DIE ERDE 143 2012 (1-2)
•
Miscellaneous Issue
pp. 49-73
Migration – Natural hazards – Coping strategies – Risky environment
Hermann Kreutzmann
After the Flood.
Mobility as an Adaptation Strategy in High Mountain Oases.
The Case of Pasu in Gojal, Hunza Valley, Karakoram
Nach der Flut. Räumliche Mobilität als Anpassungsstrategie in Hochgebirgsoasen.
Die Fallstudie Pasu in Gojal, Hunza-Tal, Karakorum
With 8 Figures, 1 Table and 3 Photos
The high mountain environment of the Hunza Valley in the Karakoram is characterised by significant
potential energy, extended glaciation and related events that tend to threaten habitations and settlements. The village oasis of Pasu is taken as a case in point to highlight adaptation and coping
strategies over a longer period. The village lands of Pasu have been shrinking over time owing to
glacier outburst floods in the upper valleys. The inhabitants of Pasu have developed a set of coping
strategies that are linked to mobility. Shifting populations to newly created irrigated oases in previously barren lands, out-migration to urban areas within the Karakoram and to metropolises in downcountry Pakistan in search of employment and education, international migration to overseas destinations, and the broadening of income generation by reducing the importance of agriculture in
favour of services and tourism are measures of adaptation that are embedded into the sociopolitical and economic framework conditions. The shrinking village lands of Pasu have posed
tremendous challenges to the mountain farmers, who have developed their own responses.
1. The Hunza Valley as a Risky Environment
On January 4, 2010 the Atabad rockfall blocked
the Upper Hunza Valley and created a lake that
extends for more than twenty kilometres northwards and interrupts access via the Karakoram
Highway to the upper villages and to China. At
the end of July, exceptional monsoonal rainfall
coincided with the peak of glacier melt from the
part of the Karakoram where more than one
third is covered by ice. The flood was disastrous
for the infrastructure of the mountain valleys
and subsequently affected millions of people in
the irrigated plains of Punjab and Sindh where
50
Hermann Kreutzmann
the water masses could not drain into the saturated soils of the most extensive and compact
irrigation oasis on earth (Kreutzmann 2010,
Kreutzmann and Schütte 2011). In this paper a
longer historical view is taken in order to investigate the hazards that have been threatening the
Karakoram oases and that have forced the inhabitants of the mountain settlements to become
experts in coping with crises and designing strategies for adaptation and mitigation. The metaphor
‘after the flood’ incorporates the pending threat
of a new hazard that is always expected in such a
mountainous risky environment.
The village of Pasu is situated at the upper end
of Atabad Lake and will be the case in point for
our argument. Its inhabitants have a long experience with environmental threats and have developed a set of coping mechanisms in response
to complex emergencies created by floods and
glacial movements that were causing blockage
of rivers and routes, subsequent dam breakages,
flash floods and debris flows destroying water
management systems and village lands.
In high mountain research, different strategies of
adaptation to challenging habitats have been discussed over time. At present, a prominent discourse is linked to climate change and its social
impact and subsequently to the potential for mitigation and adaptation. Among the numerous publications addressing climate change in mountain
regions cf. Eriksson et al. 2009, Kohler and
Maselli 2009, Spratt and Lawson 2009, UNEP
2009. From a different research perspective adaptation and coping are rooted in vulnerability research that takes into account the spatial dimensions of risk (Bohle 2007, Müller-Mahn 2012,
Wisner et al. 2004). The vulnerability framework
is embedded in “... the characteristics of a person or group and their situation that influence
their capacity to anticipate, cope with, resist and
recover from the impact of a natural hazard ... It
involves a combination of factors that determine
the degree to which someone‘s life, livelihood,
DIE ERDE
property and other assets are put at risk ...”
(Wisner et al. 2004: 11). Bohle (2007: 6) argues pointedly: “...social vulnerability will have
to analyse the options open to the vulnerable for
coping and adaptation, and the mechanisms and
structures that promote or prevent successful
livelihood activities. In risky environments it is
necessary to know the existing capacities for
sustaining livelihood security, before any political measures can strengthen or support them.”
While mitigation is out of the scope of local
people in our village setting, their everyday life
is a permanent adaptation to different challenges
originating in ecology, economy and society.
Adaptation is understood here in a broader sense
as all activities and measures that are taken by
vulnerable groups and individuals to cope with a
changed situation that was triggered by events
from the environmental, social and political
spheres. When we address resilience in the context of Pasu the capacity of mobilising human
resources needs to be highlighted and explained.
The resilience of mountain dwellers in challenging environments draws on an expertise that
should be used to cope with all sorts of crises
demanding immediate action and relief. In earlier
debates the academic emphasis was put on utilisation strategies combining resources accessible in different ecological zones. In the Andes
Robert Murra identified vertical control as a
highly sophisticated approach for establishing a
strategy to merge assets in different niches and
to disseminate risk (cf. Brush 1976a, 1976b,
1977; Guillet 1983; Murra 1985). The combination of marginal resources in their separate
settings enables the survival of mountain households whose major asset is a high degree of
mobility. In the tropical Andes, verticality is the
prime factor facilitating regular altitudinal mobility if access to scattered resources is part of
the control scheme. In the subtropical and temperate Inner Asian mountain areas, distance and
altitude are linked in a seasonal regime. Mobility connects resource-rich areas such as the high
summer pastures with permanent homesteads or,
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
51
Fig. 1 Pastoral mobility in the Hunza Valley. As an integral part of combined mountain agriculture the
distance between irrigated oases in the valley bottoms and high-lying summer pastures is covered by
herd migration. Some settlements claim pastures close-by while others manage distances between
5 and 75 km. Source: modified from Kreutzmann (2006b: 340) / Viehwirtschaftliche Mobilität im
Hunza-Tal. Als wichtiges Bindeglied der kombinierten Hochgebirgslandwirtschaft werden die
Entfernungen zwischen den Bewässerungsoasen und den hochgelegenen Sommerweiden von den
dörflichen Herden überwunden. Einige Dörfer verfügen über nahegelegene Weiden, andere legen
Distanzen zwischen 5 und 75 km zurück. Quelle: verändert nach Kreutzmann (2006b: 340)
in the case of nomadism, summer, winter, spring
and autumn pastures (Ehlers and Kreutzmann
2000, Guillet 1983, Uhlig 1995). Mobility is the
driving force enabling survival in marginal and
remote locations. Studies of mobile people have
focused on practices in the livestock sector.
Consequently, Erwin Grötzbach (1980) hypothesised that utilisation strategies of high mountain
52
Hermann Kreutzmann
DIE ERDE
Photo 1 The oasis of Pasu (2400 m) at the edge of the Hunza River with its wide bed bordered in the
northeast by steep scree slopes and rock formations culminating in Tupodan (6106 m). Photograph:
Hermann Kreutzmann, August 24th, 2003 / Die Pasu-Oase (2400 m) am Rande des weit
ausgeräumten Hunza-Flussbettes. Am gegenüberliegenden Ufer finden sich steile Schutthänge und Felsformationen, die zum Tupodan-Massiv (6106 m) gehören. Aufnahme:
Hermann Kreutzmann, 24. August 2003
pastures were an essential classification tool for
understanding cultural properties and societal
differences. Classical interpretations tended to
explain regional differences according to access
to locally available and accessible resources and
their consumption within the region. Sociopolitical embeddedness was grossly neglected
and underrated. While mobility was associated
with animal husbandry other forms of moving and
migration escaped appropriate attention. Settlements, especially when they were regarded as
permanent homesteads, counted as fixed and
immobile structural parts of human dwellings in
the mountains. Outward-oriented human mobility, encompassing migrant labourers, itinerant
traders and students, was neglected in a similar
manner (Grötzbach 1984). The assets of mountain households have been diversified over time;
non-agrarian and non-place-based resources
dominate in many cases (Kreutzmann 2006a).
