"Views from the Lava Beds" by NPS photo , public domain
Lava BedsBrochure |
Official Brochure of Lava Beds National Monument (NM) in California. Published by the National Park Service (NPS).
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Lava Beds
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National Monument
California
National Park Service
U.S. Department of the lnterior
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A Turbulent Past
Man's activities in this rugged landscape
have been nearly as violent as the natural
forces that created it. For a million years the
volcano has spewed forth lava, gases, and
cinders, creating what seems to be an inhospitable landscape. Yet the youngest cinder
cones-1,0O0 years old-are covered by
vegetation that provides food and shelter for
wildlife. For centuries this area was home to
the Modoc lndians, who hunted in the valleys and mountains, fished in the rivers and
lakes, and used the tules (reeds) that grew
around the lake to make their homes, boats,
and other items. Their way of life was changed
forever by the arrival of settlers in the 1850s.
After repeated confrontations and much
bloodshed, the Bureau of lndian Affairs negotiated with all the Klamath bands in October 1864. The settlers were relieved, but the
negotiations were disastrous for the Modocs.
They were asked to give up their homeland
and to live on a reservation with bands who
were their traditional enemies. Finally, the
Modocs agreed to try living on the reservation, but within a few months they began to
leave. They returned to their old homes
saying that they wanted a reservation for
themselves on their ancestral land. Even
the reservation. On the morning of November 29, 1872, an Army patrol went out to
bring in the lndians, but fighting broke out.
lnitially victorious, the Modocs, under the
leadership of Captain Jack, drove off the
troops and sought safety in the lava beds,
where for almost five months 52 warriors
held off a growing army, eventually 20 times
larger. An effort to end the war by negotiation ended in even more bloodshed. By late
May almost all the Modocs had been captured, and on June 1, 1873, Captain Jack
more Modocs left the reservation in 1867.
surrendered. On October 3, 1873, he and
three other Modoc leaders were hanged.
By late 1872, the U.S. Army was ordered to
return the Modocs, by force if necessary, to
The remaining members of Jack's band were
sent to a reservation in Oklahoma.
Library of Congress
teffatn- The rhrc6 mon (betow ceoter) rook part in rho llrst b.ttlo .t Lod aivor. Glllsm's Camp (tclox, dgtrt) w.s noar tho 3hor€. ol Tuls Late.
National Archtves
National Archives
National Archives
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A Natural Wealth
At first glance the land looks barren, covered by
scraurny grasses and clumps of sagebrush. Closer
examination reveals much more. ln the north end
of the park, which is also the lowest in elevation,
these grasslands dominate and few trees are to
be seen. Further south, and higher, the vegetation
gradually changes as more and more junipers
intrude on the grasslands. Eventually, in the extreme southern reaches of the park, the grasslands,
disappear altogether and the junipers give way to
a pine forest.
All of this land is volcanic in origin and making
soil that can support plantlile takes a long time.
Once established, the vegetation provides shelter,
tood, and refuge for small animals who in turn are
a source of food for predatory animals and birds
of prey. ln the northern grasslands, squirrels, kangaroo rats, yellow-bellied marmots, jackrabbits,
Calilornia quail, meadowlarks, and the rare sage
grouse can be found. During the winter, mule deer
come from the other side ol the volcano lo feed
on the grasses in the park, where snowfall is less
and does not last as long. lndeed, so many deer
spend the winter in the park that watching deer
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is a popular pastime for visitors and local people.
An unusually large concentration of raptor birds
dwells in the park and throughout the Klamath
Basin. Several lactors make this environment
favorable. This area is home to many rodentsrats, mice, squirrels-for the birds to leed upon.
The cliffs at the northern edge of the park overIooking Tule Lake Sump provide the kinds ol nesting that these birds require. Nests are inaccessible
to nearly all predators and strategically positioned
so the birds can scan the countryside and take
quick notice of any activity. Chief among the raptors is the bald eagle that winters here in numbers greater than any place outside Alaska. Twentyfour species of hawks, falcons, owls, and other
birds of prey can be seen in the park. Since rodents are their chief torm of food, the birds are an
important check on what could easily be an infestation with the attendant problems of disease and
the devastation of crops outside the park.
