PHOSPHATE
MINING IN SPAIN
Phosphate
deposits were recorded in Spain as early since 1808 but exploitation only began
on a small scale in 1845. (Blakey,A.F. "The Florida Phosphate
Industry" Wertheim Committee, Harvard, 1973,p9,147) Exactly where was not
mentioned but possibly in ESTREMADURA.
In 1849 it was stated that, "the great bed of Estremadura
phosphorite, … is at present not of sufficiently ready access to prove of any
practical importance to British agriculture." ...”The phosphorite of Spain
has not been imported into this country to any considerable extent in
consequence of the great expense of getting it on board ship; at present
therefore it is not likely to be of any practical importance in the manufacture
of superphosphate of lime." Way, J.T. Journ.Ag.Soc.vol.xii.p215
In 1851 mineral phosphate of lime was found at
Cabo di Gata, and Villa Rica and apatite found at Leigrosan, in province of
Estremadura in Spain. (Way,J.T.1851 p.253-5; Captain Widdrington and Dr.
Daubeny, 'On the Occurrence of Phosphorite in Estremadura,'
Journ.Agric.Soc.1845; Geol.Mag.1845?; 'On the use of Spanish Phosphorite as a
Manure' Sir H.Verey, Journ.Ag.Soc.vol.vi.,1845?
SPANISH ESTREMADURA PHOSPHATE AND MOROXITE
FROM JUMELLA.- Spain
Specimens
sent to the 1851 International Exhibition in London of two phosphatic minerals
which are likely to become important articles of commerce at no distant date.
One of these minerals is already in the hands of commercial men, and is
employed and exhibited by several manufacturers of manures. We refer to the
phosphorite which occurs in immense quantities at Lagrossa, near Truxillo,
Estremadura. It is here associated with foliated apatite and quartz, and forms
solid beds that alternate between with limestone and quartz. This Spanish
phosphorite has a fibrous structure, a light yellow colour, and a considerable
degree of hardness. When reduced by means of powerful machinery to a fine
powder, and treated with oil of vitriol, it becomes, like other mineral
phosphates, converted into superphosphate of lime.
Exhibited by R. Manjarres, Seville. Voelcker,Dr.A. Ph.D. Consulting chemist to
the Royal Agricultural Society of England. 'Raw Materials used as Manures, and
Artificial Manures.' Rept. International Exhibition, 1862,pp149-53
Cuthbert Johnson reported the new Spanish
deposits in the Mark Lane Express. “Found at Logrosson a rock varying from 7
- 16 feet in breadth, traceable for nearly two miles and extending into the
earth to a great, though as yet unascertained, depth." (Johnson, C.
"Mineral Phopshate of Lime," Mark Lane Express,4th Sept.1865,p.2)
"Found in 1865 on line of railway from
Estremadura to Portugal but the means of transport was very costly”.
Woodward,S.P.? Geol.Mag.c1866/7
The second specimen sent by Mr. Munoz of Lima,
Torres, as Apatita di Jumella, a variety of phosphorite mineralogists call
moroxite, which occurs in large quantities at Jumella, and is likely to find
its way very soon onto the English manure market. It contained about 80 per
cent phosphate of lime.
"Extensive and valuable deposits of
phosphorite are found near Logrosan, in the neighbourhood of the towns of
Caceres, Montanchez, and other places in the province of Estremadura, in Spain.
Portugal also possesses extensive phosphate mines, and from both countries many
thousand tons are annually shipped to England at the present time. Dr. Daubeny,
who visited the Logrosan deposits in company with Captain Widdrington, stated
in his report, published in the Royal Agricultural Society's Journal for 1845,
that he found the deposits of the richest quality, and to be practically
inexhaustible; but that the want of roads, and the expense of transport to
Lisbon, the nearest shipping port, about 250 miles distant from the mines,
rendered them valueless until better means of communication should open up the
country.
Since the opening of the line of railway
connecting Madrid with Lisbon, in 1867, numerous Spanish and Portuguese
phosphate mines have been partially developed, mainly through the
instrumentality of companies under the Limited Liability Act of 1862. After
carrying on the mining operations for a few years, and sending the produce to
England, most of the companies, for one reason or another, have been cut short
in their existence. The chief drawback in working Spanish phosphate mines
successfully is the want of good roads, and the heavy expense which has to be
incurred in carrying the produce of the mines on the backs of mules to the nearest
railway station, and thence to Lisbon.
The means of communication in the districts
where the phosphate occur have been greatly improved of late years; still there
is ample room for further improvement in that respect, and in the mean time
Spanish phosphate mines are but little developed. There can be no doubt,
however, that these mines will furnish at no very distant period a considerable
proportion of the yearly supply of phosphatic minerals, for which there is a
constantly and rapidly increasing demand. Phosphorite of Logrosan has a light
yellow colour, and a fibrous crystalline structure, and is more or less
interlaced with veins of quartz. It is hard and difficult to powder, and
becomes phosphorescent on heating. The phosphate from Caceres mines is softer,
and of an almost perfectly white colour. Generally speaking Spanish and
Portuguese phosphorites have either a white or only slightly yellow colour. The
produce of different mines varies as much as regards hardness and richness in
phosphate of lime.
Phosphorite
is frequently found in Spain in solid beds, varying in dimensions, and
alternating with beds of limestone and quartz.
(Voelcker,Dr.A. 'On the Chemical Composition of Phosphatic Minerals used for
Agricultural Purposes,' Journ.Agric.Soc.1875,p409-413)
Voelcker’s analysis showed them to have a high
phosphate contents, up to 89% but generally ranging between 60% and 70%. As a
result he pointed out that,
"They find a ready sale in the English
market, and fetch a better price per unit per cent of phosphate of lime than
coprolites and mineral phosphates containing much oxide of iron and alumina,
inasmuch as superphosphate made from high-grade Spanish phosphate retain their
high percentage of soluble phosphate unaltered on keeping; whilst those made
from materials containing much oxide of iron and alumina, on keeping become
poorer in soluble phosphate, a portion of soluble phosphate becoming
precipitated, or reduced into insoluble phosphate by the presence of oxide of
iron and alumina."
