Worldwide Volcano earthquakes and Volcano earthquake notifications – New Zealand

Last update: February 28, 2013 at 11:20 pm by By

Ruapehu volcano – latest eruption : 2007
Ruapehu, one of New Zealand’s most active volcanoes, is a complex stratovolcano constructed during at least 4 cone-building episodes dating back to about 200,000 years ago. The 110 cu km dominantly andesitic volcanic massif is elongated in a NNE-SSW direction and is surrounded by another 100 cu km ring plain of volcaniclastic debris, including the Murimoto debris-avalanche deposit on the NW flank. A series of subplinian eruptions took place at Ruapehu between about 22,600 and 10,000 years ago, but pyroclastic flows have been infrequent at Ruapehu. A single historically active vent, Crater Lake, is located in the broad summit region, but at least five other vents on the summit and flank have been active during the Holocene. Frequent mild-to-moderate explosive eruptions have occurred in historical time from the Crater Lake vent, and tephra characteristics suggest that the crater lake may have formed as early as 3000 years ago. Lahars produced by phreatic eruptions from the summit crater lake are a hazard to a ski area on the upper flanks and to lower river valleys.
(some text & images : Smithsonian Institution)

SRC Location UTC Date/time M D INFO
GEONET Ohakune Nov 19 20:27 2.6 139 MAP I Felt It
GEONET Ohakune Nov 07 03:41 1.8 62 MAP I Felt It
GEONET Ohakune Sep 29 08:57 0.9 10 MAP I Felt It
GEONET Ohakune Sep 17 10:29 1.0 12 MAP I Felt It
GEONET Ohakune Aug 19 07:04 1.9 6 MAP I Felt It
GEONET Ohakune Jul 11 02:58 2.1 10 MAP I Felt It
GEONET Ohakune Jun 16 06:36 0.9 16 MAP I Felt It
GEONET Ohakune Jun 04 02:45 0.5 14 MAP I Felt It
GEONET Ohakune Dec 27 07:30 0.6 9 MAP I Felt It
GEONET Ohakune Nov 27 14:58 3.5 135 MAP I Felt It INFO
GEONET Turangi Nov 25 10:33 1.6 77 MAP I Felt It
GEONET Ohakune Oct 22 10:42 1.4 10 MAP I Felt It
GEONET Ohakune Oct 06 06:36 1.3 66 MAP I Felt It
GEONET Ohakune Sep 23 14:13 0.9 29 MAP I Felt It
GEONET Ohakune Aug 28 05:33 1.3 7 MAP I Felt It
GEONET Ohakune Aug 20 17:27 2.8 14 MAP I Felt It
GEONET Ohakune Aug 04 14:32 1.5 22 MAP I Felt It
GEONET Ohakune Jul 22 22:46 1.9 14 MAP I Felt It
GEONET Ohakune Jul 22 17:54 0.7 5 MAP I Felt It
GEONET Turangi Jul 21 01:16 4.4 13 MAP I Felt It INFO
GEONET Ohakune Jun 25 01:37 0.5 5 MAP I Felt It
GEONET Ohakune Jun 10 17:22 2.0 17 MAP I Felt It
GEONET Ohakune May 29 15:27 0.8 26 MAP I Felt It
GEONET Ohakune May 29 15:24 0.8 40 MAP I Felt It
GEONET Ohakune Apr 28 03:32 2.7 2 MAP I Felt It
GEONET Ohakune Apr 24 22:20 2.2 52 MAP I Felt It
GEONET Ohakune Apr 02 08:14 1.0 32 MAP I Felt It
GEONET Ohakune Mar 29 18:44 1.4 17 MAP I Felt It
GEONET Ohakune Mar 28 17:50 1.9 117 MAP I Felt It
GEONET Ohakune Mar 27 12:53 0.8 36 MAP I Felt It