Food supply is managed on a monetary exchange
basis with external producers etc. Mobility and
exchange networks along modern lines of communication have added value to the households
residing in mountain villages. Emphasising mobility as a central category and dynamic element
of flexible and responsive mountain communities might be a useful approach to investigate
vital features of mobility and to understand resilience in mountain contexts.
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
53
Tab. 1 Population change in Pasu / Bevölkerungsentwicklung in Pasu
Year
1790
1886
1921
1931
1972
1981
1989
1994
2008
2011
Households
10-12
40
22
22
45
61
70
80
120
125
Inhabitants
-
-
167
155
318
375
556
711
882
917
Source: Government of Pakistan 1975, 1984; Ismaili Council for Gulmit 1994, 2012; Lockhart and Woodthorpe 1889: 135-136;
Pal 1928, 1934, Qudratullah Beg 1962: 154
The aspects to be discussed are:
– Seasonal mobility as part of combined
mountain agriculture,
– Episodical mobility as a response to natural hazards,
– Out-migration for jobs and education as a
strategy to diversify the income structure of
mountain households,
– Tourism development as a means of reinterpreting local resources.
In the following, the case of Pasu village in the
Karakoram Mountains is discussed from different
mobility perspectives as they are reflected in the
physical and social village setup. For the meaning
of village in the context of the Hunza Valley cf.
Kreutzmann (2006a: 259ff.; 2006b: 331ff.). The
story to be told is a narrative of decline in which
local land resources dwindle while multi-facetted
external resources are tapped and integrated into
the domestic strategy of income-generation.
2. The Setting
Pasu village is located at an altitude of about
2500 m in the Hunza Valley. In an arid valleyfloor environment surrounded by towering glaciated peaks of up to 7500 m, about one third of
the Hunza Basin is covered by glaciers (Hewitt
2005; 2006: 50; Photo 1) . Thermal conditions
in the valley bottoms are ideal for combined
mountain agriculture, while water from glacier
melt is in ample supply for the settlement oases
of this area with a population density of less than
ten inhabitants per km2 in the Karakoram.
In local oral tradition Pasu is regarded as one of
the oldest Wakhi settlements in the Gojal area of
the Upper Hunza Valley (Fig. 1). The Wakhi
arrived here as migrants from the Wakhan Valley
of Badakhshan in present-day Afghanistan (Qudratullah Beg 1962: 152). As permanent settlers,
they replaced the Kirghiz nomads who had previously used the Gojal area as summer pastures.
Wakhi immigration most probably took place at
the end of the 18th and beginning of the 19th century. We have not been able to trace any earlier
written evidence but the local oral tradition relates
a much longer occupation of the oasis; the first
settlers are said to have arrived up to 400 years ago.
The recorded genealogies provide names for up to
twelve generations. The early settlement history
tells us that Pasu was an important village in
Gojal I, which was one of the administrative sections (maqsòo) of the Hunza principality. Early reports mention that Pasu was a village of substantial size; some estimated as many as 300 houses.
The first empirical colonial record originates from
the ‘Gilgit Mission’ during the last quarter of the
19th century when Pasu was reported to consist of
forty houses (Lockhart and Woodthorpe 1889:
135f.). A contemporary source gave a number of
25 houses, but its author Leitner (1891: 246) did
not visit Pasu himself as did Lockhart and
Woodthorpe (1889: 396ff.). This is nearly half
54
Hermann Kreutzmann
DIE ERDE
t
Sos
4500
280
0
260
Ba
tu
a
Gl
ra
0
ci
Hunza
er
Tupopdan
0
300
al
sh
im
Sh
Janabad
Yünzeben
25
l
msha
Shi
00
Karakor a m
Y
ü
Hi
n
gh
wa
z
y
e
S
d
a
Chaoni
a
3529
s
r
35
00
h
t
4023
t
350
0
Nobod
Pasu
Kipgar
0
00
Glac
25
Pasu
300
ier
Pasu Lake
Yashwandan
Pasugah
0
Kük
300
35
00
Pe
rig
oz
Na
la
4105
Kharamabad
00
25
Hu
nz
Shahbad
a
Zarabad
Borit Lake
00
40
3000
4128
Ghulkin
ier
Karakoram
Highway
Karakoram Highway
Main
road
Main road
Secondary
road
Secondary road
Footpath
Footpath
Hussaini
lmit
Gu
Glac
Irrigated
Irrigated
land land
and moraine
GlacierGlacier
and moraine
Settlement
Settlement
in in
metres
4023
Elevation
metres
4023 Elevation
Section
Section of
figures
figures 4, 5, 6, 7
00
1 km
1 km
(contour
(contourintervall
intervall100m)
100m)
Fig. 2 Pasu and Hussaini between the glaciers – two villages and their shifting location. From the old settlement
nuclei both villages have expanded towards neighbouring scree slopes where village lands have been
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
the size of present-day Pasu, while other neighbouring villages of Gojal, such as Gulmit and
Hussaini, have experienced a six- to eightfold
growth during the same period (Kreutzmann
1996: 282ff., 2006a). Here we find an early indication that despite its importance as a strategic settlement Pasu has fared quite differently,
losing part of its population especially in the first
half of the 20th century (Tab. 1). The village was
initially established as a fortified and compact settlement (khan) which was augmented during the
last century by scattered hamlets and individual
farmsteads on the village lands (Fig. 2). These
lands consist of an irrigated oasis where crops
such as barley, wheat, potatoes, beans and peas
are cultivated. Orchards of fruit trees such as apricot (èowan, Prunus armeniaca), mulberry
(tüt, Morus alba), peach (šaftolú, Prunus
persiaca) and apple (mür, Malus sylvestris)
form the tree plantations; in addition, there are
stands of poplar (safidor, Populus) and
seabuckthorn (zaè,
x Hippophae rhamnoides);
the latter is an important fuel for preparing meals
and provides an area where grass for winter fodder is cut and the village herds scavenge.
3. Seasonal Mobility as an Essential Feature
of Combined Mountain Agriculture
In addition to crop cultivation in the irrigated mountain oasis, vast stretches at significant distances are
incorporated into the combined mountain agriculture of Pasu. The Wakhi community of Pasu claims
55
the pastoral rights for the northern bank of the
Batura glacier (Fig. 3). Since the village of Pasu
came into existence, these pastures have been an
integral part of managing survival in this location.
Between late September and May, the herds of
sheep, goat and yaks are kept in the village and the
outlying hamlet of Kharamabad on the left bank of
the Hunza River (Kreutzmann 2004), from April
onwards they are driven towards the Batura glacier
(Photo 2). The sheep and goats cross the glacier
from Yunzeben to Yashpirt already in April; yak
cows and their calves follow by the end of May.
Pasu village has distributed the higher-lying pastures between two groups. One uses Yashpirt and
Kükhel; the other keeps its flocks in Fatma hel and
Guchesm. The non-lactating yaks are kept more than
30 km away from the village in Lupdor throughout
the year. The summer pastures along the Batura glacier are a valuable resource, providing the fodder
basis for the herds; milk is processed there for butter and qurut (dehydrated whey). These two storable commodities are brought back to the village.
