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Three Fingered Jack

Three Fingered Jack 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 Three Fingered Jack rather than just read about it. In short: Three Fingered Jack is a summit of a shield volcano of the Cascade Range in the U.S. state of Oregon. Formed during the Pleistocene epoch, the mountain consists mainly of basaltic andesite lava and was heavily glaciated in the past.

Three Fingered Jack — main illustration
Three Fingered Jack — illustration

Key takeaways

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

Reference excerpt

Three Fingered Jack is a summit of a shield volcano of the Cascade Range in the U.S. state of Oregon. Formed during the Pleistocene epoch, the mountain consists mainly of basaltic andesite lava and was heavily glaciated in the past. While other Oregon volcanoes that were heavily glaciated—such as Mount Washington and Mount Thielsen—display eroded volcanic necks, Three Fingered Jack's present summit is a comparatively narrow ridge of loose tephra supported by a dike only 10 feet (3.0 m) thick on a generally north–south axis. Glaciation exposed radiating dikes and plugs that support this summit. The volcano has long been inactive and is highly eroded. Three Fingered Jack has diverse flora, fauna, and fungi. The Molala people, one of the indigenous groups in the northwestern United States, historically inhabited the area around the volcano. Not much is known about Molala culture, other than that the group fished for salmon and collected berries, fruits, obsidian, and dried herbs. David Douglas was the first person of non-indigenous descent to reach the area in 1825, followed by Peter Skene Ogden the following year. The first group to ascend the volcano reached its summit in September 1923. Three Fingered Jack can still be climbed, but climbers can require rescue after becoming disoriented in low visibility conditions.

Geography Three Fingered Jack lies in the U.S. state of Oregon, in Linn and Jefferson counties. It has a volume of 2.4 cubic miles (10 km3) and a summit elevation of 7,844 feet (2,391 m), with a proximal topographic relief of 1,300 feet (400 m) and a draping relief of 4,600 feet (1,400 m). Its jagged edifice rises between Mount Jefferson and the Three Sisters volcanic complex. Three Fingered Jack lies within the Mount Jefferson Wilderness and is only accessible on foot by trails such as the Pacific Crest Trail. Located about 20 miles (32 km) northwest of the city of Sisters, it is a prominent landmark in the area.

Physical geography

Lateral and terminal moraines formed on Three Fingered Jack during the last major advance of glacial ice in the area during the Wisconsin glaciation, along with glacial striations, altered vegetation patterns, and lithologies that suggest glacial transport of material. Jack Glacier (unofficially-named) is the sole glacier remaining on the volcano, located in a shaded cirque on the northeast side. The glacier resides at an unusually low altitude for the central Oregon Cascades it is protected by tall ridges to the south and west. Jack Glacier has an area of 2.5 acres (1.0 ha), though historically it has reached estimated areas of up to 32 acres (13 ha). It is likely stagnant. During the Little Ice Age, which spanned roughly 1350 to 1850, the glacier produced moraines with heights close to 200 feet (61 m), which are dotted with 1⁄2 to 1 foot (0.15 to 0.30 m) of ash from the Sand Mountain cinder cone chain and 1 foot (0.30 m) of ash from the Blue Lake Crater cinder cone. The moraine for Jack Glacier dammed a lake with a volume of 940,000 cubic feet (26,500 m3), a surface area of 65,900 square feet (6,120 m2), and a maximum depth of 26 feet (8 m). This lake was documented in 1937, although it did not appear on United States Geological Survey topographic maps made during the 1920s. The lake sits precariously; moraines on the volcano are steep, unstable, and populated with boulders. Before September 1960, there was a partial breach of this moraine-dammed lake that covered an area of 12,000 square metres (3.0 acres) near the moraine's base. Since 1960, there have been at least three incidents in which moraine-dammed lakes on the volcano have caused floods down the slopes, including a significant flood and debris flow in 2012. Local soil is thin, and it has been buried by a layer of weathered Holocene tephra from Three Fingered Jack, which has a maximum thickness of 3.3 feet (1 m).

