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Haleakalā

Haleakalā 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 Haleakalā rather than just read about it. In short: Haleakalā (; Hawaiian: Hawaiian pronunciation: [ˈhɐlɛˈjɐkəˈlaː]), or the East Maui Volcano, is a massive, active shield volcano that forms more than 75% of the Hawaiian Island of Maui. The western 25% of the island is formed by another volcano, Mauna Kahalawai, also referred to as the West Maui Mountains.

Haleakalā — main illustration
Haleakalā — illustration

Key takeaways

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

Reference excerpt

Haleakalā (; Hawaiian: Hawaiian pronunciation: [ˈhɐlɛˈjɐkəˈlaː]), or the East Maui Volcano, is a massive, active shield volcano that forms more than 75% of the Hawaiian Island of Maui. The western 25% of the island is formed by another volcano, Mauna Kahalawai, also referred to as the West Maui Mountains. The tallest peak of Haleakalā ("house of the sun"), at 10,023 feet (3,055 m), is Puʻu ʻUlaʻula (Red Hill). From the summit one looks down into a massive depression some 11.25 mi (18.11 km) across, 3.2 mi (5.1 km) wide, and nearly 800 m (2,600 ft) deep. The surrounding walls are steep and the interior mostly barren-looking with a scattering of volcanic cones.

History Early Hawaiians applied the name Haleakalā ("house of the sun") to the general mountain. Haleakalā is also the name of a peak on the southwestern edge of Kaupō Gap. In Hawaiian folklore, the depression (crater) at the summit of Haleakalā was home to the grandmother of the demigod Māui. According to the legend, Māui's grandmother helped him capture the sun and force it to slow its journey across the sky in order to lengthen the day.

Geology Haleakalā started forming 2 million years ago and built a massive shield volcano along 3 rift zones that was once broken by a central caldera. Haleakalā is currently in the Rejuvenated Stage of Volcanism and has produced numerous eruptions in the last 30,000 years, including ten eruptions in the past 1,000 years and at least one in the last 400–600 years, making it the only active volcano on the island of Maui. This volcanic activity has been along two rift zones: the southwest and east. These two rift zones together form an arc that extends from La Perouse Bay on the southwest, through the Haleakalā Crater, and to Hāna to the east. The east rift zone continues under the ocean beyond the east coast of Maui as Haleakalā Ridge, making the combined rift zones one of the longest in the Hawaiian Islands chain. In its prime, Haleakalā may have reached a height of 12,000 feet (3,700 m) before water and wind erosion, and possibly glaciers, began to carve two large river valleys out of the rim. Eventually, these valleys formed gaps that merged at the volcano summit to create a crater-like basin. A third rift zone exists on a North/Northwest trend that hasn't seen any recent volcanic activity. Haleakalā, also known as East Maui Volcano, was previously thought to have last erupted around 1790, based largely on comparisons of maps made during the voyages of La Perouse and George Vancouver. In 1999, the U.S. Geological Survey published in a column that radiocarbon dating indicated that the last eruption was more likely to have taken place sometime between 1480 and 1600. These last flows from the southwest rift zone of Haleakalā make up the large lava deposits of the Ahihi Kina`u/La Perouse Bay area of South Maui. The Haleakalā crater is not volcanic in origin, as it formed when the headwalls of two large erosional valleys merged at the summit of the volcano. These valleys formed the two large gaps — Koʻolau on the north side and Kaupō on the south — on either side of the depression. Macdonald, Abbott, & Peterson state it this way:

Haleakalā is far smaller than many volcanic craters (calderas); there is an excellent chance that it is not extinct, but only dormant; and strictly speaking, it is not of volcanic origin, beyond the fact that it exists in a volcanic mountain.

