"Katmai Calder, glacier, and Mt Griggs" by NPS , public domain
KatmaiBrochure |
Official Brochure of Katmai National Park & Preserve (NP&PRES) Alaska. Published by the National Park Service (NPS).
featured in
![]() | National Parks Pocket Maps | ![]() |
![]() | Alaska Pocket Maps | ![]() |
_____,_..
'
Katmai was declared a national monument in 1918 to preserve the living
laboratory of its cataclysmic 1912 volcanic eruption, particularly the
Valley of Ten Thousand Smokes. The intervening years have seen most
of the geothermal features die out. But there has welled up an equally
compelling interest: to safeguard the area's awesome brown bears. To
protect this magnificent animal and its varied habitat, the boundaries
were extended over the years, and in 1980 the area was designated a
national park and preserve. Katmai looms so vast that the bulk of it must
elude all but a very few persistent travelers. To boat its enormous lakes
and their island-studded bays, to float its rushing waterways, to backpack
-the wind-whipped passes of its imposing mountains, o r to explore its
Shelikot Strait coastline require great effort and logistical planning . This
unseen Katmai lurks beyond our usual experiences here of fishing from
B rooks Camp , walking up to Brooks Falls, and riding the van out to the
Valley of Ten Thousand Smokes. We come to Katma i to samp le but an
edg e o f t his enormity of raw natural forc es, a sampling that itself
constitutes a rare and endange red opp ortunity. Ka tmai's awe-inducing
na tural powers confront us most visib ly in its volcanics and its brown
bears: In summer North America 's largest land predator s gather along
streams to feast on the salmo n runs , those annual d isgorgings of oceanic
The 15 active volcanoes that line the Shelikof Strait
here make Katmai National Park and Preserve one of
the world 's most active volcanic centers today. These
Aleutian Range volcanoes are pipelines into the fiery
cauldron that underlies Alaska 's southern coast and
extends down both Pacific Ocean shores-the socalled Pacific Ring of Fire. This Ring of Fire boasts
more than four times more volcanic eruptions above
sea level than any other region in historic times.
Nearly 10 percent of these more than 400 eruptions
have occurred In Alaska; less than two percent in the
rest of North America. The current theory of plate
tectonics attributes this phenomenon to the collision
of the series of plates that compose the Earth's crust.
The Ring of Fire marks edges where crustal plates
bump against each other. Superimposing a map of
earthquake activity over a map of active volcanoes
creates a massed record of violent earth changes
ringing the Pacific Ocean from southern South America around through the Indonesian archipelago.
Major volcanic eruptions have deposited ash throughout the Katmai area at least 10 times during the past
7,000 years. Under the now quietfloor of the expansive
Valley of Ten Thousand Smokes, and deep beneath the
mountains that rise around it, there is still molten rock
present. Most visible as clues to this are the steam
plumes that occasionally rise from Mts. Mageik, Martin,
and Trident. These steam plumes show that there is
real potential for new eruptions to occur. And , in fact,
Mt. Trident has erupted four times in recent decades,
its last eruptive episode taking place in 1968.
A volcanic eruption capable of bringing about major
change could occur at any time in this tru ly dynamic
landscape. Since the great 1912 eruption, the massive
deposits of volcanic ash and sand that resulted have
con solidated into tutt, which is a type of rock. In the
valley these ash deposits have been rapidly cut through
by streams to form steep-walled gorges. The thousands
of fantastic smoking fumaroles that greeted the scientists who discovered the Va lley of Ten Thousand
Smokes after that powerful eruption (see story below)
have now all cooled and ceased their ominous smoking.
But the fiery cauldron, whose intense heat and pressure can be forcefully released to alter the landscape
radically in a matter of hours, still looms close to the
surface here in the park's portion of the vol canic Aleu·
tian Range.
A predictable eruption occurs here yearly as salmon
burst from the Northern Pacific and into park waters.
Sockeye salmon return from the North Pacific where
they have spent two or three years. By some homing
mechanism they return to the exact headwater gravel
beds of their birth. Their size, an average 2.2 to 3
kilograms (5 to 7 pounds), varies proportionally to how
long they spend in saltwater.
The salmon run be gins here in late June. By July's
end a million fish may have moved from Bristol Bay
into the Naknek system of lakes and rive rs . Salmonstop feeding on entering freshwater and physiological
changes lead to the distinctive red col or, humped
back, and elongated jaw they develop during spawning.
The salmon spawn during August and September.
