Haleakalā National Park Geography Quiz
Explore the geology and ecology of Haleakalā, focusing on its shield volcano structure and distinct elevation zones (10 questions).
Haleakalā National Park Geography Quiz: Quick Study Notes
Haleakalā National Park on Maui, Hawaiʻi, is a geological marvel dominated by the dormant Haleakalā shield volcano. This quiz explores its unique formation, from its gentle slopes created by effusive lava flows to the impressive ‘crater’ shaped by erosion. Discover how distinct elevation zones, influenced by the orographic effect, foster diverse ecosystems and endemic species like the iconic Silversword.
Key Concepts
A broad, gently sloping volcano built by successive flows of fluid, basaltic lava.
Non-explosive eruptions characterized by the steady outflow of highly fluid lava, common for shield volcanoes.
Distinct ecological bands (e.g., coastal, rainforest, alpine desert) formed by changes in altitude, temperature, and rainfall.
A meteorological phenomenon where moist air forced over mountains cools, condenses (rain on windward side), and creates a dry rain shadow on the leeward side.
Key Takeaways
- Haleakalā is a massive, dormant shield volcano that forms the eastern part of Maui, Hawaiʻi.
- Shield volcanoes are characterized by their gentle slopes and wide bases, a result of highly fluid, basaltic lava flows.
- The summit of Haleakalā reaches an elevation of 10,023 feet (3,055 meters) above sea level.
- The vast depression at its summit, often called a “crater,” is primarily an erosional valley rather than a collapsed caldera.
- Haleakalā exhibits distinct elevation zones, each with unique climatic conditions and ecosystems, from coastal lowlands to an alpine summit.
- The orographic effect dramatically influences rainfall distribution, creating lush windward rainforests and arid leeward zones.
- Endemic species, such as the Haleakalā Silversword (‘Āhinahina), are specially adapted to these diverse elevation zones.
Frequently Asked Questions (FAQs)
What kind of volcano is Haleakalā?
Haleakalā is a massive shield volcano, known for its broad, gently sloping profile formed by highly fluid lava flows. It is currently considered dormant, meaning it is not actively erupting but could do so in the future.
How was the “crater” of Haleakalā formed?
Despite its common name, the “crater” of Haleakalā is not a true volcanic caldera formed by collapse. Instead, it is a vast erosional valley, sculpted over millennia by wind and water carving into the volcano’s summit and merging two large amphitheater-headed valleys.
What is the significance of Haleakalā’s elevation zones?
Haleakalā’s significant elevation, reaching over 10,000 feet, creates a dramatic range of climates and ecosystems. These distinct elevation zones, from humid tropical rainforests at lower elevations to arid alpine deserts at the summit, host unique and often endemic flora and fauna specially adapted to their specific conditions.
What is the orographic effect and how does it impact Haleakalā?
The orographic effect is a change in atmospheric conditions caused by the forced lifting of air over mountains. On Haleakalā, moist trade winds from the northeast rise, cool, and release heavy rainfall on the windward slopes, creating lush rainforests. Conversely, the leeward (southwestern) side receives much less moisture, resulting in a drier rain shadow and different vegetation.
Is Haleakalā still active?
Haleakalā is classified as a dormant volcano. While it is not currently erupting, it is considered active by geologists and is capable of erupting again. Its last eruptions are estimated to have occurred relatively recently, between 200 and 500 years ago, indicating it is not extinct.

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