Animal husbandry has always been an important basis of income generation, adding to the staples cultivated on the village lands. During the last three
decades, orchards, pastures and forest resources
have formed innovations in the cultivation at
Kharamabad and Janabad Das. Agricultural mobility today includes seasonal pastoral migration to
Batura; at the same time daily circulation between
Pasu and Kharamabad is necessary when the animals are there and when crop cultivation and harvesting are required. Some households have built
new houses in Janabad Das, but the majority of Pasu
cultivated and filial settlements established. To reach the seasonal pastures the river and glaciers have to be
crossed. Source: topography based on Hunza-Karakoram, scale 1:100000; Quickbird data, May 11th, 2007;
Generalny Stab map, scale 1:100000, sheet J_43_126; design and toponymic survey: Hermann Kreutzmann;
cartography: Bernd Hilberer / Die Lage der Siedlung Pasu zwischen den Gletschern – zwei Dörfer
verlagern sich. Aus den alten Siedlungskernen heraus wurden Filialsiedlungen und junge Fluren auf
benachbarten Schutthängen erschlossen. Die Wege zu den saisonal aufgesuchten Weideplätzen erfordern die Querung des Flusses und der Gletscher. Quelle: Topographie nach Hunza-Karakoram,
Maßstab 1:100000; Quickbird-Daten, 11. Mai 2007; Generalny-Stab-Karte, Maßstab 1:100000, Blatt
J_43_126; Entwurf und Toponym-Aufnahme: Hermann Kreutzmann; Kartographie: Bernd Hilberer
56
Hermann Kreutzmann
a)
Altitude (m)
DIE ERDE
Stage/pasture
Yaks
(nonlactating)
Yaks
Sheep/goats
1 Ten herds
2 Three herds
b)
Stage/pasture
Altitude (m)
Donkeys
Sheep/goats
c)
Altitude (m)
Stage/pasture
Sheep/goats/oxen
Fig. 3 Three stage diagrams representing the mobility patterns of three village communities that occupy
pastures close to Batura and Pasu glaciers: a) Pasu on the northern side of Batura; b) Hussaini at
the lower southern side of Batura; c) Ghulkin at the upper elevations between Pasu and Batura
glaciers. The seasonal pattern of accesssing summer pastures in high-lying locations and winter
pastures close to the nuclei settlements is similar, though modified by entitlements and access
rights. Source: adapted from Kreutzmann (2006b: 349) / Drei Staffeldiagramme aus drei
Dörfern, die die Weiden im Batura- und Pasu-Gletschergebiet nutzen: a) Pasu am Nordufer
des Batura; b) Hussaini mit den tiefer gelegenen Weiden am Südufer des Batura; c) Ghulkin mit
den hoch gelegenen Weiden zwischen Batura- und Pasu-Gletscher. Das Mobilitätsmuster
zwischen höheren Sommerweiden und tieferen Winterweiden ist ähnlich und wird durch
Nutzungs- und Zugangsrechte modifiziert. Quelle: verändert nach Kreutzmann (2006b: 349)
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
57
Photo 2
Pasu is connected with its
filial settlement of Kharamabad by a lofty 140-m-long
suspension bridge. Mainly
women perform the daily
duty of caring for the animal
herds and irrigating the fields
when in season. Photograph:
Hermann Kreutzmann,
June 30 th, 1985 / Pasu und
die Sommerweidesiedlung
Kharamabad sind durch
eine 140 m lange Hängebrücke miteinander verbunden. Vorwiegend Frauen
erledigen die saisonalen
Arbeiten dort, wie Versorgung des Viehs und Feldbewässerung. Aufnahme:
Hermann Kreutzmann,
30. Juni 1985
people use the area for fodder cultivation and orchards and spend working time there whenever it
is required. Utilisation of the meagre resources involves a high degree of mobility. The agricultural
base seems to be quite archaic and stagnant. While
the utilisation system might not have changed substantially, other challenges have significantly transformed the societal setup.
4. Episodical Mobility as a Response
to Natural Hazards
Pasu’s settlement history shows quite clearly
that it is a village that was founded by migrants.
At the same time Pasu is a nuclear settlement
from which migrants moved to younger villages
in the upper Hunza and Chupursan valleys. The
58
Hermann Kreutzmann
resettlement of Pasuik – the local Wakhi term
for inhabitants of Pasu – households in Khaiber
and Hussaini is attributed to the time of Shah
Silum Khan III (1790-1824), who conquered
Gojal. He was instrumental in incorporating
Gojal villages into the Hunza principality and in
promoting Wakhi immigration. This early phase
of internal colonisation of neighbouring villages
can be attributed to the need for cultivable land.
Two major reasons are given for this. First, the
demographic growth of the village and the admission of new settlers who arrived as refugees made
it necessary to expand the food basis. Hussaini
and Pasu commanded all pastures along the northern and southern sides of the Batura glacier, while
Khaiber was a mixed settlement of Wakhi and
Burusho from which the valleys of Shaujerav
nearby and Gorhel (a side valley of Chupursan)
were accessed for summer pastures. For the
ethno-linguistic composition of Gojal villages cf.
Kreutzmann (1996: 281); the individual village
pastures and settlements are listed in Figure 1.
The second explanation for the expansion of settlements involves the loss of cultivated lands in
Pasu itself due to natural hazards. Pasu is located
between the two major glaciers of Batura and
Pasu (for geomorphological and glaciological
evidence cf. Goudie et al. 1984a; Goudie et al.
1984b; Hewitt 2001; 2005, 2010; Hewitt and Liu
2010; Iturrizaga 2005; 2007: 60ff., 176ff.).
Nevertheless, the village frequently suffered
from meagre water supplies for irrigation due to
glacial dynamics that, by advancing, destroyed
the headworks of the irrigation channels and, by
retreating or shrinking, dried up the local water
supply. In addition, the cultivated land has shrunk
owing to lateral undercutting of the river bank.
The collective memory of Pasu village strongly
focuses on regular and episodical events which
significantly reduced the village lands and space
for built environment. Qudratullah Beg (1962:
350) is the only local source referring to a
‘blockage of the Hunza River (possibly
1841 A.D.)’ at a place called Buddung (Badang)
DIE ERDE
which is just opposite Gamesar and close to the
site of the latest event. According to the recorded
tradition a “... lake was formed in the river course
which extended upstream up to the bottom of
settlement of Khyber in Gojal valley.” There is
still a place north of Batura glacier, halfway between Pasu and Khaiber called ‘sare musk’ which
refers in Burushaski to a flooded forest. A religious scholar was asked to prepare an amulet
(taawíz) “... to cause the natural dam on Hunza
River recede and save them all from its destructive effects. It was feared that the rising water
could completely inundate the villages of Fasso
[Pasu] and Gulmit and there was a real danger of
these villages getting submerged into this ever
rising lake” (Qudratullah Beg 1962: 350). The
taawíz worked and “By the grace of almighty Allah the river water started to overflow over the
dam and started to rapidly erode and cut/wash
away the natural dam. Soon the dam was busted
and washed away and a huge flood was caused.
This flood was so large that it completely washed
away the lower portion of village Ganish ... It is
narrated that the waters of this flood had completely washed away the entire village of Fasso
and it had eroded the whole lands of this village.
Prior to this flood, the village of Fasso was said
to be a wide and large settlement. It was after
this devastating flood that the remaining portions
of Fasso village continued to be eroded and
washed away by Shimshal floods every year.
Hence the area of this whole village kept on reducing and decreasing with every succeeding
year and then a time came when a very small portion of this village was left over. During the era
of rule of Mir Muhammad Nazim Khan (18921938), the barren land located above the original Fasso village was resettled and made inhabitable with the new name of Fasso”
(Qudratullah Beg 1962: 350f.). The story summarises the kind of risk, threat and loss that has
been attributed to the village of Pasu in local
historiography. The story related here is connected to a place near Sarat that was investigated by Karlheinz Paffen in 1954 (Paffen et
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
59
Photo 3
The site of the Atabad landslide (January 4th, 2010) seven months later. A nearly
two kilometres wide dam is
blocking the Hunza valley,
allowing only a narrow spillover channel to release water. Rockfall and landslides
have not stopped yet. Photograph: Hermann Kreutzmann July 31st, 2010 / Der
Ort des Atabad-Erdrutsches,
der das Hunza-Tal mit einem
fast zwei Kilometer weiten
Damm versperrt. Nur ein
kleiner Überlauf-Kanal führt
Wasser des Sees in den
Hunza-Unterlauf. Steinschlag und Rutschungen
gehen weiter. Aufnahme:
Hermann
Kreutzmann,
31. Juli 2010
al. 1956: 14) who attributed the event to the
1850s. Frederic Drew reports that in 1858 the
Sarat rockfall created a lake that reached and
flooded the upper Hunza Valley all the way to
Pasu (Drew 1875: 419). According to Qudratullah Beg and oral tradition in Gojal the lake
reached further up the valley and inundated
lands significantly above Pasu and the Batura
Glacier. The degree of damage in Pasu is not
exactly known, but the village must have been
abandoned for some time (Derbyshire et al.