Taranaki volcano (Mount Egmont) – latest eruption : 1854
The nearly symmetrical, steep-sided cone of Taranaki (also known as Egmont), is New Zealand’s largest andesitic stratovolcano. Taranaki is surrounded by a ring plain of debris-avalanche and lahar deposits that and extend to the coast. The isolated Taranaki volcanic center is located on the west coast of central North Island at the southern end of a volcanic arc extending NW along the Northland Peninsula. Taranaki is the youngest and SE-most of a group of three volcanoes beginning with the Pleistocene Kaitoke Range. Fanthams Peak breaks the symmetry of Taranaki on its south flank, and four lava domes are located on the lower north and south flanks. Multiple episodes of edifice collapse have occurred in the past 50,000 years. Explosive activity, sometimes accompanied by pyroclastic flows and lava dome growth, has occurred frequently throughout the Holocene. Taranaki’s latest eruption took place in 1854 AD.
(some text & images : Smithsonian Institution)

SRC Location UTC Date/time M D INFO
GEONET Stratford Nov 25 07:11 1.8 12 MAP I Felt It
GEONET Opunake Nov 21 16:03 2.5 7 MAP I Felt It
GEONET Opunake Nov 12 00:12 2.4 19 MAP I Felt It
GEONET Opunake Nov 09 09:49 2.7 240 MAP I Felt It
GEONET Opunake Oct 31 07:42 2.5 12 MAP I Felt It
GEONET Opunake Sep 29 10:55 2.1 11 MAP I Felt It
GEONET New Plymouth Sep 20 21:40 1.7 7 MAP I Felt It
GEONET Stratford Sep 12 02:50 2.5 223 MAP I Felt It
GEONET Opunake Sep 07 05:50 2.6 10 MAP I Felt It
GEONET Stratford Sep 05 14:00 2.8 240 MAP I Felt It
GEONET New Plymouth Aug 24 11:05 2.1 12 MAP I Felt It
GEONET Opunake Aug 22 08:38 1.9 10 MAP I Felt It
GEONET Stratford Aug 06 19:35 3.0 242 MAP I Felt It INFO
GEONET Opunake Jul 29 03:02 2.0 18 MAP I Felt It
GEONET Opunake Jul 28 18:31 1.9 19 MAP I Felt It
GEONET Stratford Jul 22 21:57 2.7 151 MAP I Felt It
GEONET Opunake Jul 20 11:41 2.2 17 MAP I Felt It
GEONET Opunake Jul 16 18:20 2.3 21 MAP I Felt It
GEONET Opunake Jul 08 03:35 2.5 18 MAP I Felt It
GEONET Opunake Jul 03 16:29 2.4 18 MAP I Felt It
GEONET Opunake Jun 21 12:46 1.6 5 MAP I Felt It
GEONET New Plymouth Jun 20 12:09 1.6 13 MAP I Felt It
GEONET Stratford Jun 05 12:45 2.0 28 MAP I Felt It
GEONET Opunake Jun 02 11:07 2.4 17 MAP I Felt It
GEONET Stratford Jun 02 00:59 3.0 240 MAP I Felt It INFO
GEONET New Plymouth May 28 10:49 2.7 13 MAP I Felt It
GEONET Stratford May 26 02:52 3.1 229 MAP I Felt It INFO
GEONET New Plymouth May 10 21:30 2.2 9 MAP I Felt It
GEONET Stratford May 04 19:31 2.6 131 MAP I Felt It
GEONET New Plymouth Apr 21 08:19 2.9 276 MAP I Felt It


