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New Zealand is a geologically active country and therefore has geohazards such as volcanoes, earthquakes, landslides and tsunami.
The word geohazard comes from two words:
So ‘geohazards’ means the risk of damage caused by a geological process.
Sometimes hazards are not obvious until pointed out. For example we wash our hands to avoid biohazards such as viruses and bacteria even though they are too small to see. We are told that some foods are poisonous (a biohazard) so we don’t eat them.
All geological hazards (geohazards) could be considered dormant until they are triggered.
When the hazard occurs it may then be called an event, accident, emergency, incident, or disaster. The study and monitoring of geohazards helps us to better prepare ourselves and respond to these geological events when they do occur.
Geohazards can be small features that have an impact only on their local area such as a small landslide that partially blocks a road or track through to large earthquakes that affect entire cities. They can also be very large events that have a widespread impact such as large tsunami.
New Zealand is geologically active. This is because it sits across the boundary between the Indo-Australian and Pacific tectonic plates. These moving plates create huge forces that have shaped our spectacular landscape; uplifting mountains, carving out lakes and rivers and creating our rugged coastline. These forces continue to form the land today and can also cause frequent earthquakes, landslides, volcanic eruptions, hydrothermal activity and even tsunami.
Earthquakes are caused when rocks break due to the stress applied by movement of the tectonic plates that make up the outer layer of the Earth. About 15,000 earthquakes occur every year in New Zealand, but we only feel about 150-200 of these earthquakes a year. While many are small, those that are strong and close to towns or cities can cause great damage and sometimes loss of life. For this reason it is important for New Zealanders to know how to prepare for and respond safely to earthquakes.
A tsunami is a series of powerful ocean surges caused by a large volume of the ocean floor being displaced – often by an undersea earthquake or landslide. Most tsunamis are similar to very strong, fast tides, rather than waves. The larger ones can travel a long way inland. Much of the damage from tsunamis is caused by the erosion generated by the strong currents and floating debris.
When molten material (magma) reaches the earth’s surface a volcano is formed. A volcano will erupt fragmented rock and magma (ash) and release steam and gases. New Zealand’s volcanoes are often active and are constantly monitored, for example Ruapehu, Tongariro, White Island. Ash from eruptions can spread over large distances so can affect people living a long way from the eruption. Hazards also exist close to the active vent(s).
Lahar is an Indonesian word that describes a volcanic mudflow. When moving, a lahar looks like a mass of wet concrete that carries rock debris. Lahars vary in size and speed and can cause widespread damage.
Eruptions may trigger lahars by quickly melting snow and ice on a volcano or ejecting water from a crater lake. Lahars are also formed by heavy rainfall during or after an eruption, when volcanic ash is washed off the volcano. Some of the largest lahars begin as landslides.
Hydrothermal systems are a by-product of volcanic activity. The residual (volcanic) heat at depth heats the local ground water to create the geothermal activity. Most of New Zealand’s hydrothermal activity occurs in the Taupō Volcanic Zone, an area that extends from White Island to Mt. Ruapehu.
Hydrothermal activity is usually confined to hot springs, geysers and warm ground. However, if they become unstable eruptions can occur. Hydrothermal processes are often acidic and can alter the nature of rocks and soils, leading to slumping and collapse of ground, which can cause damage to property and harm people. Hydrogen sulphide gas can also be emitted and if there are high levels it can be harmful.
A landslide is a movement of soil, rock and debris down a slope. Landslides often happen as a result of other natural disasters, such as earthquakes, volcanic eruptions and floods (rainfall).
Landslides are common throughout New Zealand. Serious landslides in built-up areas can cause thousands of dollars in damage and threaten lives.
Earthquakes are a common geohazard in New Zealand; why do you think we get so many earthquakes? Image: LEARNZ.
Earthquakes can cause rock fall or landslides like this one that occurred during the Christchurch earthquake. Where in Christchurch is this and what problems did these rock fall cause? Image: LEARNZ.
Volcanoes are another type of geohazard. Do you know which New Zealand volcano this is? Image: GNS Science.
Tsunami can cause huge damage to low lying coastal areas. This is a village near the coast of Sumatra after the 2004 Boxing Day tsunami. What causes tsunami? Image: Public Domain.
Hydrothermal systems can be part of volcanic activity. This is the Waimangu hot springs near Mount Tarawera. How can hydrothermal activity be hazardous and how can this hazard be avoided? Image: LEARNZ.
Landslides are also a common geohazard in New Zealand. This is the Dart landslide which has been active for several thousand years. On 4 January 2014 a large debris flow occurred; do you know what happened after this landslide? Image: Simon Cox, GNS Science.