2001; Kreutzmann 1994).
The advancing Batura glacier itself affected the
habitations of Pasu in 1873 (Hewitt and Liu
2010: 534; Mason 1929: 20f.); in 1905 culti-
60
Hermann Kreutzmann
74°5345E
74°540E
74°5345E
74°540E
36°2745N
36°2745N
36°280N
36°280N
36°2815N
36°2815N
74°5330E
DIE ERDE
74°5330E
0
100
200
300 m
Fig. 4 Pasu in 1937. The earliest and only aerial photograph known to date was taken when a colonial flight
mission was exploring potential airfields in the Karakoram. The picture is evidence for the extensive
village lands and row of houses within orchards of Pasu prior to the floods and damage of the 1960s.
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
vated land in Pasu was lost owing to glacial advances in the Shimshal valley in general and by
the Malungutti and Khurdopin glaciers in particular (IOR/2/1084/289: 153; IOL/P&S/7/
180/1426; Todd 1930: 174). In the following
year agricultural land, bridges and houses were
destroyed in Pasu, Hussaini and other villages
downstream (Singh 1917: 7; IOL/P&S/7/193/
1654). Three entries in the colonial records at
Gilgit document what had happened: “The bursting of the glacier dam in the Shingshal [Shimshal]
valley caused a very high flood in Hunza river on
the night of 11th August. … The flood was no
doubt the most serious that has occurred since
the Agency has been established … the water in
the Hunza river rose 50 feet above summer level
and 25 feet above last year’s flood. At Bunji the
Indus rose 30 feet, and the water was only
16 feet below the road way of the big suspension bridge known as the ‘Partab-pul’ (across
the Indus 7 miles above Bunji). … The road between Nomal and Chalt has been literally wiped
out …” (IOL/P&S/7/192/1618: Gilgit Diary
15/08/1906). “… flood of 11th August caused the
following damage: seven cultivated fields and one
house were washed away at Pásu, five cultivated
fields were washed away at Suseni [Hussaini]. Two
fields and rope bridge were washed away at
Gilmit [Gulmit], six cultivated fields and some
fruit trees were washed away at Ganish” (IOL/
P&S/7/193/1654: Gilgit Diary 22/08/1906).
“… recent Shingshal floods has carried away
35 fields with standing crops, 3 houses, 3 watermills and 1 orchard. A considerable quantity of
61
wheat, grain, which was lying on the threshingfloors, and fodder has also been swept away” (IOL/
P&S/7/193/1654: Gilgit Diary 29/08/1906).
Pasu has always been one of the villages hit
hardest by these glacier dam bursts. The events
described more than one hundred years ago resemble a key scenario discussed in the framework of today’s climate change debate. Although
the two glaciers bordering the village seem to
be a visible threat to the settlement, the origin
of risk and danger is located far away. Events
occurring up-stream in a side valley were the
main causes of the destruction in Pasu. Consequently, an understanding of Pasu’s position in
the riskscape of the Karakoram has to account
for events in a wider arena (Photo 3).
In 1910 damage occurred to three houses, twenty
agricultural terraced fields and many fruit trees in
Pasu, as was documented in the colonial records
(IOL/P&S/7/241/1118). In 1944 again, terraced
fields in Pasu were affected by glacial advances and
surges in the Shimshal valley (Saunders 1983:
107). Fortunately we discovered an aerial photograph (Fig. 4) depicting Pasu in 1937. Even then
the scars from undercutting of the river terrace are
perceivable, and the changing course of the Hunza
River can be imagined. Nevertheless, Pasu appears
to be a compact nuclear settlement with a distinct
border between the irrigated village lands and the
arid environment above the highest irrigation channel. The borderline on the edge of the terrace is
similarly distinct. In between, the habitations are
Pasu represents a compact oasis bordered by the prominent terrace marking the edge of the Hunza river
canyon in the East, Pasu glacier’s outflow stream in the South, and the arid and steep slope in the North and
West. Source: aerial photograph, taken September 20th, 1937 / Pasu 1937. Das früheste und bislang
einzige zeitgenössische Luftbild wurde während einer kolonialen Flugmission zur Erkundung potentieller Luftlandeplätze im Karakorum aufgenommen. Das Bild belegt die Existenz einer ausgepägten
Flur und eines Siedlungsbandes gesäumt von Baumbeständen vor den Flutereignissen der 1960er
Jahre. Pasu erscheint als kompakte Bewässerungsoase, die im Osten durch die Terrassenkante des
Hunza-Canyon, im Süden durch den Ausfluss des Pasu-Gletschers sowie im Norden und Westen durch
die steilen, trockenen Hänge begrenzt wird. Quelle: Luftbild, aufgenommen am 20. September 1937
62
Hermann Kreutzmann
74°5345E
74°540E
74°5345E
74°540E
36°2745N
36°2745N
36°280N
36°280N
36°2815N
36°2815N
74°5330E
DIE ERDE
74°5330E
0
100
200
300 m
Fig. 5 Pasu in 1966. Nearly 30 years later a spy satellite image provides evidence of the change in the
eastern section where substantial lands were lost in the aftermath of the early 1960s floods that
undercut the river terrace. The bed of the Hunza river widened and the village lands shrunk. Source:
Corona satellite image (September 22nd, 1966) / Pasu 1966: Fast 30 Jahre später belegt die
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
mainly located within the orchards – one hamlet
of the Sakhi lineage is locally called ‘boghik’ (the
people of the orchards) – while sizeable terraces
for crop cultivation are visible closer to the river
bed. This state of affairs changed significantly in
the years following the events described above.
In 1960 a bridge in Pasu was damaged (Clark
1960: 22), and this event was the beginning of a
series of severe losses of land and property in
Pasu during the following four years. In the collective memory of Pasu, the early 1960s are the
“danger years” in which the village lost a substantial share of its lands. Records of early
events are scanty, and we have listed only those
events which explicitly refer to Pasu. The living
memory of village elders is strong. Especially
the events between 1960 and 1962 have shown
dramatically that people could observe on a dayby-day basis how their fields, orchards and
grasslands disappeared. Hassan Khan’s garden
(bagh) was the first to vanish, and then the process of destruction continued. In the 1960s the
name of Virjerab glacier in the Shimshal valley
became synonymous with destruction and loss.
Terraced fields, orchards and houses were lost.
The Mir of Hunza offered some sort of compensation and made initial attempts to cultivate
Janabad Dasht, but efforts to bring water from
Batura Glacier to irrigate the uncultivated steppe
repeatedly failed. Some inhabitants were compensated with land in Nobod (new village) where
18 households found a refuge. This hamlet is
located above the old nucleus (yadiyor) close
to the Karakoram Highway. This information
was gathered in interviews with Ghulam-uddin
in Karachi, who provided a recollection and
63
history of the 1960s events and a depiction of
land losses, as well as from conversations with
Pasu village elders and Sanjar Beg in Pasu in
2008. For this period we were also able to consult an early spy satellite image: The Corona satellite image of 1966 (Fig. 5) gives a blurred impression of the land losses inflicted on Pasu in
the course of a few years; most people ascribe
these losses to the years 1960-1962, when the
village lands were substantially reduced.
To cope with the crisis, the settlement patterns of
Pasu were modified and various outward-leading
strategies were applied. The force of the natural
events had been so strong that all efforts to control
the undercutting of river banks by establishing protective bunds and other forms of stabilisation failed.
The process of land loss could not be stopped. The
most recent image in our multi-temporal comparison – a Quickbird image of 2007 (Fig. 6) – shows
that the process of undercutting continued after
the 1960s, with the river meandering and significantly widening the bed of the Hunza River. A
comparison (Fig. 7) showing land losses of Pasu
from 1937 to 2007 over the course of more than
two generations highlights the shrinking village
lands and the narrow corridor that is left for the
course of the Karakoram Highway as the major
artery of communication and trade.