Okataina volcano – latest activity : 1981
The massive, dominantly rhyolitic Okataina Volcanic Centre is surrounded by extensive ignimbrite and pyroclastic sheets produced during multiple caldera-forming eruptions. Numerous lava domes and craters erupted from two subparallel NE-SW-trending vent lineations form the Haroharo and Tarawera volcanic complexes. Lava domes of the Haroharo complex, at the northern end of the Okataina Volcanic Centre, occupy part of the 16 x 26 km Pleistocene Haroharo caldera, which formed incrementally between 300,000 and 50,000 years before present (BP). The oldest exposed rocks on the caldera floor are about 22,000 years old. The Tarawera complex at the southern end of Okataina consists of 11 rhyolitic lava domes and associated lava flows. The oldest domes were formed as late as about 15,000 years BP, and the youngest were formed in the Kaharoa eruption about 800 years BP. The NE-SW Tarawera vent lineation extends from the two dacitic cones of Maungaongaonga and Mangakakaramea on the SW to Mount Edgecumbe on the NE. Construction of the Haroharo and Tarawera complexes impounded lakes Rotoiti, Totoehu, Okataina, and Tarawera against the outer margins of the Okataina ring structure. A major hydrothermal area is located at Waimangu; the world-renowned Pink and White Terrace siliceous sinter deposits were destroyed during the major basaltic explosive eruption of 1886.
(some text & images : Smithsonian Institution)

SRC Location UTC Date/time M D INFO
GEONET Rotorua Oct 17 23:35 1.6 9 MAP I Felt It
GEONET Rotorua Oct 10 18:49 2.4 193 MAP I Felt It
GEONET Rotorua Oct 05 14:25 2.6 139 MAP I Felt It
GEONET Rotorua Sep 27 14:43 1.8 8 MAP I Felt It
GEONET Rotorua Sep 03 06:48 1.6 10 MAP I Felt It
GEONET Rotorua Aug 27 17:01 2.1 106 MAP I Felt It
GEONET Rotorua Aug 25 15:44 2.6 256 MAP I Felt It
GEONET Rotorua Aug 17 16:34 2.3 169 MAP I Felt It
GEONET Rotorua Jul 29 09:19 1.7 5 MAP I Felt It
GEONET Rotorua Jul 24 00:45 2.9 141 MAP I Felt It
GEONET Rotorua Jul 20 09:21 2.8 10 MAP I Felt It
GEONET Rotorua Jul 17 05:08 2.4 82 MAP I Felt It
GEONET Rotorua Jul 02 18:04 2.3 86 MAP I Felt It
GEONET Rotorua Jun 19 16:31 2.1 137 MAP I Felt It
GEONET Rotorua Jun 11 02:03 1.7 7 MAP I Felt It
GEONET Rotorua Jun 05 16:14 2.9 207 MAP I Felt It
GEONET Rotorua May 10 11:57 3.4 468 MAP I Felt It INFO
GEONET Rotorua Apr 26 06:11 2.7 159 MAP I Felt It
GEONET Rotorua Apr 20 17:52 1.7 10 MAP I Felt It
GEONET Rotorua Apr 08 16:39 2.2 168 MAP I Felt It
GEONET Rotorua Apr 06 21:03 2.0 10 MAP I Felt It
GEONET Rotorua Apr 05 09:24 3.1 197 MAP I Felt It INFO
GEONET Rotorua Mar 19 07:29 2.2 8 MAP I Felt It
GEONET Rotorua Feb 05 23:05 3.3 188 MAP I Felt It INFO
GEONET Rotorua Feb 01 17:44 2.3 120 MAP I Felt It
GEONET Rotorua Jan 30 11:42 3.0 187 MAP I Felt It INFO
GEONET Rotorua Jan 29 06:41 1.9 9 MAP I Felt It
GEONET Rotorua Jan 09 06:45 2.4 62 MAP I Felt It
GEONET Rotorua Jan 08 04:24 2.4 9 MAP I Felt It
GEONET Rotorua Jan 08 04:20 2.2 8 MAP I Felt It


