ora_, few in species, are
those of the other northern states of Mexico. Among the _fauna_ are--on
the west coast--sperm whales, otters, and seals. The Gulf of California
is stated to be one of the finest fishing grounds in the world:
including pearl-fishing.
If Baja California is poor in species of organic life, Nature has
compensated it in the mineral world, and that peninsula is considered
one of the most highly mineralised parts of the North American
continent. Copper, silver, and gold are among its most important
products, and quicksilver, opal, sulphur, and rock-salt exist. The
famous Boleo copper mine is situated in this territory, and some
extensive _placer_ gold mines are found near Ensenada. The principal
towns are La Paz, the capital of the southern district, and Ensenada,
of the northern.
Returning to the Mexican mainland we come to the states lying to the
south of those already described. Beginning at the west, as before, we
have the State of Sinaloa. This long narrow region lies between the
Sierra Madre on the east and the Pacific Ocean and Gulf of California
on the west, with a coast-line nearly 400 miles in length. Its area is
27,000 square miles, with a population of about 297,000 inhabitants.
Topographically the state may be divided into three zones--the coast,
the foothills, and the mountains; and in this it reminds the traveller
of California, to which it bears resemblance in many physical and
climatic respects. The coast zone consists of a well-watered and
fertile strip, producing all the crops of the tropics. Next comes the
foothill zone, rising gently to an elevation of 2,000 feet, and merging
into a fine timbered belt alternating with extensive natural pastures.
Well-watered valleys intersect this zone, capable of much cultivation,
and with splendid possibilities for irrigation, cattle-raising and
timber-cutting. Leaving this we enter on the more broken and
mountainous country, with a heavy growth of pine and oak forest,
grazing lands, and frequent streams, extending up to 4,000 or 5,000
feet elevation. This also is the rich mineral-bearing zone, whose oil
deposits have justly caused the state to be considered among the
foremost in the Republic in this field.
The Sierra Madre has a general and continuous elevation above sea-level
throughout the great length of this state, of 8,000 to 12,000 feet,
except the passes, which are crossed at much lower altitudes. The
mountains give rise to numero
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