Volcanic hazard

On the island of Hawaiʻi, lava-flow hazards are rated on a scale of one through nine with one being the zone of highest hazard and nine being the zone of lowest hazard. For example, the summits and rift zones of Kilauea and Mauna Loa volcanoes are rated Hazard Zone 1. Using this same scale, preliminary estimates of lava-flow hazard zones on Maui made in 1983 by the U.S. Geological Survey rated the summit and southwest rift zone of Haleakalā as Hazard Zone 3. The steep, downslope areas of the Kanaio and Kahikinui ahupuaʻa and the area north of Hana are rated as Hazard Zone 4. Other areas of Haleakalā are rated comparable to the lava-flow hazards of Mauna Kea and Kohala (Hazard Zones 7 through 9). These high hazard estimates for Haleakalā are based on the frequency of its eruptions. Haleakalā has erupted three times in approximately the last 900 years. By way of comparison, both Mauna Loa and Kilauea have erupted more than a dozen times each in the last 90 years. Hualalai has an eruption rate comparable to Haleakalā. All of Hualalai is rated as Hazard Zone 4. However, the frequency of eruption of a volcano is only one of the criteria on which hazards are based. The other important criterion is the lava flow coverage rate. Using the preliminary dates for Haleakalā flows, only 8.7 square miles (23 km2) of lava flows have been emplaced in the last 900 years. In comparison, approximately 43 square miles (110 km2) of Hualalai are covered with flows 900 years old or younger and approximately 104 square miles (270 km2) on Kilauea and 85 square miles (220 km2) on Mauna Loa are covered by lavas less than 200 years old. Thus, Haleakalā is a distant fourth in coverage rates. According to the United States Geological Survey Volcano Warning Scheme for the United States, the Volcano Alert Level for Haleakalā as of 3 June 2021 was "normal". A "Normal" status is used to designate typical volcanic activity in a background, non-eruptive phase.

Endangered species

Nēnē The nēnē bird is on the endangered species list. The bird was once on all the islands of Hawaii, but now it is only on the Island of Hawai’i, Maui, Moloka’i, and Kaua’i. Habitat loss, hunting, and the introduction of mammals caused the bird population to dwindle. Since 2010, only 2,000 birds were left. These birds were then kept in captivity to increase the population.

Silversword

Haleakalā silversword is a quintessential plant of Haleakalā since it grows nowhere else on Earth. Climate change has been threatening the population of this plant due to hotter temperatures and lower rainfall. The park service has erected fences to prevent damage from local herbivores and from visitors taking the plants as souvenirs.

… excerpt ends here. Continue reading the full article.

Illustrations

Haleakalā illustration
Haleakalā: Sunrise at Haleakalā
Sunrise at Haleakalā
Haleakalā: Haleakalā as seen looking northwest from Big Island, Hawaii, near Kawaihae, 85 kilometers (53 mi) away
Haleakalā as seen looking northwest from Big Island, Hawaii, near Kawaihae, 85 kilometers (53 mi) away
Haleakalā: Lava Flow Hazard map of Haleakalā. The Maui Hazard Zone numbers are two less than the equivalent Hawaiʻi Hazard Zone numbers.[9]
Lava Flow Hazard map of Haleakalā. The Maui Hazard Zone numbers are two less than the equivalent Hawaiʻi Hazard Zone numbers.[9]
Haleakalā: This rare species of Silversword is fragile and lives only upon the slopes of Haleakalā.
This rare species of Silversword is fragile and lives only upon the slopes of Haleakalā.

Worked examples

Example 1 — a first encounter with Haleakalā

Start with the simplest possible case. Write down what Haleakalā 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 Haleakalā 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 Haleakalā 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 Haleakalā

In research
Haleakalā 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 Haleakalā 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
Haleakalā is common in secondary-school and first-year university syllabi. It links to neighbouring topics Cenozoic Hawaii, Dormant volcanoes, Haleakalā National Park, so understanding it makes those chapters shorter.
In everyday life
Look for Haleakalā 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 Haleakalā in 20 minutes

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

Frequently asked questions

What is Haleakalā in simple terms?

Haleakalā (; Hawaiian: Hawaiian pronunciation: [ˈhɐlɛˈjɐkəˈlaː]), or the East Maui Volcano, is a massive, active shield volcano that forms more than 75% of the Hawaiian Island of Maui. The western 25% of the island is formed by another volcano, Mauna Kahalawai, also referred to as the West Maui Mou…

Why does Haleakalā 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 Haleakalā?

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 Haleakalā.

Tags

  • Cenozoic Hawaii
  • Dormant volcanoes
  • Haleakalā National Park
  • Highest points of United States national parks
  • Holocene Oceania
  • Holocene shield volcanoes
  • Hotspot volcanoes
  • Landforms of Maui
  • Mountains of Hawaii
  • Pleistocene Oceania
  • Pleistocene shield volcanoes
  • Polygenetic shield volcanoes

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