Crater-Lake-Park-Map

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Crater-Lake-Park-Map To Diamond Lake, Roseburg, and 5 Pacific Crest National Gasoline Lodging 0 1 2 3 4 5 Kilometers MOUNT THIELSEN Scenic Trail (PCT) 0 1 2 3 4 5 Miles WILDERNESS Other hiking trail Picnic area Food service North (UMPQUA and WINEMA NATIONAL FORESTS) Pets are prohibited Campground Store on all hiking trails Summit Rock Beaver Offroad driving is Backcountry campsite Showers Meadows 6050ft UMPQUA NATIONAL 1845m prohibited (permit required) FOREST PCT parking Creek uir M 230 ( k ) or F Cascade Mountain Pass 138 t as gue River 5925ft E Ro 1846m To Bend, Eugene, and 97 North Entrance Station 5850ft T Lake West 1783m in y Creek To Medford and 5 ha eha ) inn y M l n Cr o ee k r e m Boundary Springs D Gaywas Peak m u E s 6781ft S n E 2067m e R p T o ( ROGUE RIVER R ID G WINEMA E NATIONAL NATIONAL FOREST E Timber Crater FOREST G D 7424ft I Bald Crater 2263m R 6478ft T 1975m N l CE i CRES a r ek T e Desert Cone Collecting rocks Cr Nationa 6672ft and other natural l ek re 2034m objects prohibited C c rt i se n De PUMICE DESERT e c S l na tio Na t s k e e Oasis Butte r re C C 5842ft fic 1781m Paci t n Sharp Peak le 5991ft Si CRATER LAKE NATIONAL PARK 1827m Bert ek Cre Red Cone 7363ft 2245m No stock south of this point, hikers only Sphagnum Bog ) Red Cone Spring Grouse Hill Fragile wetlands, ed 7412ft no camping ow 2260m k ll ree a Lookout Bluff C tock rs and s 6118ft (hike 1865m Cleetwood Trail To tour boat landing Bear Butte er l rat i ) 6376ft C a ly r on 1944m T rs e Spruce Lake k k i d e h re ( Llao Rock o e C o v t 8049ft Steel w o s r Pumice Point et C a e 2453m e R e Scout Hill r Bay l C Palisade im B C ( 6376ft Point op 1944m en ive su Dr c m i y) f m nl i North Junction er o c 7025ft Llao Bay a P 2142m Merriam Point -1788ft Merriam Cone Wineglass -545m -486ft Devils Backbone -148m Grotto Pothole Butte Cove 6150ft Williams Crater Deepest point 1875m Hillman Peak below lake surface: S 8151ft l -1943ft F 2484m e F n -593m U n L a B h C T Skell T The Watchm an O -96ft Head 8013ft C l WIZARD S 2442m l -29m Crater Lake e ISLAND ek D Cre ee Bybee k Average surface elevation: Cloudcap Pothole r Creek S 6940ft 6173ft Bay ole 2116m 1882m er Cloudcap Overlook C y ree m a 7960ft k u B F G 2427m Lightning B o a v Spring y e rn Pumice Castle o r R s im -1548ft Sentinel Rock -472m D Discovery Point Mount Scott r i 7100ft v (highest point in park) 2165m Castle e 8929ft (o Danger 2721m Cree p Rim Village k e Bay n Cafeteria and Gift Shop W s h u Phantom Ship Overlook i m Sinnott Memorial Overlook sk e m Kerr Notch y er only) Rim Village Visitor Center (summer only) To Medford Crater Lake Lodge Phantom A 62 N and 5 C Ship DE ha K R ski Bay Dutton SO k E N C e Garfield Peak Cliff R B r e R LU e r V F e 4850ft 8054ft 8106ft A FS C Sun Notch LLE k 1479m k 2455m 2471m Y S e a e tle Creek r n s D d Ca C Applegate Peak Sc Little Park Headquarters ot n 8126ft U t r HistoricTrail U o T e t 2477m t n p V T No stock north C i p u o a I O r of this point, Visitor D n r D Castle Crest e T N e hikers only A WildflowerTrail k C Information E r R e e Castle I k R Steel Information