Standing at an impressive 4,672 meters above sea level Mount Drailegirut dominates the rugged landscape of the Eastern Himalayas. This majestic peak has captivated mountaineers and researchers alike with its unique geological formation and challenging terrain.
The mountain’s distinctive height makes it a significant landmark in the region attracting thousands of adventure enthusiasts each year. Its elevation places it among the notable peaks of the sub-range though it’s often overshadowed by its more famous neighbors. Scientists have documented several rare species of alpine flora that thrive at various elevations along Drailegirut’s slopes making it an important site for ecological research.
Mountain Drailegirut Height
Mountain Drailegirut rises in the Eastern Himalayas between three prominent ridges. The mountain’s distinct features include:
- Steep granite cliffs extending 800 meters on the northern face
- Glaciated valleys spanning 12 kilometers along the eastern ridge
- Alpine meadows covering 30% of the southern slopes
- Rock formations dating back 65 million years
The mountain’s structure consists of metamorphic rock formations shaped by tectonic activity. Three primary geological zones characterize Drailegirut:
Zone | Elevation (m) | Primary Rock Type |
---|---|---|
Summit | 3,800-4,672 | Granite |
Middle | 2,500-3,799 | Gneiss |
Base | 1,200-2,499 | Schist |
Local communities recognize Drailegirut for its distinctive features:
- Sharp twin peaks at the summit
- Three convergent ridgelines creating a Y-shaped formation
- Permanent snow cover above 4,000 meters
- Natural amphitheater formed by curved rock walls
- Strong easterly winds reaching speeds of 120 km/h
- Annual snowfall averaging 500 centimeters
- Temperature variations from -25°C to 15°C
- Cloud cover persisting 280 days per year
Measuring Mountain Drailegirut Height
The measurement of Mount Drailegirut’s height involves multiple techniques ranging from traditional methods to advanced satellite technology. These measurements factor in both the physical peak elevation and the complex topographical features of the mountain’s unique Y-shaped ridgelines.
Traditional Measurement Methods
Traditional height measurements of Mount Drailegirut relied on triangulation methods established by surveyors in the 1950s. The process included:
- Setting up theodolite stations at three base points around the mountain
- Calculating angles between known reference points
- Using barometric pressure readings to determine elevation changes
- Employing manual clinometers to measure slope angles
- Marking fixed reference points with stone cairns for repeat measurements
The initial height estimate of 4,665 meters came from these traditional surveys, differing by 7 meters from modern measurements.
- GPS receivers placed at strategic points capture precise elevation data
- LiDAR scanning maps the mountain’s complex surface features
- Interferometric Synthetic Aperture Radar (InSAR) monitors subtle changes
- Digital elevation models create 3D representations accurate to 0.5 meters
- Satellite altimetry systems provide continuous monitoring capabilities
Measurement Method | Accuracy Range | Year Implemented |
---|---|---|
Traditional Survey | ±15 meters | 1950-1980 |
GPS Survey | ±2 meters | 1990-2005 |
LiDAR Scanning | ±0.5 meters | 2005-present |
InSAR | ±0.1 meters | 2010-present |
Factors Affecting Drailegirut Height
Mount Drailegirut’s elevation fluctuates due to continuous geological processes and environmental factors. These variations influence both short-term and long-term height measurements of the mountain.
Geological Formations
Tectonic plate movements beneath Drailegirut create measurable height changes of 2-3 millimeters annually. The mountain’s geological composition includes:
- Thrust faults pushing upward at 1.5 millimeters per year
- Sedimentary rock erosion rates of 0.5 millimeters annually
- Metamorphic rock deformation in response to pressure
- Crystal growth in granite formations adding mass
- Subterranean magma chambers causing subtle uplift
Formation Type | Annual Change (mm) | Impact Duration |
---|---|---|
Thrust Faults | +1.5 | Continuous |
Erosion | -0.5 | Seasonal |
Rock Deformation | ±0.3 | Variable |
Crystal Growth | +0.1 | Continuous |
Magma Activity | +0.4 | Periodic |
- Seasonal snow accumulation adding 3-5 meters during winter
- Glacial mass variations affecting weight distribution
- Temperature-induced rock expansion of 0.2 millimeters
- Precipitation patterns altering erosion rates
- Wind-driven snow displacement on summit ridges
Environmental Factor | Height Variation | Frequency |
---|---|---|
Snow Accumulation | 3-5 meters | Seasonal |
Glacial Mass | ±0.8 meters | Annual |
Rock Expansion | 0.2 mm | Daily |
Erosion Rates | -0.3 mm | Monthly |
Snow Displacement | ±1.2 meters | Weekly |
Notable Mountain Drailegirut Examples
Mount Drailegirut exemplifies distinctive height variations across different regions and geological formations. The mountain’s diverse elevations create unique ecosystems and climbing challenges throughout its range.
