, one can get a magnificent view of Kathmandu valley from the temple area.
At the foot of the 108 steps that lead down from the main gate of the temple lies the
Shankha Daha. This temple is constructed in several concentric squares, with the innermost
square containing the statue of a god. For the Hindus, the god inside the temple is
Narayan and for the Buddhists it is Avalokiteshvara. So, this temple is a symbol of
religious harmony.
The temple dates back to 325 A.D.
King Haridutta Varma built the shrine along with the temple of Goddess Chhinnamasta
Adidevi. Lichhavi King Manadeva erected a stone pillar, dated 464 A.D., with inscription
written on it which is the base for considering Changunarayan temple as the oldest
specimen of pagoda architecture in Kathmandu Valley. The present form of the outer visible
superstructure of the temple was rebuilt in 1702 AD. The temple site with its close surroundings
has been declared as a protected Monument Zone by the Warning Signs in and around Temple
Premises The Changunarayan temple is a masonry
structure. The outer brick wall of the temple showed signs of twisting and tilting. The
wall tilting is one of the early indicators of possible beginning of landslides. Various
other parts of the temple also exhibit tilting. The wall of the temple is coming apart The Changunarayan hill is one of the few
sites in Nepal listed under the World Cultural Heritage Site. The hill houses the most ancient temple of
Kathmandu Valley. There are numerous land cracks at various locations around the hill and
structural cracks in the temple itself, providing early warnings of an impending landslide
that can have catastrophic and irreversible effect on this site. No one seems to be
listening to the early warnings and no agency seems to be responsible for the protection
of the hill. Sand mining is accelerating at the base of Changunarayan hill and at Manohara
River. The old ways of flood irrigation in agricultural fields is continuing. Trees are
falling and new constructions are going on in the hill without paying any heed to the
warning signs. It is time to listen, learn and act accordingly. Bricks in the upper floor of the temple
have separated from each other at the mortar joints. The wooden frames of some of the
doors of Changunarayan temple have tilted, indicating possible beginning of landslide. The
base of at least one main door frame has been lifted in one side. Some wooden frames have
protruded from its base. If no preventative actions are taken in time, the damages will
progress further. The bulging of stone steps, which is the
main access to the temple from the west side, is a clear indication of soil movement in
the Changunarayan hill. The land bulging has collapsed part of the walls on the sides of
the stone steps and displaced the stone slabs. The land bulging is a clear sign of
weakening of hill, in terms of its slope stability. Structural cracks can be seen on the
pilgrim rest houses, other buildings around the temple, and stone pavements, which are
other signs of initiation of landslide in Changunarayan hill. Pavement cracks result when
the soil underneath the pavement begins to subside. Warning Signs in Changunarayan Hill The weakening of the Changunarayan hill is
exhibited by various small and medium sized landslides, tension cracks in soil, ditch
formations etc. at various locations of the hills. Most of the evidences were noted around
places where some type of construction, such as surface drain, water supply pipe line or
foot-path have been made or around the part of the hill with human settlement. There are some ancient structures about 50
meters above the top of this landslide site. This landslide occurred probably almost a
decade ago. No protective measures have yet been taken for this landslide site. The pine
trees seen in the eastern side of the landslide were planted recently. With passing of
every monsoon season the size of this landslide is gradually getting bigger. The evidences of land subsidence (tension
cracks) can be found at various locations in Changunarayan hill. There is one such
location at the south-west part of the hill. These tension cracks in the land are some of
the clear evidences of impending catastrophic event in Changunarayan hill. Possible Reason for cracks in the
hill and temple The causes of the early warnings of
landslide potential at Changunarayan hills can be many. Only a detailed study will pin
point the exact causes. However, some of the possible reasons are apparent. There are
various settlements and agricultural fields on top of relict landslides in Changunarayan
hill. Various developmental activities are carried out around human settlement without
understanding the geology of the area, which weakens the hill. High water demanding
agricultural activities also makes the hill sides more vulnerable as water seeps down and
creates a favorable condition for landslides. In Changunarayan hill, the tree density has
severely reduced during the past decade with consequent erosion of the slopes. Much of the
forests have disappeared and hillside erosion is evident. The rate of sand mining from the
bases of the hills and from the river that runs through the base of the hill is
accelerating. Under the Local Self Governance Act-1998, the local authority (Village
Development Committee) has issued licenses to contractors for sand mining from the bases
of Changunarayan hill to enhance revenue collection. The river sides are also cut to
increase sand yield. Illegal sand mining is also going on at rapid rate from Manohara
River. The river bed of Manohara River has
declined causing collapses of river banks. A bridge over Manohara River at Sano Thimi has
collapsed and a new bridge was recently constructed. This action of sand mining is
exacerbating the fragile slope stability problem of the hill. New constructions in the
Changunarayan hill is going on with very little regard for the effects on slope stability
measures and on cultural integrity of the World Heritage site itself. In fact, UNESCO has
recently warned Nepal to take out Kathmandu Valley from the list of World Heritage site if
new constructions incompatible with UNESCO criteria around the heritage sites are not
stopped. Natural causes such as weak geological formation and intense rainfall can also
make a hill more prone to landslide. As per the geological map prepared by Department of
Mining and Geology, Changunarayan hill consists of relatively strong formation in the
upper and eastern part of the hill. The lower part of the hill in the north, west and
south is composed of loose unconsolidated alluvial deposits consisting mostly of sandy
silt and sandy clay. Layers of sand, silt and clay can be seen
in differing succession and composition. The relatively weak and erosion prone formation
at the base of the hill indicates the sensitivity of the hill towards activities that may
initiate soil erosion. Changunarayan hill experiences occasional intense rainfall in the
monsoon season. The high intensity rainfall dislodges soil particles and creates ditches.
The ditches turn into gullies which transport more soil particles downhill. This process
eventually leads to landslide event. Kathmandu Valley is situated in an
earthquake prone area. The earthquake events loosen contact between soil particles and
reduce soil strength which can trigger landslides. The silty sand, as found at the bottom
of Changunarayan hill, normally tends to have high conductivity value which facilitates
rapid infiltration of rain water. The infiltrated water raises water table elevation and
pore water pressure. The rise in pore water pressure can cause landslide by reducing soil
shear resistance. Time to Listen Nature is ringing enough warning bells to
awaken us and to take note of the impending disaster in a very important cultural heritage
of Nepal. It is time to listen, learn and act properly in time before it is too late. (The writer is associated with
Nepal Engineering College and is currently a Doctoral Candidate at Ehime University,
Japan) The Changunarayan hill is one of the few
sites in Nepal listed under the World Cultural Heritage Site. The hill houses the most
ancient temple of Kathmandu Valley. There are numerous land cracks at various locations
around the hill and structural cracks in the temple itself, providing early warnings of an
impending landslide that can have catastrophic and irreversible effect on this site. No
one seems to be listening to the early warnings and no agency seems to be responsible for
the protection of the hill. Sand mining is accelerating at the base of Changunarayan hill
and at Manohara River. The old ways of flood irrigation in agricultural fields is
continuing. Trees are falling and new constructions are going on in the hill without
paying any heed to the warning signs. It is time to listen, learn and act accordingly. |
|| Cover
Story || A Political Move || Lessening Confusion || Sudden Acceleration || Interview || Sustained
Efforts || |
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