In consequence, for some households the experience of the 1960s motivated them to develop an
alternative strategy: to leave Pasu and establish
new settlements in safer locations. During our initial enquiries in the 1990s we found that about
16 households in Khaiber (out of 30 Wakhi households) were originally Pasu migrants. In Hussaini
Aufnahme eines Spionagesatelliten den zwischenzeitlich erfolgten Verlust im östliche Abschnitt.
Beträchtliche Flurstücke fielen den Uferunterschneidungen infolge der Fluten der frühen 1960er
Jahre zum Opfer. Das Bett des Hunza-Flusses wurde geweitet, die Flur beschnitten. Quelle: CoronaSatellitenbild, aufgenommen am 22. September 1966
64
Hermann Kreutzmann
74°5345E
74°540E
74°5345E
74°540E
36°2745N
36°2745N
36°280N
36°280N
36°2815N
36°2815N
74°5330E
DIE ERDE
74°5330E
0
100
200
300 m
Fig. 6 Pasu in 2007. The Quickbird scene provides the greatest detail and underpins that land loss is
continuing to date. The river bed has widened further and the village lands have continued to shrink.
In the southern section the Pasu glacier’s outflow stream bed has been planted with seabuckthorn
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
there were only three such households. A new
opportunity arose when Mir M. Nazim Khan and
his Wazir Shukrullah Beg started the resettlement of the Chupursan valley after a major
mudflow had destroyed the settlements there in
around 1830. Damage to all settlements in
Chupursan was inflicted in 1830 by a mudflow
following a glacier advance; cf. Schomberg
(1935: 225, 1936). The resettlement in
Chupursan was initiated in 1918, but gained pace
after 1921 when Pasu settlers migrated to
Shersabz (5 households), Reshit (2), Ispenj (10)
and Zodkhon (8). The 25 households of Pasu origin made up two thirds of the 38 households recorded in the respective villages during the census of 1931 (Pal 1934). The period of relocation was initiated by the Hunza ruler as a form
of internal colonisation by cultivating barren
lands and transforming them into irrigated oases (Kreutzmann 1996). The settlers in the
newly-founded oases were initially supported by
their relatives in Pasu who inherited the remaining resources there. Later on bonds remained
strong between Pasu and the new settlements
only through marriage relations. The former
summer camps of pastoralists were converted
into permanent settlements in which the households received substantial land property. The
new settlers had easy access to nearby pastures
in the Chupursan side valleys.
5. Searching for New Opportunities
During these periods Gojal farmers were largely
restricted to crop cultivation and animal hus-
65
bandry. The Hunza rulers managed to make the
Gojali contribute four fifths of the taxes although their share in the population was only one
fifth. This statement holds true for the beginning
of colonial rule in Hunza in 1891. By the mid1930s taxation and forced labour pressure on the
Wakhi farmers had substantially increased. Mir
M. Nazim Khan exercised a strong regime with
British backing there. Wakhi farmers not only
fled from natural hazards and internal colonisation, but also began to search for new opportunities to escape the strict control of the local ruler.
Already in 1921, two Wakhi had escaped across
the northern passes towards Shughnan in presentday Tajikistan where they joined the Bolshevik
army (India Office Library & Records: IOL/P&S/
10/973: 238). Wakhi farmers and their sons
were excluded from early job opportunities offered by the colonial administration which conscripted soldiers for the Gilgit Scouts. All posts
allocated to Hunza were occupied by non-Wakhi
applicants who were selected by the ruler (India
Office Library & Records: IOL/P&S/12/3288:
Administration Report for 1935). Consequently
Wakhi, and among them the people of Pasu, failed
to participate in the early phase of entrepreneurship which was based on military service and subsequently operating small enterprises in trade.
Even today we find only five retired soldiers and
three active military men among 467 male citizens in Pasu (data taken from the 2006 census by
the Ismaili Council for Gulmit, provided by letter). Consequently, a general disharmony and exclusion was felt that articulated itself in a vigorous political debate. Today, supporters of the
local ruler (Mir party) and their opponents (in the
(Hippophae rhamnoides) shrubs that provide fodder and fuel. Source: Quickbird data, May 11th, 2007, multispectral, pan-sharpened / Pasu 2007. Die Quickbird-Aufnahme erlaubt detailliertere Einblicke und
belegt, dass die Landverluste durch Uferunterschneidung anhalten. Das Flussbett weitet sich und die
Flur schrumpft weiter. Im südlich angeschnittenen Ausflussbereich des Pasu-Gletschers wurde
Sanddorn (Hippophae rhamnoides) für Futter- und Feuerungszwecke kultiviert. Quelle: Multispektrale Quickbird-Daten vom 11. Mai 2007
66
Hermann Kreutzmann
74°5345E
74°540E
74°5345E
74°540E
36°2745N
36°2745N
36°280N
36°280N
36°2815N
36°2815N
74°5330E
DIE ERDE
74°5330E
0
100
200
300 m
Fig. 7 Loss of land in Pasu over time: 1937, 1966, 2007. Taking the rectified spatial information from all
three images, the process of loss of land becomes evident. Source: overlay from Figures 4-6
Kulturlandverluste in Pasu im zeitlichen Vergleich: 1937, 1966, 2007. In der Überlagerung der
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
case of present-day Pasu: followers of the Pakistan People’s Party) are still striving to assert
their contrasting positions. The judgement of
the opposition was that escape from the valley
would basically broaden the opportunities and
the income basis of all households. Pasu has
been a case in point to support this thesis.
6. Out-Migration for Jobs and Education
as a Strategy to Diversify the Income
Structure of Mountain Households
It took until long after Pakistan’s independence
for the Wakhi of Pasu to participate in physical infrastructure. By 1964 the first jeep had
reached Pasu. Although not directly connected
to this event, at about the same time people
from Pasu out-migrated to the south of Pakistan, to the port of Karachi. From the beginning
this out-migration was a twofold affair. Early
migrants were in search of wage labour in unskilled employment. While classical outmigration from the mountain regions of Pakistan
was for seasonal employment in road construction, service industries and menial tasks – the
major construction projects of Mangla (1967) and
Tarbela dams (1975) offered jobs for many –,
Pasu people left their village for permanent employment, not just seasonal work. And Karachi
remained their prime destination. Seeking education was another new opportunity that snowballed. After the first escapee managed to study
and get a technical degree he volunteered to
support others and so on. To cut a long story
short: The educational pioneers profited from
the introduction of basic education provided by
government schools and private institutions supported by the Aga Khan Education Service.
Wakhi children participated from an early stage
in male and female education. In addition they
67
found a supportive environment in Karachi where
Ismaili entrepreneurs, followers of the Aga
Khan, offered scholarships, material support and
jobs in their enterprises to young students from
their denominational community. Pasu is one of
the Karakoram villages with the highest record
of qualified people today. Out of 872 inhabitants
361 are ‘out of station’, of whom 17 are in government service, 90 in private service, and 16 in
business (data taken from the 2006 census by the
Ismaili Council for Gulmit). The majority of
persons outside the village receive different
forms of education in the Northern Areas (nowadays Gilgit-Baltistan), and in Islamabad, Lahore,
Peshawar and – still ranking first – Karachi.
Within the span of two generations, educationbased jobs have become the prime resource for
employment in a village where 79 % of the male
and 75 % of the female population are termed educated. The prime position of Pasu is highlighted
when compared with the neighbouring village of
Hussaini where significantly lower percentages of
professionals are to be found. The same statement
holds true for the rest of Hunza. In a survey conducted in 1990, in 70 Pasu households there were
seven engineers, two medical doctors, two chartered accountants, five social scientists and thirty
bachelor degree holders. In addition there were
three male and four female teachers from the village (Kreutzmann 1996: 313). The preference
of Pasu inhabitants for non-agrarian positions and
professions has made it complicated to find sufficient personnel to work on the fields and to care
for the animal herds in the summer pastures.
