Earth Changes
Cesar Uruena, a Red Cross rescue director, said the landslide buried more than 14 homes in the city of Manizales in Caldas state, 165 kilometres (102 miles) northwest of the capital, Bogota.
Rescuers have reports of 14 people dead and 13 injured, Uruena said.
"We are talking about an average of 60 people missing. This could be a bit speculative, but the number is high," Uruena told The Associated Press by telephone.
He said that because of the many people listed as missing, rescuers would continue the search through the night.
Caldas emergency services director Sandra Lopez said heavy rains pounded the area the night before and caused a part of a mountain to collapse onto the houses.
As a preventative measure, authorities are asking that 35 homes near the landslide site be evacuated.
Source: The Canadian Press
And along the southeast shoreline in the Imperial Valley near Niland lies an explosive history going back thousands of years.
A series of what would appear to be four rather ordinary hills are actually volcanoes known as the Salton Buttes.
"A variety of people, when it comes to the Salton Sea, ask, 'Why invest in the Salton Sea?' There's more of a history to it than what we see here today," said Chris Schoneman, the manager at the Sonny Bono Salton Sea National Wildlife Refuge.
One of the volcanoes, a butte called Rock Hill, comes at the end of a hiking trail and provides fantastic views of the sea and wildlife.
"The hill formed about 16,000 years ago. It was an active volcano -- last active about 8,000 to 10,000 years ago," said Schoneman.
Obsidian Butte has more of a volcano-look -- covered with chunks of obsidian rock. Obsidian is volcanic glass that results from lava quickly cooling above ground.
Another volcano, Mullett Island, can only be reached by boat. It's also a nesting spot for 10,000 seabirds.
The hundreds of species of birds are a big draw for the 20,000 yearly visitors to the refuge.
But Schoneman says most don't know anything about the volcanoes there. And it's not like there are lava flows or spewing ash to catch a glimpse of.
But there is molten magma miles below the earth's surface. The geothermal activity is shown by surrounding power plants, tapping into that heat to create electricity.
A large sinkhole that resembles something out of a Hollywood movie has closed a section of Bayview Avenue to traffic.
It happened overnight on Thursday after a water main break. Bayview Avenue just north of Steeles Avenue is closed between Proctor Avenue and Laureleaf Road as crews work to fix the buckled pavement.
In some sections, the crack is as wide as a traffic lane.
CBC's Lorenda Reddekopp was at the scene and said York Regional police officers were describing the nine-metre deep sinkhole as "something out of Jurassic Park."
A German tourist watched the two 250ft trees fall to the ground at the Trail of 100 Giants in California and captured the amazing moments and the crushing sound on video.
The trees lay the length of a football pitch and their diameter of their torn roots and base was 20ft.
A tornado uprooted trees and tore the roof of a stable as it swept past the village of Inkberrow in the mid-afternoon.
Amazingly, the fierce winds threw the stable roof 20metres through the air before it came to rest stuck in the branches of a nearby tree.
Other trees were left broken in half at the Knowle Fields Barn Farm complex.
The latest aftershock came at 2:44 a.m. and was a 2.7-magnitude quake, according to the USGS website .
The epicenter of the initial quake was about 6 miles north of Prague, 7 miles east-southeast of Sparks, 9 miles west-northwest of Paden or roughly 20 miles northeast of Oklahoma City. The first aftershock happened in the same area, according to the United States National Weather Service office in Norman, which posted this message to Facebook at about 3 a.m.
Needles at the U.S. Geological Survey jumped again on Thursday morning, when a 2.3 magnitude aftershock rattled Louisa County.
Geological Survey staffers said in a lecture this week they've actually recorded over 600 aftershocks following the August 23 quake.
Staff geologist and Mineral, Virginia resident Mark Carter lectured on the Virginia quake's aftershocks on November 2 in Fairfax. The lecture was also shared via the USGS twitter feed.
The geologist said that in central Virginia, seismic activity is "somewhat regular." However, the strength of the August 23 quake had not been seen in a century, and the damage has been unprecedented.
"It was a miracle that there were no casualties given the damage we found," he wrote.
Saturday, November 05, 2011 at 07:13:57 UTC
Saturday, November 05, 2011 at 04:13:57 AM at epicenter
Time of Earthquake in other Time Zones
Location 23.529°S, 70.400°W
Depth 27.3 km (17.0 miles)
Region ANTOFAGASTA, CHILE
Distances 22 km (13 miles) NNE of Antofagasta, Antofagasta, Chile
154 km (95 miles) S of Tocopilla, Antofagasta, Chile
177 km (109 miles) SW of Calama, Antofagasta, Chile
1106 km (687 miles) N of SANTIAGO, Region Metropolitana, Chile
Saturday, November 05, 2011 at 01:49:19 UTC
Saturday, November 05, 2011 at 12:49:19 PM at epicenter
Time of Earthquake in other Time Zones
Location 18.293°S, 168.309°E
Depth 39.5 km (24.5 miles)
Region VANUATU
Distances
61 km (37 miles) S of PORT-VILA, Efate, Vanuatu
172 km (106 miles) NW of Isangel, Tanna, Vanuatu
328 km (203 miles) SSE of Luganville, Espiritu Santo, Vanuatu
1869 km (1161 miles) ENE of BRISBANE, Queensland, Australia
The iceberg started out as a surface crack in the sheet of ice, which is located in front of the Pine Island Glacier (PIG) in the Antarctic region.
The rift, which was first noticed in October, runs for almost 20 miles from end to end and is thought to be 200ft deep.
With the crack widening every day, the iceberg will be formed - or 'calved' as it is scientifically known - when it breaks away from the floating ice mass.
This is expected to take place at the end of the year or in early 2012.