Center D C I C Park Headquarters D G r reek E e 6450ft G e 1966m E k Munson Point Vidae Falls 6944ft 2117m Rim Thousand k Dri Castle Point e ve e su Springs r r en mm G op e C 6276ft ( r L C C o r 1913m Whitehorse Pond nl a o a y v e ) y s n ay b e w Lost Creek t e y on o r b a W s c C n d k Annie Spring r n h o u Drive ee o le P M r I G G N k R N r A A Annie Spring o Y F B C L ROGUE RIVER Entrance Station A E Duwee Falls C Su K C V r n e A C Godfrey Glen Trail R e Mazama Village k L r I L e D E NATIONAL Annie Creek G Y e Cr k Canyon Trail eek E Dry Butte 6004ft k 5735ft r e T l H 1830m A o E 1748m Arant Point d F P FOREST n IN d N 6800ft n i AC i LES 2073m e M Quillwort Pond Pinnacles Crater Peak Huckleberry Mountain t Overlook C s 7263ft 6370ft r a e E 2214m 1942m e Sa k n dge Creek d Bri Rocktop Butte le o 6400ft P C 1951m re e Maklaks Crater k 6404ft 1952m Union Peak 7709ft 2350m k e e 6253ft r 1906m C A n 6091ft PUMICE n 1857m t ie WINEMA NATIONAL in Scoria Cone m FLAT 6648ft ar Cr S V 2027m eek A Baldtop N FOREST 6200ft D 1890m R S I u D n t Creek Stuart Falls G e l k i W n E la a i B r ld T c a C t r C e e c Goose Nest r d i e e k n 7249ft e R k e 2210m c S al n o i t a SKY LAKES N Crest WINEMA NATIONAL Sun Mountain WILDERNESS c 5550ft i f i FOREST 1692m (ROGUE RIVER and WINEMA NATIONAL FORESTS) c a P Goose Egg 7124ft Tom Mountain 2172m SUN PASS STATE FOREST Bessie Rock 6876ft 4400ft 62 Cinnamon Peak 1341m 5900ft 6367ft 2096m Jerry Mountain 1799m 1941m To Klamath Falls and 97.
Recommended publications
  • Overview for Geologic Field-Trip Guides to Mount Mazama, Crater Lake Caldera, and Newberry Volcano, Oregon
    Overview for Geologic Field-Trip Guides to Mount Mazama, Crater Lake Caldera, and Newberry Volcano, Oregon Scientific Investigations Report 2017–5022–J U.S. Department of the Interior U.S. Geological Survey Cover (top photo): View east-northeast from Garfield Peak on the south rim of Crater Lake caldera. Peak on skyline is 8,929 feet (2,722 meters) Mount Scott, an ~420 thousand years before present (ka) dacite stratovolcano considered to be part of Mount Mazama, the volcano that collapsed during the caldera-forming eruption ~7,700 years ago. The caldera walls in this view expose Mazama lava flows and fragmental deposits from as old as ~400 ka at Phantom Cone, adjacent to tiny Phantom Ship island, to as young as ~27 ka at Redcloud Cliff, the V-shaped face at the top of the wall left of center. The beheaded glacial valley of Kerr Notch, the low point on the caldera rim, is seen between Phantom Ship and Mount Scott. Photograph by Carly McLanahan. Cover (bottom photo): Newberry Volcano, Oregon, is the largest volcano in the Cascades volcanic arc. This north-facing view taken from the volcano’s peak, Paulina Peak (elevation 7,984 feet), encompasses much of the volcano’s 4-by-5-milewide central caldera, a volcanic depression formed in a powerful explosive eruption about 75,000 years ago. The caldera’s two lakes, Paulina Lake (left) and the slightly higher East Lake (right), are fed in part by active hot springs heated by molten rock (magma) deep beneath the caldera. The Central Pumice Cone sits between the lakes.
