MATURANGO MUSEUM

RIDGECREST, CA

Yellow Pepperweed Seen near Trona, California. West of Death Valley National Park.
Yellow Pepperweed Credit: string_bass_dave

The Maturango Museum in Ridgecrest, California, is a local museum that highlights the cultural and natural history of the Indian Wells Valley region. The museum was founded in 1972, and since then has been dedicated to preserving and interpreting the rich cultural heritage of the area. The museum’s permanent collection includes artifacts from local Native American tribes, including the Shoshone, Paiute, and Chemehuevi, as well as materials from early settlers of the area. The museum also features a variety of rotating exhibits of art and artifacts from around the world.

The Maturango Museum’s educational programming includes a variety of lectures, workshops, and special events. The museum also offers a Discovery Room for visitors of all ages to explore and learn about the natural and cultural history of the area. Additionally, the museum offers guided tours of the facility and its exhibits.

The museum is open daily from 10am to 4pm, except on major holidays. Admission is free, although donations are welcome. The Maturango Museum also has an online store where visitors can purchase items such as books, jewelry, and other items related to the museum.

MATURANGO MUSEUM is a Uncategorized or General Museum in RIDGECREST CA. US MID #8400602607

The museum is classed as GMU (Uncategorized or General Museums). It comes under American Alliance of Museums (AAM) region: Western (Alaska, Arizona, California, Hawaii, Idaho, Nevada, Oregon, Utah, Washington). Total revenue from most recent IRS 990 Form: $ 508,624 from tax period 201212 (YYYYMM).

Yellow Pepperweed Seen near Trona, California. West of Death Valley National Park.
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>
Wander to Trona Pinnacles A Death Valley trip to visit the ephemeral Lake Manly ended up cut short due to mechanical issues with the Jeep that prevented me from making it over the pass, but a few roadside vistas and a pitstop at Trona Pinnacles saved the day. The Trona Pinnacles are a unique geological features in the California Desert Conservation Area. The unusual landscape consists of more than 500 tufa spires, some as high as 140 feet, rising from the bed of the Searles Dry Lake basin. The pinnacles vary in size and shape from short and squat to tall and thin, and are composed primarily of calcium carbonate (tufa). The Trona Pinnacles have been featured in many commercials, films, and still-photo shoots. The Trona Pinnacles were designated a National Natural Landmark by the U.S. Department of the Interior in 1968 to preserve one of North America’s most outstanding examples of tufa tower formation. Rising from the bottom of what was once an ancient lakebed, the Trona Pinnacles represent one of the most unique geologic landscapes in the California Desert. Over 500 of these tufa (or calcium carbonate spires) are spread out over a 14 square mile area across the Searles Lake basin. These features range in size from small-coral like boulders to several that top out at over 140 feet tall. The Pinnacles were formed between 10,000 and 100,000 years ago when Searles Lake formed a link in a chain of interconnected lakes flowing from the Owens Valley to Death Valley. At one point during the Pleistocene, the area was under 640 feet of water. Description from the Bureau of Land Management <a href="https://www.blm.gov/visit/trona-pinnacles" rel="noreferrer nofollow">www.blm.gov/visit/trona-pinnacles</a>

Contact MATURANGO MUSEUM

MATURANGO MUSEUM OF INDIAN WELLS VALLEY
100 E LAS FLORES AVE
RIDGECREST
CA
93555-3654

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MATURANGO MUSEUM Information

MID # 8400602607
Name MATURANGO MUSEUM OF INDIAN WELLS VALLEY
Alternate Name MATURANGO MUSEUM
Classification Uncategorized or General Museums, , Western
Federal Employer Identification Number (EIN) 952232881
NTEECC A50
Tax period of the latest return filed (YYYYMM) 201212
INCOME 617,815
REVENUE 508,624
LAT/LONG 35.627305, -117.667002
CODES FIPS State Code: 06
FIPS County Code: 029
US Census Tract: 005300
US Census Block: 2127