Stream bottoms must have the correct texture of
loose gravel for eggs to develop. The strea m must
flow freely through winter to aerate the eggs. By
spring young fish, called smelt, emerg e from the
gravels and migrate into the larger lakes, living there
two years. The salmon then migrate to sea, returning
in two or three years to spawn an d begin the cycle
again. Salmon provide food for th e bears, bald eagles,
and other creatures that forage along streams during
the annual run . They also have been important to
Katmai peoples for sever al tho usand years , and com·
-
-
---- -- - ~ ~ -- - ------- ~-----------~-- ------------:---.
~------
Cover photo: Brown bea r on shore of Nakne k Lake. by To m Bean
protein-wealth into the upper freshwater world. Aiaska 's brown bears
and grizzlies are now considered one species. Peop le commonly consider grizzlies to be those that live 160 kilome te rs (100 mites) or more
in land. Browns are bigger than gr izzlie s beca us e of thei r high-protein
diet, t hanks primarily to the salmon that make a hea dlon g rendezvous
with death near the stream-bottom gra vels o th ei bi . Kod iak brown
bears are a different subspecies tha t is ge09raphica ll y isolated on
Kodiak Island in the Gulf of Alaska. Matu re mal e bears in Katmai may
weigh up to 400 kilograms (900 pounds). Mati ng oc curs fr m May to
mid-July, with the cubs born in dens in mid-winter. Up to fo ur cubs may
be born, at a mere half-kilo (1 pound) each. Cubs stay with the mother for
two years, during which time she does not reproduce. The interval
between litters is usually at least three years. Brown bears dig a new den
each year, entering it in November and emerging in April: About half of
their lifetimes is spent in their dens. Because each bear possesses
individual characteristics and behavior, no formulas can predict how a
given bear will act in a given situation. These awe -inspiring bears
symbolize the wildness of Katmai today.
Unseen Katmai
Wildlife
Volcanics
- -
mercial fishing - outside the park - remains the mainstay of today's local economy.
Flying into Katmai from nearby King Salmon you
cross over expansive Naknek Lake, your first clue to
the extensive system of lakes and rivers, streams and
marshes that is just one aspect of the unseen Katmai.
Katmai is so large and imposing of access that its
contrasting faces do not reveal themselves to the
usual itinerary. The vast systems of elongated lakes
nestl e in valleys gouged out by glaciers. The lower
slo pes of interior mountains are covered with birch,
poplar, and spruce forest. In the alpine tundra of the
higher slopes wildflowers abound in the brief summer
Katmai 's coastal mountains are part of the Aleutian
Range. These snow-clad mountains arc down the
Alaska Peninsula and culminate in the Aleutian Islands,
which are crests of a string of submarine volcanoes.
Katmai's high mountain passes are forbidding because of their foul weather and the intense winds that
result when major weather systems from the Gulf of
Alaska and from Siberia meet. The interior backcountry of many national parks is relatively little seen
by most travelers. All but the most minute fragments of
Katmai are backcountry wilderness, hence the un-
bald eagles, hawks, fal cons, and ow ls. Brow n bea rs
season_The
seen Ka tm ai.
and moose live throughout the coastal and lake regions,
the moose feeding on willows, water plants, and
grasses. Smaller mammals include the red fox , wolf ,
tial additio n to the park in 1980, offers brown bear
habitat and boasts extensive salmon spawning and
nursery areas. These homing salmon are critical here
to the bears, and elsewhere to commercial fishing.
Katmai 's lake edges and marshes serve as nesting
sites for whistling swans, ducks, loons, grebes, and
that 32,000-kilometer (20,000-mile) annual commuter,
the arctic tern. Sea birds abound along the coast ,
peregrine falcons nest among coastal cliffs , grouse
and ptarmigan inhabit uplands, and some 40 songbird
species summer here. Seacoast rock pin nacl es and
treetops along lakeshores provide nesti ng sites tor
secretive lynx and wolverine , river otter, mink, marten ,
weasel , and that natural hydro engineer, the beaver.
Along the coast are sea lions, sea otters, and hair
seals, wi th beluga and gray whales sometimes cruising the Shelikof Strait.
e o n try, which accounts for subs a n-
The interior mountains rise to about 900 meters (3,000
feet), but the coastal mountains, the ice-shrouded
backbone of the park and peninsula , reach above
2,100 meters (7,000 feet ). Deep bays, rock shoals,
sheer cliffs, and narrow beaches dot a rugged, indented
coast. This choppy coast provides habitat for marine
mammals and birds and for moose, bald eagles, and
brown bears. Wide valleys reach inland like corridors
into this ru gged range of wild and imposing coastal
mountains.