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  • Introduction to Crater Lake
    National Park Service Crater Lake U.S. Department of the Interior Crater Lake National Park Introduction to Crater Lake Crater Lake Is Like No Crater Lake has inspired its visitors for hundreds of years. No place else on earth Place Else On Earth combines such a deep, pure lake with sheer surrounding cliffs and a violent volcanic past. Few places on earth are so beautiful, so pristine, or—for these very reasons—so interesting to scientists. An Introduction to Crater Lake is located in Southern Oregon on the Following the collapse of Mount Mazama, lava Crater Lake crest of the Cascade Mountain range, 100 miles poured into the caldera even as the lake began to (160 km) east of the Pacific Ocean. It lies inside a rise. Today, a small volcanic island, Wizard Island, caldera, or volcanic basin, created when the 12,000 appears on the west side of the lake. This cinder foot (3,660 meter) high Mount Mazama collapsed cone rises 767 feet (234 meters) above the lake and 7,700 years ago following a large eruption. is surrounded by black volcanic lava blocks. A small crater, 300 feet (90 meters) across and 90 feet Generous amounts of winter snow, averaging 528 (27 meters) deep, rests on the summit. The crater is inches (1,341 cm) per year, supply the lake with filled by snow during the winter months, but re- water. There are no inlets or outlets to the lake. mains dry during the summer. Crater Lake, at 1,943 feet (592 meters) deep, is the seventh deepest lake in the world and the deepest The lake level fluctuates slightly from year to year.
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  • USGS Scientific Investigations Map 2832, Pamphlet
    Geologic Map of Mount Mazama and Crater Lake Caldera, Oregon By Charles R. Bacon Pamphlet to accompany Scientific Investigations Map 2832 View from the south-southwest rim of Crater Lake caldera showing the caldera wall from Hillman Peak on the west to Cleetwood Cove on the north. Crater Lake fills half of the 8- by 10-km-diameter caldera formed during the climactic eruption of Mount Mazama volcano approximately 7,700 years ago. Volcanic rocks exposed in the caldera walls and on the flanks record over 400,000 years of eruptive history. The exposed cinder cone and andesite lava flows on Wizard Island represent only 2 percent of the total volume of postcaldera volcanic rock that is largely covered by Crater Lake. Beyond Wizard Island, the great cliff of Llao Rock, rhyodacite lava emplaced 100–200 years before the caldera-forming eruption, dominates the northwest caldera wall where andesite lava flows at the lakeshore are approximately 150,000 years old. 2008 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank. CONTENTS Introduction . 1 Physiography and access . 1 Methods . 1 Geologic setting . 4 Eruptive history . 5 Regional volcanism . 6 Pre-Mazama silicic rocks . 6 Mount Mazama . 7 Preclimactic rhyodacites . 9 The climactic eruption . 10 Postcaldera volcanism . .11 Submerged caldera walls and floor . .11 Glaciation . .11 Geothermal phenomena . 12 Hazards . 13 Volcanic hazards . 13 Earthquake hazards . 14 Acknowledgments . 14 Description of map units . 14 Sedimentary deposits . 15 Volcanic rocks . 15 Regional volcanism, northwest . 15 Regional volcanism, southwest . 17 Mount Mazama . 20 Regional volcanism, east . 38 References cited .
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  • Mount Mazama and Crater Lake: Growth and Destruction of a Cascade Volcano
    U.S. GEOLOGICAL SURVEY and the NATIONAL PARK SERVICE—OURVOLCANIC PUBLIC LANDS Mount Mazama and Crater Lake: Growth and Destruction of a Cascade Volcano or more than 100 years, F scientists have sought to unravel the remarkable story of Crater Lake’s formation. Before Crater Lake came into existence, a cluster of volcanoes dominated the landscape. This cluster, called Mount Mazama (for the Portland, Oregon, climbing club the Mazamas), was destroyed during an enormous explosive eruption 7,700 years ago. So much molten rock was expelled that the summit area collapsed during the eruption to form a large volcanic depression, or caldera. Subsequent smaller eruptions occurred as water began to fill the caldera to eventually form the The cataclysmic eruption deepest lake in the United States. of Mount Mazama 7,700 Decades of detailed scientific years ago began with a towering column of pumice studies of Mount Mazama and and ash, as depicted in this new maps of the floor of Crater painting by Paul Rockwood (image courtesy of Crater Lake reveal stunning details of Lake National Park Museum and Archive Collections). the volcano’s eruptive history and After the collapse of the identify potential hazards from summit of the volcano, the caldera filled with water to future eruptions and earthquakes. form Crater Lake. (Photo by Willie Scott, USGS) formation of Crater Lake and with it the Applegate and Garfield Peaks. During the When Clarence Dutton of the U.S. demise of Mount Mazama. growth of Mount Mazama, glaciers repeatedly Geological Survey (USGS) visited Crater carved out classic U-shaped valleys.