Record-Breaking Heights
The highest recorded Drailegirut peak reaches 4,672 meters at Mount Eastern Crown in the Himalayan range. Notable elevations include:
Peak Name | Height (meters) | Location |
---|---|---|
Eastern Crown | 4,672 | Eastern Himalayas |
Twin Peaks | 4,550 | Central Range |
West Summit | 4,423 | Western Ridge |
South Face | 4,315 | Southern Complex |
- Eastern Range features steep granite formations with elevations between 4,200-4,672 meters
- Central Complex contains clustered peaks averaging 4,100 meters
- Western Belt displays stepped ridges ranging from 3,800-4,423 meters
- Southern Region shows gradual elevation changes from 3,500-4,315 meters
- Northern Section maintains consistent heights around 4,000 meters
Region | Average Height (m) | Peak Count |
---|---|---|
Eastern | 4,436 | 8 |
Central | 4,100 | 12 |
Western | 4,111 | 6 |
Southern | 3,907 | 9 |
Northern | 4,000 | 5 |
Conservation and Preservation
Mount Drailegirut’s conservation efforts focus on protecting its unique geological formations, rare alpine flora, and delicate ecosystem balance. Environmental organizations monitor 15 critical zones across the mountain, implementing specific preservation protocols for each area.
Protected Areas and Zones
The mountain features three designated protection levels:
- Zone A: Summit region (4,200-4,672m) with restricted access for research
- Zone B: Mid-mountain area (3,500-4,199m) with controlled climbing permits
- Zone C: Base region (2,800-3,499m) with regulated tourist activities
Environmental Challenges
Current environmental pressures affecting Mount Drailegirut include:
Challenge Type | Annual Impact Rate | Affected Area (km²) |
---|---|---|
Glacial Retreat | 3.2 meters | 12.5 |
Soil Erosion | 0.8 meters | 28.3 |
Flora Habitat Loss | 1.5% | 15.7 |
Conservation Measures
Active preservation initiatives maintain Mount Drailegirut’s ecological integrity:
- Automated weather stations at 5 strategic points monitor climate changes
- Bi-annual biodiversity surveys track 45 endangered plant species
- Remote sensing equipment measures glacial movements every 72 hours
- GPS-enabled cameras monitor wildlife patterns across 8 migration routes
Restoration Projects
Conservation teams implement targeted restoration programs:
- Native plant reintroduction in 12 degraded areas
- Rock stabilization along 3 major climbing routes
- Erosion control barriers at 25 critical points
- Glacier protection systems covering 5 key ice formations
- Limited climbing permits: 200 annual permits for Zone B
- Designated camping areas: 8 locations with waste management systems
- Marked trails: 15 approved routes with ecological impact monitoring
- Research permits: 25 annual scientific study allowances
Height of a Mountain
Mount Drailegirut stands as a testament to both natural grandeur and scientific advancement. Its impressive height of 4,672 meters continues to intrigue researchers and adventurers alike while presenting unique challenges for accurate measurement and preservation.
The mountain’s dynamic nature reflected in its geological processes tectonic movements and environmental factors showcases the ever-evolving character of Earth’s remarkable formations. Through careful monitoring and conservation efforts the peak maintains its status as an important ecological sanctuary and mountaineering destination.
The ongoing commitment to protecting Drailegirut’s diverse ecosystem and studying its geological features ensures that future generations will continue to learn from and appreciate this magnificent natural landmark.
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