Legalectric

This is the “artist’s conception” of the PurGen coal gasification plant proposed for Linden, New Jersey.

Last week there was an earthquake just off the cost of New Jersey and New York:

Small earthquakes in N.J. prompt calls to police, but no reported damages

Small earthquake off New Jersey felt on east coast

The US Geological Survey has a site to report earthquakes:

DID YOU FEEL IT?

What does this Linden coal gasification plant have to do with an earthquake?   Well DUH, PurGen wants to pump the earth full of CO2.  They claim that “Carbon dioxide will then be removed from the gas and safely stored offshore in a permanent repository.”

In support of this nonsense, they’re trotting out our friend from the Mesaba Project, Dan Schrag:

Storage of Carbon Dioxide in Offshore Sediments

For information on impact of gas storage on seismic activity, check out “Gas Migration” which is THE source for the real poop.  In short, pumping the earth full of gas, i.e. CO2, triggers seismic activity, CCS = earthquakes.

What’s interesting to me is that this is the second time this year for New Jersey:

Earthquake Jolts New Jersey
By Therese Crowley
2/22/2010

BERNARDSVILLE, NJ – Sunday morning reverie at 8:59 a.m. was punctuated by a big BOOM in Bernardsville- and Basking Ridge- and at least 25 more zip codes, according to the US Geological Survey. Within an hour, an earthquake measuring 2.6 on the Richter scale was confirmed by the Lamont Doherty cooperative Seismographic Network (LCSN). The quake was centered at Peapack and Gladstone, New Jersey, 13 miles WSW of Morristown.

In Bernardsville, the quake was experienced as a ‘boom. BOOM!!! shake.’ In this reporter’s old stone cottage, the shaking rang bells. The quake shook Bernardsville Police headquarters, where Dispatcher 35 was fielding calls from residents, and cautioning that an aftershock may follow. Some 100 residents called in the first hour. No damage was immediately reported, although an earthquake of mild magnitude can cause hairline cracks in structures.

The region sits on the Ramapo Fault Line, and Lamont Doherty estimates the depth of the quake at 3.1 miles, measuring the impact as mild, at ll-lV level intensity. Still, residents were excited and rattled. The first aftershock followed at 12:31pm, measuring 2.3 on the Richter scale. As with the original quake, the first alert of something happening within the earth was a booming rumble, followed by a shaking sensation. The first aftershock was centered just one mile from the morning tremor.

The quake was the talk of the Somerset Hills YMCA; many people felt it, but few had heard confirmation of the event. One Dad reported, ‘We were watching TV with the kids and heard the boom—I made them turn the TV down, and we listened and felt the shake. It was something!’

The Sunday morning earthquake follows a series of tremors that moved the ground in Far Hills and Bernardsville from Friday, February 5th to Sunday, February 7th. One of those quakes measured 1.2, but Sunday morning’s 2.6 is orders of intensity greater.

An aftershock took place around 12:30 p.m. on Sunday measuring 2.3 on the richter scale.

Residents who would like to report their experience can go to the US Geological Survey Website and fill out the ‘Did You Feel It?’ form, at http://earthquake.usgs.gov/earthquakes/dyfi/