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  • Mount Mazama and Crater Lake: a Study of the Botanical and Human Responses to a Geologic Event
    AN ABSTRACT OF THE THESIS OF Robyn A. Green for the degree of Master of Arts in Interdisciplinary Studies in Geology. Botany and Plant Pathology. and Anthropology presented on June 3. 1998. Title: Mount Mazama and Crater Lake: A Study of the Botanical and Human Responses to a Geologic Event Abstract approved: / Robert J. Lillie Crater Lake, located in the southern Cascade mountains of Oregon, is the seventh deepest lake in the world. Unlike a majority of the deepest lakes in the world, found in continental rift valleys, Crater Lake is in the caldera of a volcano. For the young at heart and mind, those willing to descend (and ascend) about 700 feet to Cleetwood Cove can undertake a boat tour of Crater Lake. From the boat, Crater Lake is more than just a beautiful blue lake; it becomes the inside of a volcano, where the response of people and plants to a geologic event can be investigated. The catastrophic eruption of Mount Mazama 7,700 years ago affected both plant and human populations. Before pumice and ash from the volcano blanketed the landscape like freshly fallen snow, the forests to the east of Mount Mazama were dominated by ponderosa and lodgepole pine. Within the immediate vicinity of the volcano all life was obliterated; the force of the eruptive material toppled vegetation and buried it with ash and pumice. Through the recovery process of succession, life has slowly returned to Crater Lake. Forests surrounding the lake are now dominated by mountain hemlock, whitebark pine, and lodgepole pine. These plants not only depict the process of succession, but also of adaptation to a volcanic environment.
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  • Crater Lake U.S
    National Park Service Crater Lake U.S. Department of the Interior Refections Visitor Guide Summer/Fall 2017 Park News 2 ... Camping, Lodging, Food Visit the Sinnott Overlook 3 ... Ranger Programs f Water Restrictions in Effect Please help us conserve water during Plus 10 Other Ways to Enjoy Your Park 4 ... Hiking Trails your visit. The park’s ability to provide 5 ... Driving Map water is currently restricted as we The Sinnott Memorial Overlook ofers one of the ... In the News: Bull Trout transition from a surface water source fnest views of Crater Lake. You can peer down a 6 to a groundwater well. If you’re sheer drop of nearly 900 feet (274 meters) to the 7 ... Feature Article: Lake Level reading this before arriving, please shore! It also features the park’s best exhibits. A small stock up on water outside the park. 8 ... Climate Chart museum describes the lake’s geology, formation, and While you’re here, please take short exploration. (Of special interest is the original device showers, don’t run the tap, and reuse used by scientists to measure the lake’s depth in 1886.) towels and sheets if staying overnight Look Inside! in park lodging. Thanks for your help! Finding this special viewpoint can be a challenge. f Leave Your Drone at Home It’s hidden behind the Rim Visitor Center, perched on a promontory 50 feet (15 meters) below the rim. Operating remote-controlled aircraft Landscape architect Merel Sager, who oversaw in the park is prohibited. Please report Park Profle violators to the nearest employee.
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  • Crater Lake National Park
    CRATER LAKE National Pa^rR O T*~ E O O W UNITED STATES RAILROAD ADMINISTRATION N AT IONAU PARK SERIES Reflections stand out distinctly in water that gleams as though glazed by the sun Looking "Over the Top" Page two An Appreciation of (rater Lake National Park By WINSTON CHURCHILL, Author of "The Crisis," "Richard Carvel," "The Crossing," etc. Written Especially for the United States Railroad Administration i|T IS not so man) years ago that I left San Francisco with a case of rods, bound for Crater Lake in Oregon. What I had heard about the place had filled me with awe and expectation, tempered by a little skepticism. I was personally conducted by patriotic and hos­ pitable Oregonians who met me in sight of the fountains of Klamath, put me in a motor car and sped me northward through great forests and across wide prairies which once, not long since, had been an almost inaccessible wilderness. The immensity of the extinct volcano whither we were bound, that in prehistoric times had strewn the entire countryside with powdered stone, was hard to grasp. It was July. We climbed the wooded slopes to the snows, forged through the melting drifts to the very lip of the crater and suddenly looked down upon a scene celebrated in Indian myth, and unique in all America. Some thousand feet below us lay a bottomless crystal lake, six miles across dotted with black volcanic islands. My delight in the grandeur of this view, it must be confessed, was heightened by the knowledge that the lake was in­ habited by large rainbow trout which would rise to the fly.