Crossing Martin Cree k
Eruption! And the Valley of Ten Thousand Smokes
The June 1912 eruption of Novarupta Volcano altered the Katmai area
dramatically. Severe earthquakes rocked the area tor a week before Novarupta exploded with cataclysmic force (see diagram). Enormous quantities
of hot, glowing pumice and ash were ejected from Novarupta and nearby
fissures. This material flowed over the terrain, destroying all life in its
path. Trees upslope were snapped off and carbonized by the blasts of hot
wind and gas. For several days ash, pumice, and gas were ejected and a
haze darkened the sky over most of the Northern Hemisphere.
When it was over, more than 65 square kilometers (40 square miles) of
lush green land lay buried beneath volcanic deposits as much as 200
meters (700 feet) deep. At nearby Kodiak, for two days a person could
not see a lantern held at arm's length . Acid rain caused clothes to
disintegrate on clotheslines in distant Vancouver, Canada. The eruption
was 1O times more forceful than the 1980 eruption of Mount Saint
Helens. Eventually Novarupta became dormant. In the valleys of Knife
Creek and the Ukak River, innumerable small holes and cracks devel-
oped in the volcanic ash deposits, perm itting gas and steam from the
heated ground water to escape.
It was an apparently unnamed val ley when the 20th century 's most
dramatic volcanic episode took place. Robert Griggs, exploring the
volcano 's aftermath tor the National Geographic Society in 1916, stared
awestuck off Katmai Pass across the valley's roaring landscape riddled
by thousands of steam vents. The Valley of Ten Thousand Smokes, Griggs
named it.
"The whole valley as far as the eye could reach was full of hundreds, no
thousands-literally, tens of thousands-of smokes curling up from its
fissured floor," Griggs would write. One thousand steam vents reached
150 meters (500 feet) in the air, some more than 300 meters (1 ,000 feet).
Such marvels inspired explorers on the next year's expedition:
" I felt like a boy at a circus, for I couldn 't take time to study the attraction
Robert Griggs th ought
t a a1 had blownhe found its new crater
lake o arupta Vol cano
subseq ently proved th e
source . al hough much of
the e1ec ted magma was
before me because I suspected something more capti va tin g farther on. "
" The meager pictures of the previ ous year . .. had not pr epa red me to
face such a spectacle of awesome magnitude . I had pictu re !! the Valley
as large; the actual view dwarfed my wildest imagery to insi g nificance."
" You may build in memory , but never reproduce the see n s which lie
beyond the Katmai Pass. They seem too big to be a part of th rest of the
world. They do not connect up with the little things which a. e built into
our lives."
The expedition's surveyor did not concur with such glowing a sessments
of natural wonders that seriously reduced visibility: "The smokes did not
impress me with their grandeur. . . . The ir ability to make surveying next to
impossible did ... A wool comfort placed on the ground which is 110°F ...
will steam beautifully. It is a natural phenomenon, but ii is not a good
bed." Nature can 't please everyone.
drained from beneath Mt.
Katmai. As Mt. Katm ai's
foundation was drawn
aw ay, its su mmi t su bsid ed, leaving a ca ldera
in wh ich a crater lake
formed . The ash flows
that spewed out over the
valley held their heat for
years. Surface water pe rcolating through them
was heated and vented to
the surface as fumaroles.
Only one eruption in historic times-Greece's Santorini in 1500 B .C.
-displaced more volcanic matter than Novarupta . The terrible 1883
eruption of Indonesia 's Krakatoa belched out little more than half as
much, yet killed 35,000 people. Vastly isolated Novarupta killed no one.
If the eruption occurred on Manhattan Island in New York City, Robert
Griggs calculated, residents of Chicago would hear it plainly. The fumes
would tarnish brass in Denver. Acid raindrops would burn your skin in
Toronto. In Philadelphia the ash would lie nearly as deep as this folder is
wide. Manhattan would have no survivors.
Today you can take the trip from Brooks Camp out to the Valley of Ten
Thousand Smokes, where the turbulent Ukak River and its tributaries cut
deep gorges in the accumulated ash. The landscape slowly recovers: In
nature, each destruction is somewhere's new creation.
·· GPO 1964 - 421·578 / 473
Ukak River. The streams
cut steep gorges in the
volcanic debris.
At Th ree Forks. in the
Valley of Ten Thousand
Smokes. Knife and Windy
Creeks join the River
Lethe, headed for the
Porcupines eat bark,
twigs, leaves, buds,
and an occasional piece
of camping gear.