Ibid.p413
Manure manufacturers, having read the article
would almost surely have increased their purchases of these minerals, helping
to explain why sales of coprolites fell so dramatically at the end of the
1870s.
SPANISH
and PORTUGUESE Phosphorites generally go under the name of Estremadura
phosphate, from the province in Spain where it is chiefly found. It is hard, of
light yellow colour, crystalline structure, and generally more or less mixed
with quartz, and becomes phosphorescent when heated. It is tolerably free from
iron and alumina, but contains variable and often considerable quantities of
flouride of calcium... In dissolving, from 30 to 33 per cent of the phosphates
in the superphosphates is rendered soluble; but, owing to the small quantity of
carbonate of lime in the mineral, the superphosphate when first made are
generally dense and damp, and require some time to get into good condition.
Reid,W.C. 'Mineral Phosphates and Superphosphate of Lime,'Chemical News
Aug.11th 1876 pp55-6
Although knowledge of Spanish mineral
phosphate deposits existed as early as 1808 it was only worked on a small scale
from 1845 in the province of Estremadura. (Captain Widdrington and Dr. Daubeny,
'On the Occurrence of Phosphorite in Estremadura,' Journ.Agric.Soc.1845; Geol.Mag.1845?
Verey,Sir H. 'On the use of Spanish Phosphorite as a Manure'
Journ.Ag.Soc.vol.vi.,1845?; Blakey,A.F. "The Florida Phosphate
Industry" Wertheim Committee, Harvard, 1973,p9,147) Its existence was
acknowledged in British agricultural journals
but it was stated that,
"...the great bed of Estremadura
phosphorite, which is at present not of sufficiently ready access to prove of
any practical importance to British agriculture... The phosphorite of Spain has
not been imported into this country to any considerable extent in consequence
of the great expense of getting it on board ship; at present therefore it is
not likely to be of any practical importance in the manufacture of
superphosphate of lime."
(Way,J.T.Journ.Ag.Soc.vol.xii.p215 )
However, during the 1840s European manure
manufacturers demand for whatever phosphate deposits they could get their hands
on, led to new workings opening at Cabo di Gata and Villa Rica in 1851 and a
deposit of apatite was found at Leigrosan, Estremadura. (Way,J.T.1851 p.253-5)
By the 1860s large quantities of moxorite were found in Jumella containing up
to 80% phosphate of lime and the opening of the railway to Portugal in 1867
allowed them access to the British market - but at a high price.
(Voelcker,Dr.A. Ph.D. Consulting chemist to the Royal Agricultural Society of
England. 'Raw Materials used as Manures, and Artificial Manures.' Rept.
International Exhibition, 1862, pp149-53; Woodward,S.P. '?' Geol.Mag.1866/7) By
the mid-1870s most of the deposits were being exploited and Voelcker described
how,
"Extensive and valuable deposits of
phosphorite are found near Logrosan, in the neighbourhood of the towns of
Caceres, Montanchez, and other places in the province of Estremadura, in Spain.
Portugal also possesses extensive phosphate mines, and from both countries many
thousand tons are annually shipped to England at the present time. Dr. Daubeny,
who visited the Logrosan deposits in company with Captain Widdrington, stated
in his report, published in the Royal Agricultural Society's Journal for 1845,
that he found the deposits of the richest quality, and to be practically
inexhaustible; but that the want of roads, and the expense of transport to
Lisbon, the nearest shipping port, about 250 miles distant from the mines,
rendered them valueless until better means of communication should open up the
country. Since the opening of the line of railway connecting Madrid with
Lisbon, in 1867, numerous Spanish and Portuguese phosphate mines have been
partially developed, mainly through the instrumentality of companies under the
Limited Liability Act of 1862. After carrying on the mining operations for a
few years, and sending the produce to England, most of the companies, for one
reason or another, have been cut short in their existence.
The chief drawback in working Spanish
phosphate mines successfully is the want of good roads, and the heavy expense
which has to be incurred in carrying the produce of the mines on the backs of
mules to the nearest railway station, and thence to Lisbon.
The means of communication in the districts
where the phosphate mines occur have been greatly improved of late years; still
there is ample room for further improvement in that respect, and in the mean
time Spanish phosphate mines are but little developed. There can be no doubt,
however, that these mines will furnish at no very distant period a considerable
proportion of the yearly supply of phosphatic
minerals, for which there is a constantly and rapidly increasing demand.
(Voelcker,Dr.A. 'On the Chemical Composition
of Phosphatic Minerals used for Agricultural Purposes,'
Journ.Agric.Soc.1875,p409-413
His analysis showed the these deposits to have
a high phosphate content, up to 89% but generally ranging between 60% and 70%.
(Reid,W.C. 'Mineral Phosphates and Superphosphate of Lime,'Chemical News
Aug.11th 1876 pp55-6) As a result he pointed out that,
"They find a ready sale in the English
market, and fetch a better price per unit per cent of phosphate of lime than
coprolites and mineral phosphates containing much oxide of iron and alumina,
inasmuch as superphosphate made from high-grade Spanish phosphate retain their
high percentage of soluble phosphate unaltered on keeping; whilst those made
from materials containing much oxide of iron and alumina, on keeping become
poorer in soluble phosphate, a portion of soluble phosphate becoming
precipitated, or reduced into insoluble phosphate by the presence of oxide of
iron and alumina."
(Voelcker,op.cit.p413)