Scraping saltpeter
off rocks was not exactly a reliable way to gather massive quantities of it. Extracting
it from manure spread over land was also a slow and smelly process. For every
pound of manure, a few crystals would grow.
In the mud
areas of the River Ganges in India, the local population had been using saltpeter
for a long time in their agricultural practices of fertilization with manure. The
first documented reference to saltpeter is found in the early 17th
century when the English East India Company considered importing it from India
in the early 1620s. The first recorded shipment to England was made in 1626. Saltpeter
became one of the most important items traded by the English company.
On the three
Chincha Islands located 21 km off the coast of Peru, on a group of rocks inhabited
exclusively by flocks of birds, boobies, cormorants, and penguins, over thousands
of years, bird droppings had formed a crust over a hundred feet deep, one of
the finest natural fertilizers called guano.
The Inca
called the bird droppings huanu, hence our term guano. Sprinkling
it onto their fields as fertilizer, Incas valued guano just like gold and
considered the killing of birds a capital crime.
Peru started
trading the guano in 1840, after using Chinese labor to harvest the highly flammable
fertilizer. By late 1850, the Chincha guano was exhausted when the workers struck
rocks. Economists calculated that by 1860, 4,000 Chinese workers had died
working in extremely noxious conditions. Peru’s source of riches was exhausted
in two decades.
Peru had
another unique salt called caliche found in the northern reaches they
controlled in the Atacama Desert. The word caliche is derived from
Quechua and it means salt.
Caliche appeared as a crust found by a
stroke of luck by locals traveling from the Andes foothills to the Pacific
Ocean. While making camp for the night and building fires, they noticed rocks
on the ground sparking and igniting.
The
explosive and fertile caliche is made up of sodium chloride (table
salt), nitrates, iodates, sulphates, and chlorides. The caliche is slightly
different from saltpeter in that it has sodium nitrate rather than potassium
nitrate.
Nobody is
quite sure how the caliche appeared in the northern parts of the Atacama
Desert. According to Ed Conway, there are theories:
1.
The
product of an eerie fog that often forms across the desert at night and morning.
2.
These
salts washed down from the Andes.
3.
Caliche
was deposited here by an ancient sea.
Even though
the deposits were mostly located in Peruvian and Bolivian territory, according
to Conway, it was “enterprising Chilean immigrants who discovered most of the caliche,
did most of the mining, and forged the all-important links with English and
German financiers who provided the capital for their businesses." [mid 1870s]
The greedy
decision by Bolivia to enact a retroactive tax of ten cents per quintal (100 lbs.)
of nitrates exported from the area, even though they signed a treaty in 1874,
pledging not to impose taxes on mineral exploitation, gave rise to a serious conflict.
The railway’s manager, George Hicks, refused to pay and sought refuge on a Chilean
warship stationed off the coast. Chilean troops occupied the area and the port
a few days later.
Following
the Ten Cents War which lasted five years (1879-1884), fought between Chile,
Peru, and Bolivia over the nitrate-rich Atacama Desert region, Chile won “control
over the most important mineral resources in the world - not just the nitrates
of the Atacama, but the world’s biggest reserves of copper and lithium.” Bolivia
lost its coastline and Chile became “a resource superpower.” (Ed Conway,
Material World, p. 170)

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