The a~ oe Ar:iencan pit
house or ba'aoara used
effect .e sod nsi; a 100
Rock ptarmigan wear
whi te in wi nter, brown in
summer, and " mottled "
in between.
Access and Information
A skier surveys Katmai's
wintry backcou ntry from
a ridge on Baked
Mountain.
Red-necked grebes build
f loating nests in vegetat ion along shallow lake
marg in s.
Accommodations and Services
Katmai National Park and
Preserve I ies on the Alaska Peninsula 470 kilometers (290 miles)
southwest of Anchorage.
Daily commercial fl ights
connect Anchorage with
King Salmon, about 10
99613. Maps and books
about Katmai may be purchased by mail from the
non profit Alaska Natural
History Association at the
same address.
kilometers (6 miles) from
the park's west boundary.
Comm ercial float planes
operate daily between
King Salmon and Brooks
Camp from June to September.Year-round ai r
charter services are available in King Salmon.
boundary. Boat service
between Lake Camp and
Brooks Camp and elsewhere on Naknek Lake is
available from late June
through September.
Make all charter arrangements before vou arrive
to ensu re service that fits
your schedule.
A 14-kilometer (9-m ile)
dirt road connects King
Salmon with Lake Camp,
inside the park's west
Weather and Clothing.
Be prepared for
stormy weather
and some sun'
shine. Summer
~'!'t daytime temperatures range
from about 12° to 18° C
(mid- 50s to mid-60s F);
the average low is 7° C
(44 FJ. Strong winds and
sudde n gusts-williwaws
-frequently sweep the
area. Skies are clear
about 20 percent of the
sum mer. Light rain can
last for days.
For Information. Write
the Superintendent. P.O.
Box 7, King Salmon, AK
Bring comfortable outdoor clothes. Include a
warm sweater. wind-
'1
breaker or hghtw e1ght
fiberfill Jacket, footgear
that provides good support, woot socks, and a
wool hat. Rain gear
shou ld include ra incoat
and pants, parka, and hat.
A concessioner provides
accommodat ions and
services at five points in
the park and preserve
from June 1 into early
September. For addresses and information, write
to the park address.
Insects. You will need insect repellent!
Firearms. Hunting, or discharging any weapon . is
prohibited in the park,
and firearms must be unloaded and cased. Hunting - under Alaska State
law -and carrying firearms are allowed in the
preserve only.
Limited camping and food
supplies and some fishing tackle are sold at
Brooks Lodge. Several
commercial operators
are authorized to provide
air taxi, "flightseeing,"
backpacking, canoe, and
i ishing guide services in
the par and preserve
Write he park address
ora list.
Overnight services by
package rates are offered
at Grosvenor Lake, Kulik
Lodge, Battle Lake, and
onv1anu Camp Reser·
vat1ons are necessary.
Aea!s and accommodations are also a a1lable i
ing Salmon
lems with bears while
f ishing.
Regulat ions and Saf e ty
The National Par Service conducts guided
nature walks and evening
programs at Brooks
Camp from Memorial Day
to Labor Day week. I nformation, maps, and other
publications are available
at the Brooks Camp Visitor Center and at park
headquarters in King
Salmon .
At Brooks Camp are
B rooks Lodge, a campground , and the park's
summer headquarters.
Brooks Lodge on Naknek
Lake offers cabins (with
plumbing) that sleep four
per unit. The lodge serves
family-style meals.
Catch-and-release fishing is encouraged in
these trophy waters. Follow the suggestions
above for avoid rn g prob-
Seeing Katmai. A 37-kiloe er (23-mile) d road
be!Y. een B roo s Camp
and he Valley o · Ten
Thousand Smokes oilers
a view of this w ilderness
sculpted by glaciers,
stream erosion , and volcanism . A foot trail descends to the valley from
road's end. Concessionoperated vans make daily
rou nd-trip excursio ns to
the valley. Park rangers
accompany you.
Charter aircraft at King
Salmon and Brooks
Camp offer scenic fl ights.
In good weather you see
the bays, fjords, and
waterfalls along the coast,
glacier-clad mountains
with steam ing volc anic
peaks, and t e 1slandstudded lakes You may
fly o er the alley o Ten
Thousano Smo es seeing ;he 912 erup on
site
Backco untry Travel.
Katmai s rugged wilderness offers rewarding
experiences-with reaso nable precaut ions. Be
well prepared and
equipped. There are
several good short routes
and unlimited opportunities for long trips. Katmai
has few trails, but passable routes can be found
along river bars, lakeshores, and gravel
ridges. For overnight
Valley hikes you can
arrange a van d rop-off
and pick-up. For more
information, request the
free "Traveling the
Katmai Backcountry"
brochure.