For some, the most spectacular aspect of the
wildlite in the area surrounding the park is the
Flyway. Many waterfowl nest on the lakes of the
Klamath Basin, and in late spring the waters are
covered with thousands of ducklings, goslings,
and the offspring of other waterfowl. Despite the
magnificence of the springtime numbers however,
the fall gathering is even more spectacular, for approximately 2 million ducks and 1 million geese
stop here to rest and feed on their way south,
some birds coming lrom as lar away as Siberia.
There are times when the sky is literally darkened
by the arrival oI a very large llock of birds, an
increasingly rare event in North America. The road
from the northeast entrance into the park is parallel to the common boundary of the park and the
Tule Lake Unit of the Klamath Basin National Wildlife Refuge. From vantage points along the way
you can watch more than 20 species of ducks, plus
many varieties of geese, grebes, pelicans, herons,
cormorants, gulls, coots, terns, avocets, and other
birds.
Enjoy your visit to the park and the variety-both
in history and natural wonders-that it has to offer.
semiannual migration of birdlife along the Pacific
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Regulations
Lava Beds
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o All natural and historical objects must be
left in place and
undisturbed.
o Hunting, gathering
specimens, and collect'
a leash. They are not
permitted on trails or
in caves or public
wildlite.
o All weapons must be
ing souvenirs are
prohibited.
o Pets must be kePt on
o Do not leed or molest
buildings.
broken down or cased.
o Base hunting camps
are not permitted.
a Be carefulwith all
lire, including cigarettes, and make sure
your campfire is out
and al! embers are
extinguished.
o Vehicles are restricted to roads..
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Collapsed roofs, crustose lichens, perfectly
formed tubes, and yearround ice are just samples of what you can
expect to find in the
A
Hidden World
hasa historyol
itLaieaot noittrern
Catifornia
lava caves. Exploring
them can be exciting, if
you take the proper precautions and use commonsense. Make sure
that you wear some-
thing on your head; hard
hats are for sale in the
visitor center. Wear
hard-soled shoes, because the lava can be
sharp. And carry at least
thellowcool rapidly, however, and b6ginloslow
,oi"*iinr- ffr. f.q""v ot those times-and iishould down and harden. This outside layer aats as insu-
lating malerial while the rest ol the llow beneath it
.iifr" prdi* ifti" *sfon is considore; active-is rema-ins hot and lasl-moving. The flow continuos
on, somewhal llke a dver that koeps on llowing
att arouna.-CinOer cones, shield volcanoes, slEtoeven though lhe su ace has lrozon over. When
volcanoes, lava tubes, tlows ol both Pahoehoe
ropvt unO Aa (rough and clinker-lik€) the erupti;n stops and the river ot lavs ceases, a
t"ro"if,
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tunnel or tube-lhe outer shell-is lefl. The numchimniys are all a part ot
i"r", ip"tt..
"."-.'", -a ot ths ;ost striking volber ol tubes in sny one tlow varies. Lava tubos lie
ifrf" L-ir"v. p.itr"p'io"e
canic ;alures in Lava Bods is lhs phenomenon alop one anolher, the resu lt ot su bsequent tlows,
Th€ most rccent tubes in tho parkurereloamed
ol lavalubo caves.
about 3O,OOO years ago from lava llowsthat came
trom Mammoth craffiheudrtSlgouthe.n
Levatubos are not particularly unusual irrayolnot be assumod tiat; votcanic activity is a thing
ca"l"
*r l"ifrit, f.rmati;n dilticult to exiiii" .i"i*,rai."t""a. u"arly 2oocaves havo been
Ior"t a *itfti"ift" p*t, m;king thesetormafionjan especiaffy prominentl;atu@.
boundary.
