A magnitude 4.0 earthquake near Maunaloa Road on November 30 occurred at a depth of 13 miles and was not linked to volcanic activity. The Hawaiian Volcano Observatory confirmed the event had no impact on the local volcanoes, despite around 130 residents reporting felt sensations across East Hawai‘i, North Kona, and southern Ka‘ū.
A magnitude 4.0 earthquake struck at 8:40 a.m. on Saturday, November 30th, approximately 11 miles west-northwest of Volcano on the Island of Hawai‘i, at a depth of 13 miles beneath the sea surface. According to the Hawaiian Volcano Observatory, this seismic event occurred south of the Northeast Rift Zone of Maunaloa and was not associated with any magmatic activity. The earthquake was reported to have no discernible impact on either Maunaloa or Kīlauea volcanoes. Following the quake, the United States Geological Survey (USGS) recorded about 130 reports from residents who felt the tremor, primarily from areas including East Hawai‘i, the Puna district, Hilo, Hamakua coast, North Kona, and southern parts of Ka‘ū.
The Hawaiian Islands are situated in a geologically active region, which frequently experiences seismic activity due to tectonic movements. Earthquakes in this area can signal various geological processes, including those associated with volcanic activity. However, the Hawaiian Volcano Observatory’s assessment indicates that not all earthquakes are related to magma movements within volcanoes. Understanding this distinction is crucial for public awareness and safety.
In summary, the 4.0 magnitude earthquake that occurred near Maunaloa Road did not correlate with volcanic activity, as reported by the Hawaiian Volcano Observatory. The event’s depth and location suggest it was part of the region’s natural tectonic activity rather than a precursor to volcanic eruptions. Monitoring such events helps to maintain public safety and understanding of geological processes in Hawai‘i.
Original Source: mauinow.com
