MONTE NEGRAS DISTRICT.

Near the south boundary of San Bernardino County, and about 75 miles

directly east of Mount San Bernardino, a new mining district has been

organized within the past two years, and considerable development work

accomplished by the claim owners, who, as usual, are men of limited

means.

This district is 22 miles northeast of Cottonwood Springs, 16 miles

north of Eagle Mountain, and about 6 miles south from Virginia Dale. The

belt is about 1½ miles in width and 5 miles in length. The veins trend

north and south.

This new district, which has been named the Monte Negras, or Black

Mountain District, has attracted considerable attention by the discovery

in one of the claims of nuggets of gold and quartz of extreme richness.

At the time of this discovery some newspapers in this county published

the report that the mythical “Pegleg Smith” Mine had actually been

found, which only added to the excitement produced by the bringing into

San Bernardino of several hundred dollars worth of specimens.

I visited this new district in the month of May, 1892, and spent several

days in making an examination of the claims and adjacent country. The

Monte Negras camp is on the south side of the range of hills 45 miles

northeast of Walters Station, on the line of the Southern Pacific

Railroad, being reached by a fair desert road. By fair I mean a heavy,

but not rough or hilly road.

Walters Station is nearly 200 feet below the level of the sea. From that

point every foot of the way is up hill, till a divide near Cottonwood

Springs is reached, at an altitude of 3,157 feet, the distance being 27

miles; from there to the foot of the wash, which extends 2 or 3 miles

from the base of the mountains, down hill 19 miles, where the altitude

is 1,300 feet. The altitude of the camp is 1,520 feet. All the mines

lying back in the mountains are at higher, though varying, altitudes,

the greatest elevation being 3,500 feet, at the Ramona. The neighboring

peaks rise from 200 to 800 feet higher.

This district is distant about 35 miles from Cadiz, on the line of the

Atlantic and Pacific Railroad. I have never traveled the road, and know

nothing of it, although I am told it is a good desert road. Wood is not

obtainable at all in the vicinity of the mines, and water is scarce, but

has been obtained by sinking a well in a basin at Virginia Dale, a few

miles north of these mines. A shaft was sunk 140 feet in the wash 3

miles south of the most southerly Monte Negras mines, but no water was

obtained. Bedrock was not reached at the depth mentioned, but it is not

unlikely water may be secured by continuing this shaft downward.

I mention all these drawbacks to what I otherwise believe to be

promising property, because I think the difficulties may be offset by

the fact that the ore is high grade.

The Monte Negras uplift consists, as far as my observation extended,

entirely of eruptive rocks, diorite, quartz porphyry, and fine-grained

more or less porphyritic rocks, cut by later dikes of felsite and

dark-green or black diorite. Epidote occurs in great quantity throughout

the region, usually associated with micaceous iron ore, which is found

in the form of veins and bunches everywhere. The iron ores contain no

precious metals, and are of no economic importance.

The region, although entirely eruptive, and in part volcanic (large

fields of basalt occurring on the western slopes) is in the immediate

vicinity of a large hill called Pinto, or Painted Mountain, which is

made up of metamorphic strata, chloritic and hornblende rocks, quartzite

and mica schist predominating.

The mineral-bearing veins of the Monte Negras District are all of the

fissure type, and are mostly quite simple in form. The gangue is quartz,

carrying iron and copper sulphurets, and the secondary products of those

minerals, iron oxide and copper carbonate, with gold and silver. No lead

or zinc was observed. The economic value of the ore lies almost,

evidently, in its gold contents, the silver occurring so sparingly as to

amount to very little. The bullion obtained from these ores is worth

about $17 per ounce. The ore ranges in value from $20 to over $100 per

ton. Observations on the principal mines of this district, viz.: Great

Eastern, Venus, Columbus, Summit, Porcupine, Schiller, Hillerman, Annie

Rooney, Ethel, Republican, Ramona, McKinley Bill, and Revenue, have to

be omitted in order to condense the report.

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