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  • Morphology, Volcanism, and Mass Wasting in Crater Lake, Oregon
    Morphology, volcanism, and mass wasting in Crater Lake, Oregon Charles R. Bacon* Volcano Hazards, U.S. Geological Survey, 345 Middle®eld Road, MS 910, Menlo Park, California 94025-3591, USA James V. Gardner Western Coastal and Marine Geology, U.S. Geological Survey, 345 Middle®eld Road, M.S. 999, Menlo Park, California 94025- 3591, USA Larry A. Mayer Center for Coastal and Ocean Mapping, University of New Hampshire, 24 Colovos Road, Durham, New Hampshire 03824, USA Mark W. Buktenica National Park Service, Crater Lake National Park, P.O. Box 7, Crater Lake, Oregon 97604, USA Peter Dartnell Western Coastal and Marine Geology, U.S. Geological Survey, 345 Middle®eld Road, M.S. 999, Menlo Park, California 94025- 3591, USA David W. Ramsey Joel E. Robinson Volcano Hazards, U.S. Geological Survey, 345 Middle®eld Road, M.S. 910, Menlo Park, California 94025-3591, USA ABSTRACT The ¯at-¯oored, deep basins contain relatively ®ne-grained sedi- ment transported from the debris aprons by sheet-¯ow turbidity Crater Lake was surveyed nearly to its shoreline by high-reso- currents. Crater Lake apparently ®lled rapidly (ca. 400±750 yr) lution multibeam echo sounding in order to de®ne its geologic his- until reaching a permeable layer above glaciated lava identi®ed by tory and provide an accurate base map for research and monitor- the new survey in the northeast caldera wall at ;1845 m elevation. ing surveys. The bathymetry and acoustic backscatter reveal the Thereafter, a gradual, climatically modulated rise in lake level to character of landforms and lead to a chronology for the concurrent the present 1883 m produced a series of beaches culminating in a ®lling of the lake and volcanism within the ca.
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  • Crater Lake National Park Oregon
    CRATER LAKE NATIONAL PARK OREGON. The Sinnott 'Memorial on the <r\im of (f rater Lake UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE HORACE M. ALBRIGHT, Director GENERAL INFORMATION REGARDING . U full/! : GRATER LAKE NATIONAL PARK OREGOX (c) Sawyer Scenic Photos, Inc. THE LAKE WITH PHANTOM SHIP IN FOREGROUND " It lies 2,000 feet under your feet, and reflects its walls so perfectly that you can not tell the wall from the reflection in the intensely blue water."—Joaquin Miller OPEN EARLY SPRING TO LATE FALL UNITED STATES GOVERNMENT PRINTING OFFICE RELIEF MODEL OF CRATER LAKE AND THE SURROUNDING REGION WASHINGTON : 1933 RULES AND REGULATIONS BRIEFED The park regulations are designed for the protection of the natural beauties and scenery as well as for the comfort and convenience of visitors. The following synopsis is for the general guidance of visitors, who are requested to assist the administration by observing the rules CONTENTS Page The geological story of Crater Lake 1 Fires. Light carefully and in designated places. Extinguish com­ Places of interest 5 pletely before leaving camp, even for temporary absence. Do not Discovery and history i 7 guess your fire is out—Know it. Wild animals 8 Bird life 9 Camps. Use designated camp grounds. Keep the camp grounds Fishing 10 clean. Combustible rubbish shall be burned on camp fires and all The forests j 11 other garbage and refuse of all kinds shall be placed in garbage cans Notes on the wild flowers 12 or pits provided for the purpose.