Hiking Safety.
Cold 1t nds and cywa ers
pose grea hazards Gear
us '" nstand g
1>.rldS 80- -00 0 .50-60
m are not nusualancl b , ng ' 8 n Carry
extra cry clo ng. preferably woos Read up on
hypothermia symptoms
and their trea tment. Be
prepared to wait out
storms: carry matches,
fi rst aid kit, and emergency food . Rains or
melting glac iers can
make stream crossings
impossible. You need
sneakers and hiking
boots here. Be extremely
cautious when crossing
muddy waters. Streams
rise quickly during rainstorms or heavy glacial
melt.
Salmon. Backcountrv
campers must read the
bear safety leaflet/ There
is a National Park Service
campgrou nd with firepits,
tables, water, pit to ilets,
and a food storage cache
at B rooks Camp on
Naknek Lake. Wh ite gas
is available from the concessioner. Please use
stoves; firewood is
limited. Onl y deadwood
that is down may be used
for firewood. You can arrange in advance for
meals at the lodge. Otherwise. bring all food with
you.
Camping. You may camp
a yw ere in the park, but
·or backcoun ry camping,
p ease ob;a a permit
'ro · e B<oc-<S Camp
s :or Cer.:er or park
r.eadeuar:e·s n Ki ng
Because of bears and
other wild life. please
don't bring pets. Check
with the park for current
aircraft landing regulations. Leave archeo logical artifacts and historical
objects where you find
them .
Fishing. An Alaska fi shing
license is required in th e
park . Obtain a license
and regulations in King
Salmon or at B rooks
Camp. Catch-and-release
fishi ng is encouraged.
Brooks River is a flyfishing-onl v river. The
Naknek drainage offers
gray li ng, Dolly Varden,
northern pike, and the
more abundant rainbow
trout and sockeye (red)
sa lmon. Coho (silver) and
pink (humpback) salmon
are som etimes taken in
streams.
Boating Safety. Katmai
w aters can become suddenly viole nt. Know your
boat and its ope rat ion
before setting o ut. A ll
s tate and federal boati ng
regulations app ly. One
Coast Guard-approved
personal flotation device
is requ ired for each
person on a craft. Ca rry
signal equi pment. Don't
ov erload your craft; load
it low for stability. Beware
of underwater rock outcrops. Watch the weather
and stav ashore when
water is rough.
Wild River. The Alagnak
Wi ld River is managed by
the park staff. The upper
r iver is rocky and mod erately sw ift. Lower down it
slows, and you can take
leisurely floats throu gh
expans ive t undra.
Q
1 - 1Katmai
(}
L____) NationSI Park ~-~
~
~-0
()
r - - - - r Ka
m
~~
<>
·
ILIAMNA LAKE
_,£-
___ ·1
t.___.:! Trail
L____J Nat1a'lrtill"reserve
\/,0
c:::==J
!====J Unpaved ~cad
10 Ki19meters
20
~
~
""""'
f........
i.J.J
K A MJ S H A K
'-.J
~
B AY
'
-<
0
0
()
ATIONAL
PRESERVE
Mount Douglas
2153 m
7063 It .
-NATIONAL
-.u '"R'2.u- •
EsUno Pl1 Houae
---o-Brooks Camp ~=
•(II
Visitor Center
..
Mount Kelez
991 m
3250 ft .
Devils Desk
1954 m
64 11 n.
Alount Katohna1
1442 m
4 73() ft .
• ic;.ukak Vofc8no
2042 m
6700 ff
• Mount Ste'ler
2225 m
7300 n
Granite Peak
513 m
)683 ff
Mou nt Griggs
2316 rn
,.lflll<I ff
•325 m
1005 ft
Snowy Mountain
216 1 m
7090 ft .
Baked !-l<>untaon ""
.~~~
o~~
No~~f': • 4-(,
·Mount Katmai
2047 m
6715 ft
4860 ft
Katmai Pass •
·Trident Volcano
1832 m
6010 It
Mount \~ege1k
2210 m
Mount Martin
1844 m
60,.SO fl .
BECHAROF NATIONAL
W I LDL I FE R E F U G E
I
~
Ir----'
I ~
-~
f
PENINSULA
WILDLIFE
_,REFUGE
!.....,
~t
L,
~·~
~
/
<'
7250 ' ' ·
'.::"Qbservalion Mour:itein
994 m
• 32t30 t:.