Terms and Definitions for 3.1 External. Based on Te Kura GYO3004 and GYO3005
Plate tectonics
Scientific theory that describes the large-scale motion of Earth's lithosphere (crust), which is divided into several plates that float on the semi-fluid asthenosphere
Volcanism
The process by which magma, gas, and ash erupt onto the Earth's surface through volcanoes, creating new landforms and releasing pressure from the Earth's interior
Pyroclastic
Fragments of rock and debris from a volcanic eruption
Pyroclastic eruption
A rapid and explosive volcanic eruption that releases hot ash, rocks, and gases into the atmosphere at high speeds
Basic magma
Has low silica content and is less viscous, allowing gases to escape easily. It often leads to gentle volcanic eruptions
Where can basic magma be found in NZ?
Auckland and Northland
Acidic magma
Has high silica content, making it viscous with explosive eruptions. It forms light-colored rocks like rhyolite
Where can acidic magma be found in NZ?
Taupo-Rotorua volcanic zone; Taupo to Bay of Plenty
Intermediate magma
Has a silica content between that of basaltic and rhyolitic magma
Where can intermediate magma be found in NZ?
Taranaki and Tongariro regions
Composite cone
A volcano formed by alternating layers of lava flows and pyroclastic material, such as ash and volcanic rocks. It has a steep profile and can erupt explosively. Formed during andesitic eruptions. Example: Ruapehu
Shield volcano
A broad, gently sloping volcano characterized by flowing lava and built from many eruptions. Example: Rangitoto Island
Caldera
A large volcanic crater formed by the collapse of a volcano after an eruption, often filled with water. Example: Lake Taupo
Tephra
Fragments ejected during a volcanic eruption, including ash, lapilli, and bombs. Vary in size and composition, impacting landscapes and air quality
Hot springs
Natural bodies of water heated geothermally by the Earth's crust. They are formed when groundwater comes into contact with hot rocks below the surface, heating the water and bringing it back to the surface in the form of a spring. Example: Ketetahi Springs
Fumarole
An opening in or near a volcano, emitting steam and gases like sulfur dioxide. It results from the heating of groundwater
Sills
Horizontal igneous rock formations that form when magma intrudes between layers of existing rock and solidifies underground
Dykes
Vertical sheets of igneous rock that cut across the layers of pre-existing rock in the Earth's crust, formed by the intrusion of magma
Explosion crater
A bowl-shaped depression formed by the explosion of a volcanic vent, often filled with water or lava
Fault lines
Fractures in Earth's crust where rocks on either side have moved relative to each other. They are responsible for earthquakes due to the release of built-up stress
Fire-fountaining
Volcanic eruption where lava is ejected into the air, forming fountains of molten rock
Scoria cone
A steep-sided volcanic cone made of fragmented volcanic rock, forming from explosive eruptions of gas-rich magma
Height of Mt. Tongariro
1964m
Height of Mt. Ngauruhoe
2291m
Height of Mt. Ruapehu
2797m
Lahar
A fast-moving volcanic mudflow consisting of a mixture of volcanic debris, water, and mud
How do crater lakes make volcanoes more dangerous?
Crater lakes can cause explosive eruptions when heated by magma, leading to sudden releases of gas and ash
How do snowfields make volcanoes more dangerous?
Snowfields on volcanoes can melt rapidly during an eruption, causing lahars that can travel quickly down the slopes
Tongariro, Ruapehu, and Ngauruhoe are examples of ________ volcanoes
Andesite
Taupo is an example of a ________ volcano
Rhyolite
The Pacific - Australian plate margin is an example of a _______ margin
Collsion/subduction
At divergent plate margins, the plates ________
Move apart
At transform plate margins, the plates _________
Slide past each other
At collision plate margins, the plates __________
Collide; converge; subduct; move towards each other
Geographic environment
Refers to the physical surroundings of an area, including landforms, climate, vegetation, and natural resources
Natural features
Landscape features (or phenomena) that are a result of natural processes
Processes
A series of actions or events that shape and change environments
Location
Where features are sited
Spatial variation
Differences or changes in characteristics across different locations or areas
Temporal variation
Refers to changes or fluctuations that occur over time in a particular phenomenon or system
Dispersal
When the effects of a process are large-scale and affect a large area
Concentrated
When the effects of a process are localised an affect a small area
Age of Mt. Tongariro
275,000 years
Age of Mt. Ngauruhoe
2,500 years
Age of Mt. Ruapehu
250,000 years
When was Ruapehu’s last large eruption?