Tongariro volcano – latest activity : 2006 – latest eruption : 1977
Tongariro is a large andesitic volcanic massif, located immediately NE of Ruapehu volcano, that is composed of more than a dozen composite cones constructed over a period of 275,000 years. Vents along a NE-trending zone extending from Saddle Cone (below Ruapehu volcano) to Te Mari crater (including vents at the present-day location of Ngauruhoe) were active during a several hundred year long period around 10,000 years ago, producing the largest known eruptions at the Tongariro complex during the Holocene. North Crater stratovolcano, one of the largest features of the massif, is truncated by a broad, shallow crater filled by a solidified lava lake that is cut on the NW side by a small explosion crater. The youngest cone of the complex, Ngauruhoe, has grown to become the highest peak of the massif since its birth about 2500 years ago. The symmetrical, steep-sided Ngauruhoe, along with its neighbor Ruapehu to the south, have been New Zealand’s most active volcanoes during historical time.
(some text & images : Smithsonian Institution)

SRC Location UTC Date/time M D INFO
GEONET Turangi Nov 26 05:52 1.5 5 MAP I Felt It
GEONET Turangi Nov 09 07:47 0.9 8 MAP I Felt It
GEONET Turangi Oct 22 15:54 1.1 5 MAP I Felt It
GEONET Turangi Oct 17 09:46 2.3 6 MAP I Felt It
GEONET Turangi Oct 16 03:32 0.8 5 MAP I Felt It
GEONET Turangi Sep 04 06:02 1.4 5 MAP I Felt It
GEONET Turangi Sep 01 04:59 1.3 5 MAP I Felt It
GEONET Turangi Aug 30 08:06 1.7 103 MAP I Felt It
GEONET Turangi Aug 27 17:56 0.8 11 MAP I Felt It
GEONET Turangi Aug 25 06:04 0.7 5 MAP I Felt It
GEONET Turangi Aug 23 22:02 2.3 147 MAP I Felt It
GEONET Turangi Aug 19 22:59 1.3 105 MAP I Felt It
GEONET Turangi Aug 11 06:18 2.0 88 MAP I Felt It
GEONET Turangi Jun 15 07:57 3.0 114 MAP I Felt It INFO
GEONET Turangi Jun 01 08:54 2.0 135 MAP I Felt It
GEONET Turangi May 23 06:37 2.4 95 MAP I Felt It
GEONET Turangi May 03 14:59 1.7 126 MAP I Felt It
GEONET Turangi Mar 25 21:49 1.7 7 MAP I Felt It
GEONET Turangi Mar 22 22:08 2.3 105 MAP I Felt It
GEONET Turangi Mar 22 10:09 2.0 113 MAP I Felt It
GEONET Turangi Feb 23 19:53 1.4 5 MAP I Felt It
GEONET Turangi Feb 05 00:10 1.3 10 MAP I Felt It
GEONET Turangi Feb 04 05:54 1.4 76 MAP I Felt It
GEONET Turangi Jan 27 02:32 2.6 114 MAP I Felt It
GEONET Turangi Jan 13 10:47 2.1 109 MAP I Felt It
GEONET Turangi Jan 01 05:01 2.4 123 MAP I Felt It
GEONET Turangi Dec 22 13:49 1.1 5 MAP I Felt It
GEONET Turangi Nov 27 10:08 1.2 5 MAP I Felt It
GEONET Turangi Nov 25 04:19 2.4 163 MAP I Felt It
GEONET Turangi Nov 20 06:05 1.1 9 MAP I Felt It


White Island volcano – latest eruption : 2001
Uninhabited 2 x 2.4 km White Island, one of New Zealand’s most active volcanoes, is the emergent summit of a 16 x 18 km submarine volcano in the Bay of Plenty about 50 km offshore of North Island. The 321-m-high island consists of two overlapping andesitic-to-dacitic stratovolcanoes; the summit crater appears to be breached to the SE because the shoreline corresponds to the level of several notches in the SE crater wall. Volckner Rocks, four sea stacks that are remnants of a lava dome, lie 5 km NNE of White Island. Intermittent moderate phreatomagmatic and strombolian eruptions have occurred at White Island throughout the short historical period beginning in 1826, but its activity also forms a prominent part of Maori legends. Formation of many new vents during the 19th and 20th centuries has produced rapid changes in crater floor topography. Collapse of the crater wall in 1914 produced a debris avalanche that buried buildings and workers at a sulfur-mining project.
(some text & images : Smithsonian Institution)

