Earthquakes
The tremor occurred at 23:48 GMT. The epicenter of the quake was located at the depth of 190 kilometers (118 miles) and centered 91 kilometers (56.5 miles) west of Madang province.
There have been no reports of destruction or casualties caused by the earthquake so far.
No tsunami warning was issued.
The earthquake, which struck at 1:25 p.m. local time on Friday, was centered about 112 miles (180 kilometers) northwest of Attu Island in Alaska, or 168 miles (270 kilometers) southeast of Bering Island in Russia. It struck at a depth of about 19 miles (31 kilometers), making it a shallow earthquake.
The U.S. National Tsunami Warning Center put the preliminary magnitude of the earthquake at 6.8. "Based on earthquake information and historic tsunami records, the earthquake is not expected to generate a tsunami," the center said.
Friday's earthquake is expected to have been felt across parts of the Aleutian Islands, but damage or casualties are unlikely. The closest islands - Attu Island and Bering Island - have only a small population. Attu Island is also home to Attu Station, which was closed in 2010.
The sparsely populated region of Alaska, which sits on the so-called 'Pacific Ring of Fire', is occasionally struck by powerful earthquakes. Most notably, an enormous 9.2-magnitude earthquake struck north of Prince William Sound in Alaska on March 27, 1964, unleashing a tsunami which killed at least 143 people.

More than 450 people felt a 'moderate' earthquake near Whakatane when it hit at 9pm yesterday. It was followed hours later with another shake in the Bay of Plenty.
At 9.06pm yesterday a 4.2 magnitude quake struck at 10km deep. Only eight people reported feeling the early morning quake, but 454 said they felt last night's tremor. The quakes follow a 4.1 shake in the same spot at 1.35pm and another at 11.39am. Geonet recorded at least 86 "felt" reports from people describing yesterday afternoon's quake between "strong" and "light".
All occurred in the northern part of the caldera, the first at 9:49, the second at 9:53 and the third at 9:54. This is reported by the Iceland Met Office.
Last week, nearly 600 earthquakes were measured in Iceland which is similar to the preceeding week. Only six of them exceeded the magnitude of 3, the largest occurring on May 27th in Bárðarbunga.
Iceland Met Office link for current earthquake graphs

This Temblor map shows the Global Earthquake Activity Rate (GEAR) model for Svalbard in the Arctic Circle. This map shows that today’s M=5.0 earthquake (magnitude from the USGS) should not be considered surprising and that the region could experience larger quakes.
The Svalbard archipelago represents an uplifted portion of the Barents Sea, which separates Svalbard from Northern Europe. To the west of the archipelago is the Mid-Atlantic Ridge, and the Spitsbergen Fracture Zone, a divergent plate boundary between the North American and Eurasian plates. Much of the seismicity in this part of the Arctic Ocean occurs on or near the Mid-Atlantic Ridge, which has a spreading rate of approximately 2.5 cm/yr (1 inch). However, by examining the historical seismicity of the island of Spitsbergen and the rest of Svalbard, it is clear that this remote archipelago is no stranger to earthquakes.

This U.S. Geological Survey map shows the location of a powerful earthquake that struck Indonesia's central Sulawesi province on Monday, May 29, 2107.
The U.S. Geological Survey says the quake Monday evening near the city of Poso had a preliminary magnitude of 6.6 and was located at a depth of 9 kilometers (6 miles).
Al Shinto radio reported that residents ran from their homes in panic.
Shallow earthquakes tend to cause more damage on the Earth's surface.
Source: AP
A large earthquake also rocked south Iceland in early May 17 with reports of Hekla Volcano being ready to erupt.
Bardarbunga, is a volcano located under Iceland's most extensive glacier, Vatnajokull glacier to the north. Bardarbunga is the second highest mountain in Iceland and is a part of a volcanic system that is approximately 200 kilometers long and 25 kilometers wide, that system includes Hekla Volcano.
"People were just wondering what was going on," said William Faught, the director of the Vinton County Emergency Management Agency, who also felt a tremor from the earthquake.
"It's the first indication that we have in our catalog of any earthquake occurring in Vinton County," said Jeff Fox, a seismologist at the Ohio Department of Natural Resources (ODNR).
He classified yesterday's earthquake at a 3.8 magnitude instead of the 3.4 magnitude that was reported through the U.S. Geological Survey (USGS). John Bellini, a geophysicist at the USGS, didn't think much of yesterday's event other than it being another sporadic earthquake. Bellini says yesterday's earthquake did not reach the level of intensity to do any real damage.

Earthquakes were found to be the largest hazard, with the number of people potentially affected jumping from 1.4 billion in 1975 to 2.7 billion in 2015. Now, they say one in three people is exposed to the risk of earthquakes.
In the last few decades, the risk has dramatically increased; the number of people living in seismic areas, for example, has increased by 93 percent in just 40 years.
The findings, compiled in the Atlas of the Human Planet 2017, reveal the global exposure to natural disasters has doubled since 1975, largely as a result of population growth and development.
Additional images
USGS page: M 5.8 - 161km ESE of Nikolski, Alaska
USGS status: Reviewed by a seismologist
Reports from the public: 1 person
2017-05-24 16:36:01 UTC 5.8 magnitude, 11 km depth