While the latter is mainly under female control,
additional non-local labour has been hired in recent years for sowing and harvesting as well as
for other domestic tasks in the homesteads.
So far we have discussed only migration within
Pakistan. It is important to note that in this remote
rektifizierten räumlichen Informationen wird der anhaltende Landvelust belegt. Quelle: Überlagerung der Informationen aus den Abbildungen 4-6
68
Hermann Kreutzmann
DIE ERDE
Foreign visitors
3000
2500
2000
1500
1000
500
2001
2002
2003
2004
2005
2006
2007
2008
2009
Fig. 8 Foreign visitors to Baltit Fort 2001-2009. The data on a monthly basis significantly show the
seasonality of visitors’ arrivals and how the events of 9/11 affected tourism in the Hunza valley. Since
then tourism never recovered and failed to reach former levels. Source: Annual reports, Baltit Fort
Office, Karimabad, Hunza / Ausländische Besucher in Baltit Fort 2001-2009. Die Darstellung
der Monatsdaten unterstreicht die Saisonalität des Fremdenverkehrs und den nachhaltigen
Einbruch des Besucheraufkommens infolge der Ereignisse des 11. Septembers 2001. Seither
hat sich der Fremdenverkehr nicht mehr erholt bzw. nicht mehr die früheren Besucherzahlen
erreicht. Quelle: Jahresberichte des Baltit Fort Office, Karimabad, Hunza
mountain village international migration is as common as in down-country Pakistan. During the late
1970s and early 1980s, when Pakistan derived a
substantial share of foreign currency earnings
through overseas Pakistanis in the Gulf States,
five Pasuik were among those migrants who went
to Saudi Arabia. In recent years their share has decreased. During our survey in 2003 four Pasuik
were still working in Saudi Arabia, Kuwait and the
United Arab Emirates. In addition three men managed to enter the United States of America, of
whom two acquired legal residence status there,
while one returned after five years to retire in Pasu.
Three young men from Pasu spent educational
stints in Canada, one migrated to the UK, one
married a Japanese wife and one an Australian.
Both couples have been active in tourism for the
last decade. Thus, international migration is significant for one tenth of the households in Pasu.
These migrants send substantial remittances to
Pasu, a fact which is reflected in housing construction and other amenities.
7. Tourism Development as a Means of
Re-Interpreting Local Resources
While all previously mentioned migrationrelated strategies for diversification of income
resources have increased the exodus from Pasu
village, there is one process that provides nonagrarian employment in the village. After the
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
opening of the Karakoram Highway for international travellers to Pasu in 1982, tourism activities were added to the income structure. For an
assessment of the trading and tourism potential
connected with the Karakoram Highway and its
constraints cf. Kreutzmann (2009). Much earlier, porters and mountain guides from Pasu had
been engaged to accompany mountaineering
expeditions in Baltistan and to Nanga Parbat.
Therefore the opening of the road meant that
local expertise could be utilised locally. In the
beginning three small guesthouses were established, which have meanwhile increased to eight.
More importantly, the services of guides were
offered for trekking and mountaineering tours
in the Batura and Shimshal valleys. Before 9/11
a substantial income could be derived from tourism as some men found employment in travel
agencies or founded their own travel businesses.
Tourism being a difficult resource in politically
unpredictable times, reliance on these undertakings has diminished in recent years (Fig. 8). Nevertheless, the skills revive as soon as new opportunities arise. A number of people have been engaged in assisting the Chinese engineers who
started a project to widen the Karakoram Highway in 2008. Hotels have been transformed into
rented-out accommodation, etc. Tourism completely collapsed in the aftermath of the events
mentioned at the outset. Atabad Lake and the
floods that damaged the Karakoram Highway as
the major line of communication have terminated
classical tourism for the time being. Nevertheless, tourism entrepreneurs provide local services
to relief organisations and development projects.
8. Conclusions
Mobility as an adaptive strategy has played a
major role in Pasu in helping the inhabitants to
cope with the crises inflicted on them by environmental threats. During the 19th and early 20th
century the securing of agricultural resources
was of prime interest. Consequently, during this
69
period out-migration aimed at establishing new
settlements with a sound agricultural base and
access to summer pastures. The settlements in
the upper Hunza Valley and Chupursan are ample
evidence of this strategy. The flood disasters of
the early 1960s changed attitudes quite significantly. The severity of the losses and the concomitant opportunities provided by improved infrastructure and educational options motivated
other strategies. Pasu developed into one of the
‘model villages’ of Hunza in terms of professional careers and female education (Felmy
2006). The investments in non-agrarian income
opportunities were significant and greatly improved the well-being of its residents and their
migrant relatives at other stations. In comparison
with neighbouring villages of the same size and
similar assets, Pasu has taken a leading role in
diversifying its income structure and placing its
people in a number of locations. Beyond the challenges posed by environmental threats, social
cohesion within the Wakhi community of Pasu
plays a major role in mutual support systems, in
accepting female leadership and human capacity
building. During the 19th century, Gojal was the
grain chamber of Hunza and supplied the villages
of Central Hunza with valuable resources. Nowadays Gojal is the brain chamber of Hunza with the
highest number of professionals and highly educated people. Nevertheless, Pasu as a residential
hub of the Pasuik remains in high esteem; migrants
invest in new houses and improved facilities. The
newly established filial settlement of Janabad
functions as a land resource for further expansion
of the settlement. Multi-locality and seasonal absence of household members is the price that has
to be paid for a coping strategy based on the mobility of individual women and men. In times of
severe political crisis the village itself is the last
refuge for everybody to return to when enterprises
in tourism or trade collapse, the KKH is blocked
and communication is interrupted.
Despite numerous floods and high risk exposure
that have regularly occurred in the course of cen-
70
Hermann Kreutzmann
turies, the people of Pasu have shown significant
stamina and resilience to cope with substantial
challenges. Their adaptation and experience
could well be a major asset in coping with
climate change challenges.
Acknowledgements
Several persons supported the research in and on
Pasu. First of all, my gratitude goes to my local
supporter, consultant and friend for more than three
decades, late Ghulam-ud-din to whom this paper is
dedicated. Sanjar Beg in Janabad provided valuable
evidence about the 1960s floods from his own experience. I am indebted to Ahmed Jami Sakhi and Ali
Qurban in Gilgit for compiling valuable information
about the oral traditions concerning Pasu memory
and history. Office-bearers from the Ismaili Council
for Lower Gojal in Gulmit took an interest in recording the employment and migration histories of Pasuik.
I am especially indebted to Sharif Uddin and
Sherullah as well as to Fazal Amin Beg. Technical
support in rectifying multi-temporal aerial photographs and satellite images was kindly extended by
Marcus Nüsser in Heidelberg.
9. References
Bohle, H.-G. 2007: Living with Vulnerability. Livelihoods and Human Security in Risky Environments. –
InterSecTions. Interdisciplinary Security ConnecTions. Publication Series of UNU-EHS 6. – Bonn. –
Online available at: http://www.ehs.unu.edu/file/get/
3858, 19/04/2012
Brush, S.B. 1976a: Introduction, Symposium on Cultural Adaptation of Mountain Ecosystems. – Human
Ecology 4: 125-134
Brush, S.B. 1976b: Man’s Use of an Andean Ecosystem. – Human Ecology 4 (2): 147-166
Brush, S.B. 1977: Mountain, Field, and Family. The
Economy and Human Ecology of an Andean Valley. –
Philadelphia
Clark, L.P. 1960: Progress in the Gilgit Agency. –
Eastern World 14 (5): 21-22
DIE ERDE
Derbyshire, E., M. Fort and L. Owen 2001: Geomorphological Hazards along the Karakoram Highway: Khunjerab Pass to the Gilgit River, Northernmost Pakistan. – Erdkunde 55 (1): 49-71
Drew, F. 1875: The Jummoo and Kashmir Territories. –
London. – Reprint: Graz 1976, Karachi 1980
Ehlers, E. and H. Kreutzmann (eds.) 2000: High
Mountain Pastoralism in Northern Pakistan. – Erdkundliches Wissen 132. – Stuttgart
Eriksson, M., J. Xu, A.B. Shrestha, R.A. Vaidya,
S. Nepal and K. Sandström 2009: The Changing
Himalayas. Impact of Climate Change on Water
Resources and Livelihoods in the Greater Himalayas. – Kathmandu
Felmy, S. 2006: Transfer of Education to the Mountains. – In: Kreutzmann, H. (ed.): Karakoram in
Transition. Culture, Development, and Ecology in the
Hunza Valley. – Karachi et al.: 370-381
Goudie, A.S., D. Brunsden, D.N. Collins, E. Derbyshire, R.I. Ferguson, Z. Hashmet, D.K.C. Jones, F.A.