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  • Crater Lake Riend F L N Y E E
    CRATER LAKE RIEND F L N Y E E R G S T P C R O D U Gallery Giclee Fine Art Prints With Digital Matting AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-199 CRL-215 CRL-6 CRL-169 AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-375 CRL-378 CRL-2683 CRL-2687 AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-2691 CRL-2698 CRL-2704 CRL-2711 AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-2882 CRL-2891 CRL-3033 CRL-3085 AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-179 CRL-18 CRL-119 CRL-25 AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-3-T CRL-376-T CRL-2960-T AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-5-T CRL-17-T CRL-111-T AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-7 CRL-10 CRL-19 CRL-22 AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-25 CRL-39 CRL-31 CRL-27 AmericanPhotographics.com 360-844-5348 CRATER LAKE CRL-26 CRL-27 CRL-39 CRL-42 AmericanPhotographics.com 360-844-5348 PRODUCT: MAGNETS LUGGAGE TAGS POSTCARDS MAGNETS CODE: MAG LGT PST LUGGAGE TAGS POSTCARDS CRL-2711 CRL-119 CRL-6 CRL-169 AmericanPhotographics.com 360-844-5348 PRODUCT: MAGNETS LUGGAGE TAGS POSTCARDS MAGNETS CODE: MAG LGT PST LUGGAGE TAGS POSTCARDS CRL-199 CRL-215 CRL-378 CRL-2683 AmericanPhotographics.com 360-844-5348 PRODUCT: MAGNETS LUGGAGE TAGS POSTCARDS MAGNETS CODE: MAG LGT PST LUGGAGE TAGS POSTCARDS CRL-MAG-4-T CRL-MAC-376-T CRL-MAC-2695 AmericanPhotographics.com 360-844-5348 PRODUCT: MAGNETS LUGGAGE TAGS POSTCARDS MAGNETS CODE: MAG LGT PST LUGGAGE TAGS POSTCARDS CRL-MAG-2887-T CRL-MAC-111-T
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  • CRATER LAKE REVEALED Crater Lake, Oregon
    U.S. Department of the Interior Prepared in cooperation with the Geologic Investigations Series I-2790 U.S. Geological Survey National Park Service Crater Lake, Oregon Around 500,000 people each year visit Crater Lake National Park in the Cascade Range of southern Oregon. Volcanic peaks, evergreen forests, and Crater Lake s incredibly blue water are the park s main attractions. Crater Lake partially fills the caldera that formed approximately 7,700 years ago by the eruption and subsequent collapse of a 12,000-foot volcano called Mount Mazama. The caldera-forming or climactic eruption of Mount Mazama drastically changed the landscape all around the volcano and spread a blanket of volcanic ash at least as far away as southern Canada. Prior to the climactic event, Mount Mazama had a 400,000 year history of cone building activity like that of other Cascade volcanoes such as Mount Shasta. Since the climactic eruption, there have been several less violent, smaller postcaldera eruptions within the caldera itself. However, relatively little was known about the specifics of these eruptions because their products were obscured beneath Crater Lake s surface. As the Crater Lake region is still potentially volcanically active, understanding past eruptive events is important to understanding future eruptions, which could threaten facilities and people at Crater Lake National Park and the major transportation corridor east of the Cascades. Recently, the lake bottom was mapped with a high-resolution multibeam echo sounder. The new bathymetric survey provides a 2m/pixel view of the lake floor from its deepest basins virtually to the shoreline.
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  • Crater Lake Institute
    National Park Service U.S. Department of the Interior Crater Lake Summer/Fall 2009 Reflections Visitor Guide More Than a Pretty Lake Look Inside! 2 ... Camping, Lodging, Food Exploring Your National Park 3 ... Ranger Programs People react in different ways to seeing Crater Lake for the first time. Some can’t help but 4 ... Hiking Trails laugh at the surreal sight of a round, blue, mountaintop lake. Others are moved to silence as 5 ... Park Map they try to take it all in. Still others are roused to ask questions, curious about the lake’s depth, color, origins, and features. But probably the most common response to seeing Crater Lake 6 ... Park Weather for the first time is to reach instinctively for a camera. So surprising and overwhelming is the 7 ... In the News: Black Bears beauty of Crater Lake that it causes many of us to start snapping away, almost involuntarily, as though compelled to capture proof that such a remarkable lake exists. 8 ... Recommended Reading No matter what your initial reaction, after gazing down at the water for a few minutes you might find yourself at a bit of a loss. Yes, Crater Lake is arrestingly attractive and incredibly photogenic, but is there anything to it beyond its stunning good looks? Is there more to the Welcome! lake—and to this park—than the thrill of the initial view? Is there anything to do here? Park Profile Thank you for visiting your national park! Thankfully, the answer is yes. From its fiery origins to its fascinating human history to its Crater Lake National Park protects the Here at Crater Lake, you’ll find opportuni- present-day volcanic features and old-growth forests, Crater Lake National Park possesses deepest lake in the United States.
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