SRC Location UTC Date/time M D INFO
GEONET White Island Nov 27 07:12 2.4 6 MAP I Felt It
GEONET White Island Nov 27 05:29 2.3 8 MAP I Felt It
GEONET White Island Nov 24 02:39 2.2 108 MAP I Felt It
GEONET White Island Nov 23 08:38 2.6 137 MAP I Felt It
GEONET White Island Nov 22 18:40 2.0 43 MAP I Felt It
GEONET White Island Nov 22 13:45 2.3 109 MAP I Felt It
GEONET White Island Nov 21 17:05 3.1 235 MAP I Felt It INFO
GEONET White Island Nov 19 23:42 2.7 8 MAP I Felt It
GEONET White Island Nov 19 23:35 2.8 5 MAP I Felt It INFO
GEONET White Island Nov 19 21:38 3.0 5 MAP I Felt It INFO
GEONET White Island Nov 19 13:25 2.5 171 MAP I Felt It
GEONET White Island Nov 19 12:11 1.8 14 MAP I Felt It
GEONET White Island Nov 14 21:57 2.7 122 MAP I Felt It
GEONET White Island Nov 10 10:33 2.3 65 MAP I Felt It
GEONET White Island Nov 08 11:17 2.3 58 MAP I Felt It
GEONET White Island Nov 07 13:13 2.2 74 MAP I Felt It
GEONET White Island Nov 07 10:48 2.4 90 MAP I Felt It
GEONET White Island Nov 04 09:38 2.0 118 MAP I Felt It
GEONET White Island Nov 03 19:37 2.5 151 MAP I Felt It
GEONET White Island Nov 02 12:44 2.8 162 MAP I Felt It
GEONET Whakatane Nov 02 07:29 2.0 5 MAP I Felt It
GEONET White Island Oct 31 01:37 2.3 68 MAP I Felt It
GEONET White Island Oct 29 22:38 2.9 158 MAP I Felt It
GEONET White Island Oct 29 12:32 3.7 262 MAP I Felt It INFO
GEONET White Island Oct 29 12:10 2.3 106 MAP I Felt It
GEONET White Island Oct 25 05:35 2.7 119 MAP I Felt It
GEONET White Island Oct 21 22:52 2.3 18 MAP I Felt It
GEONET White Island Oct 21 13:30 2.5 5 MAP I Felt It
GEONET White Island Oct 21 08:16 2.5 69 MAP I Felt It
GEONET White Island Oct 21 00:59 2.5 134 MAP I Felt It


