LASSEN VOLCANIC NATIONAL PARK

An active volcano is the imposing exhibit in the Lassen Volcanic

National Park. The fiery Lassen Peak rises in the midst of telling

volcanic records that have been made and changed through many thousand

years.

This Park is in northern California. It is about one hundred and fifty

miles south of the Crater Lake National Park. The territory embraces

the southern end of the Cascade Mountains, the northern end of the

Sierra, and through it is the cross-connection between the Sierra and

the Coast Range. The area is about one hundred and twenty-five square

miles. The major portion of the Park lies at an altitude of between

six thousand and eight thousand feet, the lowest part being about four

thousand feet, while the highest point, the summit of Lassen Peak, is

10,437 feet above the level of the sea. The Park is reached by

automobile roads. It is easily accessible from the Southern Pacific

Railroad in the upper Sacramento Valley, and from the Western Pacific

Railroad on the Feather River.

The scientific and scenic merits of this territory were of such

uncommon order that in 1907 they were reserved in the Mount Lassen and

Cinder Cone National Monuments. Both these reservations are now merged

into the Lassen Volcanic National Park.

Lassen Peak is one of the great volcanoes of the Pacific Coast. Most

of the material in it, and that of the surrounding territory, appears

to be of volcanic origin. It is in the margin of one of the largest

lava-fields in the world. The lava in this vast field extends

northward through western Oregon and Washington and far eastward,

including southern Idaho and the Yellowstone National Park. It has an

area of about two hundred and fifty thousand square miles, over parts

of which the lava is of great depth.

Lassen is the southernmost fire mountain of that numerous group of

volcanoes that have so greatly changed the surface of the Northwest.

Among its conspicuous volcanic companions are Crater Lake, formerly

Mount Mazama, Mount Hood, Mount St. Helens, Mount Baker, and Mount

Rainier. Until Lassen Peak burst forth in 1914 it had slumbered for

centuries, and was commonly considered extinct. It has probably been

intermittently active for ages. Many geologists think that this

activity has extended through not less than two million years. Just

how long it may show its red tongue and its black clouds of breath is

uncertain; and just how violent and how voluminous its eruptions may

become are matters of conjecture.

All about Lassen Peak are striking exhibits of vulcanism--fields of

lava, quantities of obsidian or natural glass, sulphur springs, hot

springs, volcanic sand and volcanic bombs, and recent volcanic

topography, including Snag Lake.

Two of the imposing cañons here are Los Molinos and Warner Cañon.

These and other changes in the sides of Lassen Peak illustrate the

old, ever-interesting, and eternal story of erosion. Both these cañons

are wild places which have cut and eroded deeply into the ancient

lavas of Mount Lassen. Frost and water have reshaped the work of fire.

The mountain's sides show that it withstood the latest visits of the

Ice King. What appear to be the distinct records of glacial erosion

mark many spaces of its slopes.

[Illustration: LASSEN PEAK IN ERUPTION

_Copyright, 1914, by B. F. Loomis_]

The eruption of May 19, 1915, produced many changes. A volume of

super-heated gases burst out beneath the deeply snow-covered northeast

slope. The snow was instantly changed into water and steam. The mighty

downrush and onrush of water wrecked the channel of Lost Creek for

several miles. Meadows were piled with boulders, rock fragments, and

finer débris. Trees were uprooted or broken off, carried downward, and

left in piles of fierce confusion.

The hot gases played havoc with the forests. A stretch from a quarter

of a mile to nearly a mile wide and about ten miles long was killed by

the heat of the sweeping hurricane. Thousands of trees were instantly

killed and their green changed to brown. Others were charred. Forest

fires were started in a number of places.

The spectacular ruins which this left behind--the trees, wreckage,

slides, the changes made by ashes--may now be viewed with ease and

safety. It is probable that for years to come this volcanic wreckage

will be seen by thousands of visitors annually.

Fiery Lassen Peak is snow-crowned. One may ride to its summit on

horseback. From the top one has magnificent views of the mountains to

the north, the distant Coast Range, and the mountains eastward by the

Great Basin. On the whole, the surrounding mountain distances are

hardly excelled for grandeur in the entire country.

Cinder Cone is about ten miles to the northeast of Lassen Peak. It has

an altitude of only 6907 feet. It appears to have been built up

chiefly during the last two hundred years and for the most part by two

eruptions. One of these occurred nearly two hundred years ago. It

originated Stump Lake and ejected and spread materials over

considerable territory. The more recent eruption appears to have taken

place less than a century ago. In the summer of 1890 I found in the

crater a lodge-pole pine that was about eighty years of age.

Cinder Cone is a strikingly symmetrical small crater formed of cinders

and other volcanic products. It stands in a lava-field that has an

area of about three square miles. Its base measures about two

thousand feet in diameter, its truncated cone seven hundred and fifty

feet, and it is about six hundred and fifty feet high. Its

well-preserved crater is two hundred and forty feet deep and is nicely

funnel-shaped.

The Indians of the region had a popular tradition of the intense

activity of this cone about three centuries ago. This tradition was

that for a long time the sky was black with ashes and smoke. Thousands

of acres of forest were buried or smothered. The world appeared to be

coming to an end. But finally the sun appeared, red as blood. The sky

cleared, and volcanic activity ceased.

A number of the hot springs are agitated almost enough to be called

geysers. Cold and mineral springs abound. There are a number of lively

streams and plunging waterfalls.

The lake-area is twenty-three hundred acres. The largest of the lakes

is Lake Bidwell. Cinder Cone stands between two lakes which appear to

have been formerly one. The eruption of this cone probably extended a

lava-flow across the lake, dividing it into two parts. An outpouring

of volcanic material apparently made a dam, which formed a reservoir,

now occupied by Stump Lake. This filled with water and drowned a

forest growth. Through the surface of this lake still thrust numerous

tree-trunks of the drowned forest. The outburst of Cinder Cone that

formed this lake and overwhelmed the forest probably took place nearly

two hundred years ago. Other lakes are Juniper, Tilman, and Manzanita

Lakes.

The greater portion of the Park is forested. Among the more common

species of trees are Jeffrey pine, red fir, mountain hemlock,

lodge-pole pine, white fir, and incense cedar. In places among the

forests are beautiful mountain meadows.

There are scores of varieties of wild flowers. Most of these grow

under favorable conditions; have warmth, moisture, and rich soil; and

they show bright, clean blossoms. The district has its full share of

bird and animal life. In a number of streams fish are plentiful.

The Lassen Volcanic National Park was created chiefly through the

efforts of Congressmen John E. Raker and William Kent.

The varied objects of interest in this Park, especially those

associated with topography and geology, make it not only a place with

curious features, but a region affording unusual opportunities for the

gathering of fundamental facts concerning our resources. Here also are

scenes to inspire the souls of such as can be moved by the beauty and

grandeur of Nature and by the awful manifestations of her power.

Says J. S. Diller, of the United States Geological Survey, "With its

comfortably active volcano, inviting cinder cones and lava fields,

vigorously boiling hot springs, mud lakes and 'mush pots' for the

vulcanologist to study, and the glaciated divides and cañons for the

physiographer, in a setting of lovely scenery and attractive camps,

for the tourists all easily accessible, the Lassen Peak region affords

one of the most alluring and instructive spots for a National Park."

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