Ecology

Douglas fir, Alpine fir, blue spruce, mountain hemlock, and bear grass can be found along the volcano and its hiking trails. Cascade parsley fern grows on Three Fingered Jack between elevations of 6,500 to 7,000 feet (2,000 to 2,100 m). There are also mountain goats in the surrounding wilderness area. Carnivorous animals in the surrounding area include American black bears, coyotes, cougars, red foxes, raccoons, American martens, stoats (also known as ermines), long-tailed weasels, American minks, North American river otters, and bobcats. Deer species include Roosevelt elk, black-tailed deer, and mule deer; insectivores include vagrant shrews, American water shrews, and coast moles. Bats at Jefferson include little brown bats and silver-haired bats, and American pikas and snowshoe hares are also present. Rodents such as yellow-bellied marmots, mountain beavers, yellow-pine chipmunks, Townsend's chipmunks, golden-mantled ground squirrels, western gray squirrels, Douglas squirrels, mountain pocket gophers, North American beavers, deer mice, bushy-tailed woodrats, water voles, Pacific jumping mice, and North American porcupines are present. Birds nearby include mallards, American goshawks, sharp-shinned hawks, red-tailed hawks, dusky grouse, grey partridges, killdeer, spotted sandpipers, California gulls, band-tailed pigeons, great horned owls, mountain pygmy owls, common nighthawks, rufous hummingbirds, Northern flickers, pileated woodpeckers, yellow-bellied sapsuckers, hairy woodpeckers, and white-headed woodpeckers. Other bird species found in the area consist of American three-toed woodpeckers, willow flycatchers, olive-sided flycatchers, tree swallows, Canada jays, Steller's jays, common ravens, Clark's nutcrackers, black-capped chickadees, mountain chickadees, chestnut-backed chickadees, red-breasted nuthatches, pygmy nuthatches, brown creepers, American dippers, wrens, American robins, varied thrushes, hermit thrushes, Townsend's solitaires, golden-crowned kinglets, ruby-crowned kinglets, American pipits, blue-headed vireos, western tanagers, Cassin's finches, gray-crowned rosy finches, pine siskins, red crossbills, green-tailed towhees, dark-eyed juncos, white-crowned sparrows, golden-crowned sparrows, fox sparrows, and Lincoln's sparrows. Long-toed salamanders, California giant salamanders, rough-skinned newts, tailed frogs, western toads, Pacific tree frogs, northern red-legged frogs, Oregon spotted frogs, pygmy short-horned lizards, common garter snakes, and northwestern garter snakes make up some of the amphibious and reptilian animals in the vicinity.

… excerpt ends here. Continue reading the full article.

Illustrations

Three Fingered Jack illustration
Three Fingered Jack: The moraine-dammed lake in summer
The moraine-dammed lake in summer
Three Fingered Jack: A herd of mountain goats seen on the flank of Three Fingered Jack
A herd of mountain goats seen on the flank of Three Fingered Jack
Three Fingered Jack: Three Fingered Jack as seen from Santiam Lake
Three Fingered Jack as seen from Santiam Lake
Three Fingered Jack: Three Fingered Jack has a desiccated, jagged appearance.
Three Fingered Jack has a desiccated, jagged appearance.

Worked examples

Example 1 — a first encounter with Three Fingered Jack

Start with the simplest possible case. Write down what Three Fingered Jack 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 Three Fingered Jack 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 Three Fingered Jack 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 Three Fingered Jack

In research
Three Fingered Jack 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 Three Fingered Jack 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
Three Fingered Jack is common in secondary-school and first-year university syllabi. It links to neighbouring topics Cascade Range, Cascade Volcanoes, Deschutes National Forest, so understanding it makes those chapters shorter.
In everyday life
Look for Three Fingered Jack 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 Three Fingered Jack in 20 minutes

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

Frequently asked questions

What is Three Fingered Jack in simple terms?

Three Fingered Jack is a summit of a shield volcano of the Cascade Range in the U.S. state of Oregon. Formed during the Pleistocene epoch, the mountain consists mainly of basaltic andesite lava and was heavily glaciated in the past.

Why does Three Fingered Jack 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 Three Fingered Jack?

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 Three Fingered Jack.

Tags

  • Cascade Range
  • Cascade Volcanoes
  • Deschutes National Forest
  • Extinct volcanoes of the United States
  • Landforms of Jefferson County, Oregon
  • Landmarks in Oregon
  • Mountains of Linn County, Oregon
  • Mountains of Oregon
  • Pleistocene shield volcanoes
  • Polygenetic shield volcanoes
  • Quaternary Oregon
  • Shield volcanoes of the United States

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