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Latitude (area) where you felt the earthquake
Longitude (area) where you felt the earthquake
MMI II (Very weak shaking) ?
People :
Felt by persons at rest, on upper floors or favorably placed.
MMI III (Weak shaking) ?
People :
Felt indoors; hanging objects may swing, vibration similar to passing of light trucks, duration may be estimated, may not be recognized as an earthquake.
MMI IV (Light shaking) ?
People :
Generally noticed indoors but not outside. Light sleepers may be awakened. Vibration may be likened to the passing of heavy traffic, or to the jolt of a heavy object falling or striking the building.
Fittings :
Doors and windows rattle. Glassware and crockery rattle. Liquids in open vessels may be slightly disturbed. Standing motorcars may rock.
Structures :
Walls and frames of buildings, and partitions and suspended ceilings in commercial buildings, may be heard to creak.
MMI V (Moderate shaking) ?
People :
Generally felt outside, and by almost everyone indoors. Most sleepers awakened. A few people alarmed.
Fittings :
Small unstable objects are displaced or upset. Some glassware and crockery may be broken. Hanging pictures knock against the wall. Open doors may swing. Cupboard doors secured by magnetic catches may open. Pendulum clocks stop, start, or change rate.
Structures :
Some large display windows cracked. A few earthenware toilet fixtures cracked.
MMI VI (Strong shaking) ?
People Felt by all. People and animals alarmed. Many run outside. Difficulty experienced in walking steadily.
Fittings :
Objects fall from shelves. Pictures fall from walls. Some furniture moved on smooth floors, some unsecured free-standing fireplaces moved. Glassware and crockery broken. Very unstable furniture overturned. Small church and school bells ring. Appliances move on bench or table tops. Filing cabinets or "easy glide" drawers may open (or shut).
Structures :
Slight damage to buildings with low standard. Some stucco or cement plaster falls. Large display windows broken. Damage to a few weak domestic chimneys, some may fall.
Environment :
Trees and bushes shake, or are heard to rustle. Loose material may be dislodged from sloping ground, e.g. existing slides, talus slopes, shingle slides.
MMI VII (Very strong shaking) ?
People
General alarm. Difficulty experienced in standing. Noticed by motorcar drivers who may stop.
Fittings :
Large bells ring. Furniture moves on smooth floors, may move on carpeted floors. Substantial damage to fragile contents of buildings.
Structures :
Unreinforced stone and brick walls cracked. Low standard buildings cracked with some minor masonry falls. A few instances of damage to buildings of ordinary workmanship. Unbraced parapets, unbraced brick gables, and architectural ornaments fall. Roofing tiles, especially ridge tiles may be dislodged. Many unreinforced domestic chimneys damaged, often falling from roof-line. Water tanks Type I burst. A few instances of damage to brick veneers and plaster or cement-based linings. Unrestrained water cylinders (hot-water cylinders) may move and leak. Some common windows cracked. Suspended ceilings damaged.
Environment :
Water made turbid by stirred up mud. Small slides such as falls of sand and gravel banks, and small rock-falls from steep slopes and cuttings. Instances of settlement of unconsolidated or wet, or weak soils. Some fine cracks appear in sloping ground. A few instances of liquefaction (i.e. small water and sand ejections).
MMI VIII (Severe shaking) ?
People Alarm may approach panic. Steering of motorcars greatly affected. Structures : Low standard buildings heavily damaged, some collapse. ordinary workmanship buildings damaged, some with partial collapse. Reinforced masonry or concrete buildings damaged in some cases. A few instances of damage to buildings and bridges designed and built to resist earthquakes. Monuments and pre-1976 elevated tanks and factory stacks twisted or brought down. Some pre-1965 infill masonry panels damaged. A few post-1980 brick veneers damaged. Decayed timber piles of houses damaged. Houses not secured to foundations may move. Most unreinforced domestic chimneys damaged, some below roof-line, many brought down. Environment : Cracks appear on steep slopes and in wet ground. Small to moderate slides in roadside cuttings and unsupported excavations. Small water and sand ejections and localized lateral spreading adjacent to streams, canals, lakes, etc.
MMI IX (Violent shaking) ?
Structures Many low standard buildings destroyed. Ordinary workmanship buildings heavily damaged, some collapse. Reinforced masonry or concrete buildings damaged, some with partial collapse. Buildings and bridges designed and built to resist earthquakes damaged in some cases, some with flexible frames seriously damaged. Damage or permanent distortion to some buildings and bridges, designed and built to normal use standards. Houses not secured to foundations shifted off. Brick veneers fall and expose frames. Environment : Cracking of ground conspicuous. Landsliding general on steep slopes. Liquefaction effects intensified and more widespread, with large lateral spreading and flow sliding adjacent to streams, canals, lakes, etc.
Write your experience below + let us know if your property has been damaged (even slight damage) or if you have knowledge of any damage caused by this earthquake. (max. 500 characters)

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