A busy day in one of the most seismically active regions of Canada – offshore Vancouver Island.

Four earthquakes between M5.1 and 6.0 over the past 5 hours (and many more aftershocks). No damage/impacts

Latest information: https://t.co/XG5si9iphu

Shaking: https://t.co/pEuqG9lO4P pic.twitter.com/qMVEwlKGqX — John Cassidy (@earthquakeguy) December 23, 2019

In April, 1992 a M6.8 earthquake occurred in this same region, along the Revere-Dellwood-Wilson transform fault…

Details:https://t.co/puTROCwkFe — John Cassidy (@earthquakeguy) December 23, 2019

Five earthquakes, including a magnitude-6.0, struck west of northern Vancouver Island Monday. According to Natural Resources Canada, the first quake hit at 8:44 a.m. at a magnitude 5.1. The second was a 5.6 at 11:13 a.m. The third was at 11:49 a.m. and was a 5.8. The fourth and largest was a 6.0 magnitude at 12:56 p.m. And the fifth was at 4.8 magnitude at 3:38 p.m. (all times in PST)None of the quakes caused a tsunami warning. Andrew Schaeffer, a seismologist with Earthquakes Canada, said during the first four earthquakes, two plates were sliding past each other, which don’t generate a tsunami. “To generate a tsunami, you need to have some vertical movement on the fault and this is not what happened,” Schaeffer said.“It’s pretty common to get these events in this area… it’s a strike-slip fault between North America and the Pacific,” Schaeffer said. “Magnitude 5s and larger [are common]. The largest we see in the area is about a 6.0.”Each earthquake was around 170 kilometres west of Port Hardy, at a depth of five-kilometres. “This is where a few plates come together that accommodate the relative motion between the Pacific Ocean and the North American Plate. This area is a little bit separate from the Cascadia Subduction Zone,” Schaeffer said. “It’s one of the more seismically active areas, for example, over the last year there’s been almost 90 magnitude three earthquakes within 100 kilometres of this region. Almost 20 magnitude fours.” Schaeffer says the quakes coming in a sequence is often seen, although it’s not as common for the magnitudes to climb like they did on Monday. However, it has happened before. Seismologist John Cassidy says there are also numerous aftershocks in the area. He also said there was a 6.3 magnitude earthquake and a 5.5 magnitude earthquake in July, 60 to 80 kilometres to the northwest of Monday’s four earthquakes. Foreshocks are relatively smaller earthquakes that precede the largest earthquake in a series, which is termed the mainshock. Not all mainshocks have foreshocks. Schaeffer said researchers are still examining the quakes. “This may not necessarily be a case of foreshock, aftershock but rather this might be some sort of swarm but to identify whether this is an earthquake swarm or not, we need to look at the data as it comes in,” Schaeffer said. According to the University of Alaska Fairbanks Alaska Earthquake Center, an earthquake swarm has no clear mainshock. Instead, it churns out a number of earthquakes of comparable size over days or months, with a lot of smaller quakes thrown in. There were a few people on northern Vancouver Island, Richmond and the Lower Mainland who reported feeling the third and fourth earthquake. Schaeffer said a 6.0 magnitude earthquake that is shallower and closer to Victoria or the Lower Mainland would lead to some moderate shaking being felt and possibly cause damage to some older buildings. “Where these earthquakes were, they were far enough offshore that they’re essentially not felt,” Schaeffer said.With files from The Canadian Press