Perrott, M. Said, R.S. Waters and W.B. Whalley 1984a:
The Geomorphology of the Hunza Valley, Karakoram
Mountains, Pakistan. – In: Miller, K.J. (ed.): The International Karakoram Project, Vol. 2. – Cambridge: 359-410
Goudie, A.S., D.K.C. Jones and D. Brunsden
1984b: Recent Fluctuations in Some Glaciers of the
Western Karakoram Mountains, Hunza, Pakistan. –
In: Miller, K.J. (ed.): The International Karakoram
Project, Vol. 2. – Cambridge: 411-445
Government of Pakistan 1975: District Census of
Pakistan. Gilgit District 1972. – Islamabad
Government of Pakistan 1984: 1981 District Census
Report of Gilgit (Population Census Organization,
Statistics Division). – Islamabad
Grötzbach, E. 1980: Die Nutzung der Hochweidestufe als Kriterium einer kulturgeographischen Typisierung von Hochgebirgen. – In: Jentsch, C. und
H. Liedtke (Hrsg.): Höhengrenzen in Hochgebirgen. –
Arbeiten aus dem Geographischen Institut der Universität des Saarlandes 29. – Saarbrücken: 265-277
Grötzbach, E. 1984: Mobility of Labour in High Mountains
and the Socio-Economic Integration of Peripheral Areas. –
Mountain Research and Development 4 (3): 229-235
Guillet, D. 1983: Toward a Cultural Ecology of
Mountains. The Central Andes and the Himalaya
Compared. – Current Anthropology 24 (5): 561-574
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
Hewitt, K. 2001: Catastrophic Rockslides and the
Geomorphology of the Hunza and Gilgit River Valleys,
Karakoram Himalaya. – Erdkunde 55 (1): 72-93
Hewitt, K. 2005: The Karakoram Anomaly? Glacier
Expansion and the ‘Elevation Effect’, Karakoram
Himalaya. – Mountain Research and Development
25 (4): 332-340
Hewitt, K. 2006: Glaciers of the Hunza Basin and
Related Features. – In: Kreutzmann. H. (ed.): Karakoram in Transition. Culture, Development, and
Ecology in the Hunza Valley. – Karachi et al.: 49-72
Hewitt, K. 2010: Gifts and Perils of Landslides.
Catastrophic Rockslides and Related Landscape
Developments are an Integral Part of Human Settlement along upper Indus Streams. – American
Scientist 98 (5): 410-419. – Online available at: http://
www.americanscientist.org/issues/issue.aspx?
id=10386&y =2010&no=5&content=true&page
=5&css=print, 19/04/2012
Hewitt, K. and J. Liu 2010: Ice-Dammed Lakes and
Outburst Floods, Karakoram Himalaya: Historical
Perspectives on Emerging Threats. – Physical Geography 31 (6): 528-551
India Office Library & Records: Departmental Files
relating to Indian States Extracted from the Political
and Secret Letters from India 1881-1911, IOL/P&S/7/
180, 192, 193, 241
India Office Library & Records: Departmental Papers: Political and Secret Separate (or Subject) Files
1902-1931, IOL/P&S/10/973
India Office Library & Records: Departmental
Papers: Political & Secret Internal Files & Collections 1931-1947, IOL/P&S/12/3288 Administration
Report for 1935
71
des lateroglazialen Sedimentformenschatzes. –
Geography International 2. – Aachen
Kohler, T. and D. Maselli (eds.) 2009: Mountains
and Climate Change: From Understanding to Action. –
Berne
Kreutzmann, H. 1994: Habitat Conditions and Settlement Processes in the Hindukush-Karakoram. – Petermanns Geographische Mitteilungen 138 (6): 337-356
Kreutzmann, H. 1996: Siedlungsprozesse und territoriale Aneignung im zentralen Hunza-Tal. Kulturgeographische Anmerkungen zur Publikation der Karte HunzaKarakorum 1 : 100 000. – Erdkunde 50 (3): 173-189
Kreutzmann, H. 2004: Pastoral Practices and their
Transformation in the North-Western Karakoram. –
Nomadic Peoples 8 (2): 54-88
Kreutzmann, H. 2006a: Settlement History of the
Hunza Valley and Linguistic Variegations in Space
and Time. – In: Kreutzmann, H. (ed.): Karakoram in
Transition. Culture, Development, and Ecology in the
Hunza Valley. – Karachi et al.: 251-272
Kreutzmann, H. 2006b: High Mountain Agriculture
and its Transformation in a Changing Socio-Economic
Environment. – In: Kreutzmann, H. (ed.): Karakoram in Transition. Culture, Development, and Ecology in the Hunza Valley. – Karachi et al.: 329-358
Kreutzmann, H. 2009: The Karakoram Highway as
a Prime Exchange Corridor between Pakistan and
China. – In: Kreutzmann, H., G. Amin Beg,
L. Zhaohui and J. Richter (eds.): Proceedings of the
Regional Workshop ‘Integrated Tourism Concepts to
Contribute to Sustainable Development in Mountain
Regions’. – Bonn: 13-36
Kreutzmann, H. 2010: An Inevitable Disaster. –
Himal Southasian 23 (6): 24-25
India Office Library & Records: Crown Representative’s Records. Indian States Residencies. Gilgit,
Chilas, Hunza and Nagir Files (Confidential), IOR/
2/1084/289
Kreutzmann, H. (ed.) 2012: Pastoral Practices in
High Asia. Agency of ‘Development’ Effected by
Modernisation, Resettlement and Transformation. –
Dordrecht
Ismaili Council for Gulmit 1994, 2012: Local Census
Data Provision by Letter from the Secretary. – Gulmit
Kreutzmann, H. and S. Schütte (eds.) 2011: After
the Flood in Pakistan. Assessing Vulnerability in
Rural Sindh. – Berlin Geographical Papers 38
Iturrizaga, L. 2005: New Observations on Present
and Prehistorical Glacier-Dammed Lakes in the
Shimshal Valley (Karakoram Mountains). – Journal
of Asian Earth Sciences 25 (4): 545-555
Iturrizaga, L. 2007: Die Eisrandtäler im Karakorum. Verbreitung, Genese und Morphodynamik
Leitner, G.W. 1891: Rough Accounts of Itineraries
Through the Hindukush and to Central Asia. – The
Imperial and Asiatic Quarterly Review N.S. II: 243-248
Lockhart, W.S.A. and R.G. Woodthorpe 1889: The
Gilgit Mission 1885-86. – London
72
Hermann Kreutzmann
Mason, K. 1929: Indus Floods and Shyok Glaciers. –
The Himalayan Journal 1: 10-29
Müller-Mahn, D. (ed.) 2012: The Spatial Dimension
of Risk. How Geography Shapes the Emergence of
Riskscapes. – London. – in print
Murra, J.V. 1985: ‘El Archipiélago Vertical’ Revisited. – In: Masuda, S., I. Shimada and
C. Morris (eds.): Andean Ecology and Civilization. An Interdisciplinary Perspective in Andean
Ecological Complementarity. – Papers from WennerGren Foundation for Anthropological Research
Symposium 91. – Tokyo: 3-13
Paffen, K., W. Pillewizer and H.-J. Schneider
1956: Forschungen im Hunza-Karakorum. Vorläufiger Bericht über die wissenschaftlichen Arbeiten
der Deutsch-Österreichischen Himalaya-KarakorumExpedition 1954. – Erdkunde 10 (1): 1-33
Pal, M.M. 1928: Letters of Pal to D.L.R. Lorimer
dated 5 January, 19 January, 14 February, 20 April,
8 July 1928. – In: Lorimer Personal Records located
at SOAS (MS 181247)
Pal, M.M. 1934: Letters of Pal to D.L.R. Lorimer
dated 24 July, 28 July 1934. – In: Lorimer Personal
Records located at SOAS (MS 181247)
Qudratullah Beg, H. 1962: History of Ancient Era
Hunza State. Part 1. – English edition 2006, translation by Saadullah Beg. – Baltit
Saunders, F. 1983: Karakoram Villages FAO. –
Gilgit
Schomberg, R.C.F. 1935: Between the Oxus and
the Indus. – London. – Reprint: Lahore 1976
Schomberg, R.C.F. 1936: Unknown Karakoram. –
London
Singh, T. 1917: Assessment Report of the Gilgit
Tahsil. – Lahore
Spratt, D. and D. Lawson 2009: High Stakes: Climate Change, the Himalayas, Asia and Australia. –
Collingwood. – Online available at: http://www.
