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Mount Blackburn

Mount Blackburn 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 Mount Blackburn rather than just read about it. In short: Mount Blackburn (Ahtna: K’ats’i Tl’aadi) is the highest peak in the Wrangell Mountains of Alaska in the United States. It is the fifth-highest peak in the United States and the twelfth-highest peak in North America.

Mount Blackburn — main illustration
Mount Blackburn — illustration

Key takeaways

  • Mount Blackburn 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 Mount Blackburn to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Mount Blackburn from memory before moving on to harder problems.

Reference excerpt

Mount Blackburn (Ahtna: K’ats’i Tl’aadi) is the highest peak in the Wrangell Mountains of Alaska in the United States. It is the fifth-highest peak in the United States and the twelfth-highest peak in North America. The mountain is an old, eroded shield volcano, the second-highest volcano in the U.S. behind Mount Bona and the fifth-highest in North America. It was named in 1885 by Lt. Henry T. Allen of the U.S. Army after Joseph Clay Stiles Blackburn, a U.S. senator from Kentucky. It is located in the heart of Wrangell – St. Elias National Park, the largest national park in the country.

Description The mountain's massif is covered almost entirely by icefields and glaciers and is the principal source of ice for the Kennicott Glacier, which flows southeast over 20 miles (32 km) to just above the town of McCarthy. The mountain also contributes a large volume of ice to the north-flowing Nabesna Glacier and the Kuskulana Glacier system. Mount Blackburn is a large, dramatic peak, with great local relief and independence from higher peaks. Its west face drops over 11,000 ft (3,350 m) to the Kuskulana Glacier in less than 4 horizontal miles (6.4 km). Its other faces drop 8,000–10,000 ft (2,440–3,050 m), all in less than 8 miles (13 km). The toe of the Kuskulana Glacier, less than 12 miles (19 km) from the summit, lies at an elevation of 2,400 ft (730 m), giving a rise of 14,000 ft (4,270 m). While these figures speak to the peak's relief, one measure of its independence is that it is the 50th-most topographically prominent peak in the world. The western of Blackburn's two summits is the mountain's highest point, a fact that was not understood until the 1960s when new USGS maps were published. The first ascent of the west peak, and hence Mount Blackburn, was done on May 30, 1958, by Bruce Gilbert, Dick Wahlstrom, Hans Gmoser, Adolf Bitterlich, and Leon Blumer via the North (also called the Northwest) Ridge. This team made the first ascent of Blackburn but did not even know it at the time due to the incorrect identification of the highest point. Blumer's article in the 1959 American Alpine Journal is titled "Mount Blackburn – Second Ascent."

Other subfeatures Kennedy Peak, or East Blackburn, 16,286 ft (4,964 m), is the eastern summit and was originally thought to be the highest point. The first ascent of this summit was made in 1912 by Dora Keen and George Handy via the Kennicott Glacier (on the south side of the mountain) and East Face. This heady exploit was ahead of its time. Dora Keen, driven by a deep desire for the climb, solicited miners from the nearby Kennecott Copper Mines, and forged a route up the heavily crevassed East Face to the East Peak, but did not traverse over to the West Peak. Keen went on to write a famous article for the Saturday Evening Post titled, "First up Mount Blackburn." In 1912, Keen and Handy thought they were on Blackburn's highest point. Keen's summit is recognized as the first summit of an Alaskan peak by a woman.

Geology Mount Blackburn represents the heavily eroded core of a shield volcano. Because it is shrouded in permanent ice, its internal structure cannot be determined. It is believed to have a summit caldera, greatly modified by glaciation. The oldest rocks in the area are granites, about 4.2 million years old, representing an intrusive mass. The majority of the mountain is 3.4 million year old granite, intruding between andesite flows. From this it is inferred that a caldera collapse took place between 4.2 and 3.4 million years ago, after which activity ceased.

Climbing Today's standard route on the peak is the 1958 ascent route, the North (or Northwest) Ridge, which is approached from the Nabesna Glacier, on the north side of the mountain, opposite from Keen and Hardy's route. The route starts from an airstrip on the glacier at an altitude of 7,200 feet (2,200 m). It is a moderate climb by Alaskan standards (Alaska Grade 2).

Gallery

See also

List of mountain peaks of North America List of mountain peaks of the United States List of mountain peaks of Alaska List of the highest major summits of the United States List of the most prominent summits of the United States List of the most isolated major summits of the United States List of volcanoes in the United States

References and notes

Notes

References

Sources Wood, Michael; Coombs, Colby (2001). Alaska: A Climbing Guide. Mountaineers Books. ISBN 0-89886-724-X. Winkler, Gary R. (2000). A Geologic Guide to Wrangell—Saint Elias National Park and Preserve, Alaska: A Tectonic Collage of Northbound Terranes. USGS Professional Paper 1616. ISBN 0-607-92676-7. Richter, Donald H.; Preller, Cindi C.; Labay, Keith A.; Shew, Nora B. (2006). Geologic Map of the Wrangell-Saint Elias National Park and Preserve, Alaska. USGS Scientific Investigations Map 2877.

External links

Illustrations

Mount Blackburn illustration
Mount Blackburn illustration
Mount Blackburn illustration
Mount Blackburn illustration

Worked examples

Example 1 — a first encounter with Mount Blackburn

Start with the simplest possible case. Write down what Mount Blackburn 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 Mount Blackburn 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 Mount Blackburn 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 Mount Blackburn

In research
Mount Blackburn 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 Mount Blackburn 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
Mount Blackburn is common in secondary-school and first-year university syllabi. It links to neighbouring topics Four-thousanders of the United States, Landforms of Copper River Census Area, Alaska, Mountains of Unorganized Borough, Alaska, so understanding it makes those chapters shorter.
In everyday life
Look for Mount Blackburn 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 Mount Blackburn in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Mount Blackburn 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 Mount Blackburn out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Mount Blackburn in simple terms?

Mount Blackburn (Ahtna: K’ats’i Tl’aadi) is the highest peak in the Wrangell Mountains of Alaska in the United States. It is the fifth-highest peak in the United States and the twelfth-highest peak in North America.

Why does Mount Blackburn 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 Mount Blackburn?

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 Mount Blackburn.

Tags

  • Four-thousanders of the United States
  • Landforms of Copper River Census Area, Alaska
  • Mountains of Unorganized Borough, Alaska
  • Pliocene United States
  • Shield volcanoes of the United States
  • Subduction volcanoes
  • Volcanoes of Alaska
  • Volcanoes of Unorganized Borough, Alaska
  • Wrangell Mountains
  • Wrangell–St. Elias National Park and Preserve

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