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Oil and Gas at Your Door? (2005 Edition) - Earthworks

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<strong>Oil</strong> <strong>and</strong> <strong>Gas</strong> Development <strong>and</strong> Impacts<br />

1. EXPLORATION<br />

Only after minerals have been leased (or permission obtained from mineral owners) may an<br />

individual or company go out onto the l<strong>and</strong> to explore for oil <strong>and</strong> gas deposits.<br />

Remote sensing techniques, such as photography, radar, infrared images, <strong>and</strong> microwave frequency<br />

receivers, are used to identify potential production areas <strong>and</strong> predict the likelihood of<br />

significant reserves. 33 Geophysical explor<strong>at</strong>ion is the <strong>at</strong>tempt to physically loc<strong>at</strong>e oil or gas-bearing<br />

geological structures. The mostly widely used technique in on-shore geophysical explor<strong>at</strong>ion<br />

is the seismic test. 34<br />

Seismic Explor<strong>at</strong>ion<br />

Seismic tests are based on the fact th<strong>at</strong> acoustic or seismic waves will travel through, bend,<br />

absorb, <strong>and</strong> reflect differently off of various layers of subsurface rock. Seismic waves can be<br />

gener<strong>at</strong>ed in several ways:<br />

1. by blasting dynamite from a hole drilled several hundred feet in the ground;<br />

2. by dropping a heavy weight, known as a thumper, from a truck (called a thumper truck)<br />

onto hard ground surfaces such as paved roads. This technique is known as l<strong>and</strong> vibroseis,<br />

<strong>and</strong> it is typically used near popul<strong>at</strong>ed areas <strong>and</strong> in sensitive environmental areas<br />

where explosions are not desirable; 35 or<br />

3. by shaking the ground with a device known as a vibrasizer.<br />

Seismic waves travel downward <strong>and</strong> outward, <strong>and</strong><br />

are reflected back <strong>at</strong> different r<strong>at</strong>es <strong>and</strong><br />

strengths, depending upon the underground<br />

structures encountered. The strength <strong>and</strong> timing<br />

of the reflected signals are measured <strong>at</strong> the surface<br />

by geophones, which are connected to a line<br />

laid along a predetermined course. The line is<br />

connected to a machine th<strong>at</strong> records the signals.<br />

In the 1990s, geologists began using high-powered<br />

computers th<strong>at</strong> could analyze much<br />

gre<strong>at</strong>er numbers of seismic signals <strong>and</strong> display<br />

them on three-dimensional (3-D) maps. To<br />

increase the detail <strong>and</strong> accuracy of these 3-D<br />

maps, the seismic lines <strong>and</strong> geophones are<br />

spaced more closely together, which means th<strong>at</strong><br />

l<strong>and</strong> disturbance also increases. 36<br />

FIGURE I-2. SEISMIC EXPLORATION<br />

30-ton thumper trucks leave lasting impressions on the<br />

surface.<br />

Seismic Explor<strong>at</strong>ion—Issues <strong>and</strong> Impacts<br />

• Survey stakes for mapping out the explor<strong>at</strong>ion area should be wooden, <strong>and</strong> not wire pin<br />

flags, because farming activities like making silage or hay can shred the wire flags. The<br />

resultant metal bits can kill livestock th<strong>at</strong> e<strong>at</strong> the feed. Also, all stakes <strong>and</strong> markers should<br />

be removed after explor<strong>at</strong>ion is completed, because livestock <strong>and</strong> wildlife can die from<br />

e<strong>at</strong>ing ribbons or flags. 37<br />

• Seismic lines will destroy veget<strong>at</strong>ion <strong>and</strong> may cause erosion, which could lead to sediment<br />

entering surface w<strong>at</strong>ers. 38<br />

• 3-D tests tend to cause gre<strong>at</strong>er surface disturbance <strong>and</strong> companies use your l<strong>and</strong> for<br />

longer periods of time than with two-dimensional surveys.<br />

I-6

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