tibetnetwork.org/sites/default/files/highstakes.pdf,
20/04/2012
Todd, H. 1930: Correspondence: Gilgit and Hunza
River Floods. – The Himalayan Journal 2: 173-175
Uhlig, H. 1995: Persistence and Change in High
Mountain Agricultural Systems. – Mountain Research and Development 15 (3): 199-212
DIE ERDE
UNEP 2009: Global Outlook for Ice and Snow. –
Nairobi. – Online available at: http://www.unep.org/
geo/geo_ice/PDF/full_report_LowRes.pdf, 20/04/2012
Wisner, B., P.M. Blaikie, T. Cannon and I. Davis
2004: At Risk. Natural Hazards, People’s Vulnerability and Disasters. – 2nd edition. – London et al.
Summary: After the Flood. Mobility as an Adaptation
Strategy in High Mountain Oases. The Case of Pasu
in Gojal, Hunza Valley, Karakoram
The high mountain environment of the Hunza Valley
in the Karakoram is characterised by significant
potential energy, extended glaciation and related
events that tend to threaten habitations and settlements. The village oasis of Pasu is taken as a case in
point to highlight adaptation and coping strategies
over a longer period of time. The village lands of
Pasu have been shrinking over time due to glacier
outburst floods in the upper valleys. The memory of
these devastating events that have threatened the
resource base for agricultural undertakings again
and again is omnipresent, part of the oral traditions
and local historiography. Evidence of disaster events
and local responses is provided from diverse sources. The inhabitants of Pasu have developed a set of
coping strategies and flexible responses that are
mainly linked to mobility. Among these are the shifting of population to newly established irrigated oases
on previously barren lands and out-migration to various destinations for employment and education.
Nowadays we find Wakhi from Pasu in urban areas
in the Karakoram and in metropolises in downcountry Pakistan. Remittances from international migration to overseas destinations had a significant
impact on broadening income-generation by reducing
the importance of agriculture in favour of services and
tourism. All strategies are measures of adaptation that
are embedded into the socio-political and economic
frame conditions. The shrinking village lands of Pasu
have posed tremendous challenges to the mountain
farmers who developed their own responses without
abandoning their inherited settlement.
2012/1-2
After the Flood. Mobility as an Adaptation Strategy in High Mountain Oases
Zusammenfassung: Nach der Flut. Mobilität als
Anpassungsstrategie in Hochgebirgsoasen. Die
Fallstudie Pasu in Gojal, Hunza-Tal, Karakorum
Die Hochgebirgsumwelt des Hunza-Tales im Karakorum ist durch hohe Reliefenergie, ausgedehnte
Vergletscherung und Schadensereignisse charakterisiert, die Wohngebäude und Siedlungen gefährden.
Die Bewässerungsoase von Pasu hat über längere
Zeiträume einen bedeutenden Anteil der Flur als
Folge von Gletscherseeausbrüchen in höher gelegenen Talabschnitten verloren. Die Erinnerungen an
die zerstörerischen Umweltereignisse sind allgegenwärtig, Teil der oralen Tradition und lokalen Geschichtsschreibung. Belege für derartige Ereignisse
und lokale Reaktionen darauf werden aus verschiedenen Quellen herangezogen. Die Einwohner von
Pasu haben auf diese Ereignisse mit einer Vielzahl
von Anpassungsstrategien reagiert, die in vielfältiger Weise mit Mobilität verknüpft sind. Bevölkerungsgruppen siedelten sich in neu angelegten Bewässerungsoasen an; Abwanderung erfolgte zur
Beschäftigungssuche und Ausbildung in urbane
Marktzentren des Karakorum, aber auch in die pulsierenden Metropolen des Tieflandes. Remissen aus
internationaler Migration nach Übersee hatten großen
Einfluss auf die Erweiterung der Einkommensquellen
wie auch die Verminderung des landwirtschaftlichen Beitrags zugunsten einer höheren Wertschöpfung aus Dienstleistungen und Fremdenverkehr. Die vorgestellten Maßnahmen belegen das
hohe Maß der Anpassung und des Umgangs mit
einschneidenden Ereignissen im Rahmen der
gegebenen sozio-politischen und wirtschaftlichen
Möglichkeiten. Die schrumpfende Flur von Pasu
hat die Gebirgsbauern vor gewaltige Herausforderungen gestellt, denen sie eigene Kompensationsstrategien ohne Aufgabe des ererbten Siedlungsplatzes entgegengesetzt haben.
Résumé: Après la marée: Mobilité comme stratégie
d’adaptation aux oases de haute montagne. Étude
modèle de Pasu en Gojal, Vallée de Hunza,
Karakoram
L’environnement de haute montagne de la Vallée de
Hunza en Karakoram est caractérisé par un relief
73
marquant, une vaste glaciation et des dégâts possibles qui s’ensuivent et mettent en danger les bâtiments d’habitation et les villages. L’oasis de Pasu est
à juste titre un exemple pour mettre en relief les
stratégies d’adaptation et pour faire face aux événements à long terme. Au cours du temps, les territoires
du village de Pasu ont reculé à cause des inondations
par les glaciers dans les vallées supérieures. Le
souvenir de ces événements dévastateurs qui ont
menacé la base de ressources pour les activités
agricole est omniprésent et fait partie de la tradition
orale et de l’historiographie locale. Preuves de l’occurrence de ces désastres et des réactions locales
sont fournies par une variété de sources. Les habitants de Pasu ont développé une multitude de stratégies pour faire face aux événements et des réactions
d’adaptation qui sont associées surtout à la mobilité.
Entre autres on compte le déplacement de la population aux nouvelles oases irriguées qui se trouvent sur
des territoires qui antérieurement ont été arides et la
migration en quête d’emploi et éducation vers les
centres urbains de Karakoram et aussi vers les autres
métropoles animées du pays. Les versements de la
migration internationale vers des destinations transatlantiques ont eu une conséquence significative pour
l’augmentation des sources de revenue par la diminution de l’importance de l’agriculture en faveur de la
prestation de services et du tourisme. Les mesures
mentionnées prouvent un haut degré d’adaptation et
la manière de traiter les événements décisifs en
contexte de l’ensemble des conditions sociopolitiques
et économiques. Le territoire en diminution des villages de Pasu a représenté une épreuve immense pour
les paysans montagnards, à laquelle ils ont répondu
avec leurs propres stratégies de compensation sans
quitter leur habitat hérité.
Prof. Dr. Hermann Kreutzmann, Institut für Geographische Wissenschaften, Freie Universität Berlin,
Malteserstr. 74-100, 12249 Berlin, Germany,
h.kreutzmann@fu-berlin.de
Manuscript submitted: 08/03/2011
Accepted for publication: 08/07/2011