1995-96
When was the last eruption of the Taupo volcano?
232 AD
When was the last eruption of Mt. Ngauruhoe?
1975
Average annual rainfall at Chateau Tongariro (1097m asl)
2754mm
Average annual rainfall at Ohakune (820m asl)
1412mm
Average annual rainfall at Waiouru (607m asl)
1081mm
Adiabatic Lapse Rate
Temperatures decrease by 1 degree for every 100m increase in altitude
Orographic Rainfall
Precipitation produced when moist air is lifted and cooled as it moves over a mountain range.
Westerly
Prevailing wind in Tongariro region
Climax vegetation
The final stage of vegetation succession attainable by a plant community in an area under the environmental conditions
Beech forests
Climax vegetation in Tongariro region
Where can beech forests be found in the Tongariro region?
Southwest slopes of Ruapehu
Pihanga
Snowline
The altitude above which there is a permanent layer of ice and snow
Treeline
The altitude above which trees cannot grow
Where is the snowline on Ruapehu?
2000m asl
Where is the treeline on Ruapehu?
1600m asl
Plants found between snowline and treeline
Alpine herbs
Mosses
Lichen
Matweed
Maximum altitude beech forests can be found on Ruapehu
1200m asl
Average temperature at base of Ruapehu
13 degrees
Average temperature 1200-1600m asl on Ruapehu
9-12 degrees
Average temperature 1600-2000m asl on Ruapehu
5-9 degrees
Average temperature above the snowline on Ruapehu
5 degrees
How does volcanism interrupt vegetation succession in the Tongariro region?
Ash showers and ignimbrite flows smother plants, while fires, lahars, mass movements, pyroclastic flows, lava flows, and debris avalanches destroy everything in their path.
Trellis drainage pattern
Contains right angles. Result from underground folding and faulting which influence drainage
Radial drainage pattern
Patterns occur on round cones or mountains
Dendritic drainage patterns
From tree-like pattern. Develop in broken hill country with no marked differences in rock hardness.
Aeolian erosion
Erosion by wind
Fluvial erosion
Erosion by running water
Frost heave
The uplift of soil or debris due to the expansion of groundwater upon freezing.
Frost shattering
The mechanical disintegration of rock by the pressure of water freezing in pores and along grain boundaries. Also called freeze-thaw
Mass movement
Bulk movements of soil, rock, or debris downhill due to the influence of gravity
Weathering
The process of being worn down by the environment. Includes mechanical and chemical weathering.
Glaciation
The process of being covered by glaciers
Firn
Snow that has been compacted but is not yet glacial ice
Neve
The partially compacted granular snow that forms the surface part of the upper end of a glacier
Cirque
A bowl or depression formed by glaciation
Arete
A sharp ridge, formed by glaciation
Plucking
Erosion caused by glaciers along the ground as they pull up pieces of rock
Abrasion
Erosion caused by glaciers along the valley walls as they grind off pieces of rock
Lateral moraine
Moraine along the sides of a glacier
Terminal moraine
Moraine at the end of a glacier
U-shaped valley
Steep, straight-sided valleys with a flat bottom, created by glaciers
V-shaped valley
Steep-sided valleys created by rivers
Accumulation zone
The high-altitude area of a glacier where accumulation and compaction of snow/ice takes place.
Ablation zone
The low-altitude area of a glacier where melting takes place
When did the last Ice Age begin?
100,000 ya
When did the last Ice Age end?
18,000 ya
Wind eddies
Circular current of air
Alpine saddle
Lowest point of a ridge between two peaks.
How do alpine saddles increase denudation?
Wind funnels through the saddle and increases in strength, increasing denudation
How does frost heave move debris downhill?
When occurring on a slope, the frost heave will push debris out perpendicular to the surface, but when the frost melts the debris will move downhill. This is an example of soil creep
Soil creep
Downward movement of soil due to gravity. Happens over a long period of time
How does high precipitation affect mass movement?
Mass movement can be accelerated when the ground is waterlogged. This can trigger landslides or increase the rate of soil creep.
Average annual rainfall in Rangipo Desert
1000mm
Average annual rainfall at Whakapapa Village (1119m asl)
2200mm