When lava pourslrom a volcano lt is extremely hot
(abour 1 SOOo F)- The outer 6dges and su rlace ol
During lhe cooling procoss, portions of the tubes'
roofs;ollapse. These opsnings make it possible
for plants, animals, and precipitation to enter the
caves and create a world ol lile within them. A
few ot lhe tubss ar€ i@ caves; rain collects in lhem
three different sources
of light;free lights are
available in the visitor
center. Do not explore
the caves alone.
and the air temperature remains fairlv constanl-
bolow treezing. Even when temperatures reach
10OoF outside, lava is such a good insulator thal
the air remains cold and ic€ lormations can be
tou nd the year round.
Many ol the cavqs were firsl exDlor€d and named
by J.D. Howard, a local rancher. The names he
painted on lhe walls ar€ still Yisible in most ol the
caves. ln many of lhe caves, trails have b€sn laid
out and ladders inslalled to makeaccesseasy.
Many of these caves lie otf Cave Loop Road, south'
wastof ptat@rs;
llrushpot ervs'En ex;
tonsion ofthe visitor center, is the onlv cave ln
which lighls have been installed. Before ontar
ing anv cave, check at th€ visllor cenler lor inlormation on spacilic caves and lor goneral salely
informalion.
ill cr.psrornd
fl Lookout lower
m Ranger station
ffi lnterpretive trail
f:_-_"r Unpaved road
o
H
lr, Picnic area
Overlook
Petroglyph
Section
North
TULE LAKE SUMP
Kilometer
Dike Road
lnlormation
Eg:t.wlldlife Kiosk
West Wildlife
Overlook
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1.5 mi loop
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Park Information
Park headquarters for
Lava Beds National
Monument is 30 miles
from Tulelake, Calif .,
and 58 miles from
Klamath Falls, Ore.
Watch .l39,5
for signs on
Calif.
miles
south of Tulelake and
26 miles north of
Canby. Airlines serve
Medford and Klamath
Falls where rental cars
are available.
Tourist Information
Food, lodging, gasoline, oil, and auto repairs are available in
Tulelake and Klamath
Falls. Near the visitor
center a 40-unit campground with sites suitable for tents, pickup
campers, and small
trailers is open all year.
There are no hookups.
Water is available during the summer. From
September 15 to May
15 water is available at
the visitor center. The
Fleener Chimneys picnic area has no water,
and open f ires may not
be built there.
50oF. Precipitation during the summer averages 1.25 inches or
less per month.
ln the summer park
rangers lead daily walks
o There is a large pop-
and cave trips and conduct campf ire programs. Check bulletin
boards or ask at the
visitor center for the
schedule. The park
ranges in elevation
from 4,OOO to 5,700
feet, and at these
heights cold weather is
possible any time of the
year. Snow has been
recorded in nearly all
months. ln the winter
daily high temperatures average around
4OoF; lows are 2OoF.
Fog is frequent
throughout the winter.
Summers are moderate, with daytime highs
averaging from 75o to
8OoF and lows about
Safety
ulation of ground squirrels and other rodents
in the park. Rodents
are known to harbor
f leas that catry a bacterium that causes Bubonic Plague. Leave all
rodents alone.
o ln the winter large
numbers of deer are in
the park, and especially at dawn and dusk
they can be found on
the roads. Be alert
when you are driving.
o Owls, too, often sit
on the roads, so be
alert for them at night.
o When you are exploring caves, you willencounter a number of
potential hazards.
Watch out for low ceilings, steep trails, and
l,il,
COkm
66mi
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Macdoel
uneven footing. Take
more than one light
source and wear protective headgear. Cave
temperatures are cool,
so wear adequate clothing. Get a permit from
a park ranger to go
into a cave other than
those shown on the
map in this folder.
a Rattlesnakes are
found throughout the
park; do not put your
hands and feet in
places where you cannot see. Snakes are
an important and protected part of this
ecosystem.
lf you have questions
or comments, ask any
park ranger. We are
here to help you. For
further information,
write to. Superintendent, Lava Beds National Monument, Box
867, Tulelake, CA
96134.
*GPO: 1985-461-444/20105