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Lava Butte

Lava Butte is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Lava Butte rather than just read about it. In short: Lava Butte is a cinder cone in central Oregon, United States, just west of U.S. Route 97 between the towns of Bend, and Sunriver in Deschutes County.

Lava Butte — main illustration
Lava Butte — illustration

Key takeaways

  • Lava Butte belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Lava Butte to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Lava Butte from memory before moving on to harder problems.

Reference excerpt

Lava Butte is a cinder cone in central Oregon, United States, just west of U.S. Route 97 between the towns of Bend, and Sunriver in Deschutes County. It is part of a system of small cinder cones on the northwest flank of Newberry Volcano, a massive shield volcano which rises to the southeast. The cinder cone is capped by a crater which extends about 60 feet (20 m) deep beneath its south rim, and 160 feet (50 m) deep from the 5,020-foot (1,530 m) summit on its north side. Lava Butte is part of the Newberry National Volcanic Monument.

Volcanic history

Like the other cinder cones in the area, Lava Butte only experienced a single eruption, dated by geologists in 1977 to 6,150 carbon-14 years, equivalent to about 7,000 years ago. The eruption began with a fissure spewing hot cinders to form the cone. In the next phase, a river of hot basalt flowed from the base of the small volcano to cover a large area to the west with a lava flow which remains largely free of vegetation. The lava flows reached the Deschutes River about 2.5 miles (4.0 km) to the west of the cone, burying its former channel under over 100 feet (30 m) of lava and damming the river to form a lake, known as Lake Benham. The river eventually overflowed the lava dam and eroded down into it, draining the lake and forming Benham Falls. Geologists estimate that 90% of the magma erupted as lava flows, 9% as scoria which forms the cone, and 1% as volcanic ash which forms a thin layer extending to the north.

Human history

The early history of Lava Butte is not known, but it is assumed that Native Americans observed the eruptions and later ascended the prominent new landmark. White settlers arriving in the 1800s also noted the landmark. In 1903, I.C. Russell was the first geologist to study the butte and speculated that it erupted as recently as 150 years ago. Dr. Howel Williams estimated it to be much older, but incorrectly at 1,000 years old. In September 1914, Lava Butte "erupted" when the Bend Chamber of Commerce simulated an eruption to surprise a visiting Portland group. In 1925, USGS geologist Harold Stearns studied the Newberry area and recognized the fissure system which extends from Lava Butte to East Lake within Newberry Caldera. Sometime after 1901, the Great Northern Railway was extended south through the area. The construction crew built the rail line directly through the ʻAʻā lava flow of Lava Butte.

The cinder cone was also exploited to some extent for its economic value. In June 1926, a quarry was developed in the fault scarp east of Lava Butte as a source for paving material for the first The Dalles-California Highway (later U.S. Route 97). In November 1929, cinders from Lava Butte were shipped to Longview, Washington, to be used in construction of Longview Bridge across Columbia River. A United States Forest Service fire lookout tower was built on the summit in 1931, and in early 1933 a steep, single-lane road was constructed spiraling up to the summit. In February of that year, the local Skyliners ski club proposed a ski jump on Lava Butte, but it was never built. In June 1946, widening of the road up Lava Butte to two lanes was completed, along with constructing two small parking lots at the summit. The road was later paved in July 1950. The original lookout was replaced with a larger one in 1957, which was subsequently enlarged in 1962 to accommodate a small visitor center and museum on the first floor. In 1998 this was replaced with a new lookout built in the original L-4 style of 1931. In July 1966, twenty-two astronauts trained in Central Oregon for the upcoming Moon landings, at sites including Lava Butte, Lava River Cave, and Newberry Crater. In May 1967 the U.S. Forest Service created the 8,983 acres (3,635 ha) Lava Butte Geological Area to protect the cinder cone, with plans for recreational and interpretive development. Construction of the Lava Lands Visitor Center located just south of the cone began in April 1969 and it was finally dedicated in September 1975. In November 1990, Newberry National Volcanic Monument was created encompassing Newberry Crater, Lava Cast Forest Geological Area, Lava River Cave, and the Lava Butte Geological Area. From early May to mid October, a shuttle transports visitors up Red Cinder Road from the Lava Lands Visitor Center to the lookout on Lava Butte. Hiking up Red Cinder Road is a year-round option. A scenic rim trail around the top of Lava Butte is 0.35 miles (0.56 km) long.

References

External links

"Newberry National Volcanic Monument". US Forest Service. Archived from the original on June 10, 2010. Retrieved April 1, 2008. "Architectural drawing of 1957 Lava Butte Lookout Tower" (PDF). US Forest Service. Retrieved April 1, 2008. "Map of Lava Butte, Deschutes County, Oregon" (PDF). oregongeology.org. Retrieved May 31, 2018.

Illustrations

Lava Butte illustration
Lava Butte: Visible from the top of Lava Butte is the black lava flow leading to Route 97.
Visible from the top of Lava Butte is the black lava flow leading to Route 97.
Lava Butte: Lava Butte from the south
Lava Butte from the south
Lava Butte: Sign at the summit of the butte
Sign at the summit of the butte

Worked examples

Example 1 — a first encounter with Lava Butte

Start with the simplest possible case. Write down what Lava Butte claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Lava Butte before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Lava Butte ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Lava Butte

In research
Lava Butte appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Lava Butte in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Lava Butte is common in secondary-school and first-year university syllabi. It links to neighbouring topics Buttes of Oregon, Cascade Volcanoes, Cinder cones of the United States, so understanding it makes those chapters shorter.
In everyday life
Look for Lava Butte outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

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How to study Lava Butte in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Lava Butte means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Lava Butte out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Lava Butte in simple terms?

Lava Butte is a cinder cone in central Oregon, United States, just west of U.S. Route 97 between the towns of Bend, and Sunriver in Deschutes County.

Why does Lava Butte matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Lava Butte?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Lava Butte.

Tags

  • Buttes of Oregon
  • Cascade Volcanoes
  • Cinder cones of the United States
  • Holocene cinder cones
  • Mountains of Deschutes County, Oregon
  • Mountains of Oregon
  • Newberry National Volcanic Monument
  • Quaternary Oregon
  • Subduction volcanoes
  • Volcanoes of Deschutes County, Oregon
  • Volcanoes of Oregon

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