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OUR MAIN GOAL IS TO FIND AND HELP RECOVER POSSIBLE TREASURE ON YOUR PROPERTY.
ARCHEOLOGY, SINK HOLES IN FLORIDA AND OTHER STATES,
CAVES DETECTION, LOST PROPERTY FINDINGS, MAP DOWSING
WE HAVE HELPED HUNDREDS OF PROPERTY OWNERS IN PROJECTS INVOLVED IN TREASURE SEARCH AND RECOVERY.
OVER 20 YEARS EXPERIENCE.
TOP PROFESSIONALS IN THE FIELD OF TREASURE SEARCH AND RECOVERY.
THE BEST ON LAND EQUIPMENT AVAILABLE.
PROFESSIONAL APPROACH TO EVERY PROJECT.
100% PRIVACY ASSURED - WE DO NOT SHARE ANY INFORMATION ON PROPERTY OWNERS WITH ANYONE.
DUE TO GOOD FINDINGS HISTORY WE HAVE BEEN HIRED BY MANY INVESTORS AND CORPORATIONS NEEDED OUR SERVICES.
GROUND PENETRATING RADAR - GPR,
COMPUTER SYSTEMS FOR GPR,
COMPUTER DATA ANALYSES FROM GPR
METAL DETECTORS,
LONG RANGE LOCATORS,
DOWSING OF MAPS BY PROFESSIONAL MAP DOWSERS,
COMPUTER SYSTEMS,
GEOLOGICAL EQUIPMENT
COMPUTER GENERATED MAPS AND DIGITAL IMAGES FROM GPS
OUR MOST FAMOUS EQUIPMENT WE USE IS GROUND PENETRATING RADAR SYSTEM
Ground penetrating radar (GPR, sometimes called ground
probing radar, georadar, subsurface radar, earth sounding radar or "radar
terrestre penetrant") is a noninvasive electromagnetic geophysical technique
for subsurface exploration, characterization and monitoring (history).
It is widely used in locating lost utilities, environmental site characterization
and monitoring, agriculture, archaeological and forensic investigation,
unexploded ordnance and land mine detection, groundwater, pavement and
infrastructure characterization, mining, ice sounding, permafrost, void,
cave and tunnel detection, sinkholes, subsidence, karst, and a host of
other applications. It may be deployed from the surface by hand or
vehicle, in boreholes, between boreholes, from aircraft and from satellites.
It has the highest resolution of any geophysical method for imaging the
subsurface, with centimeter scale resolution sometimes possible.
Resolution is controlled by wavelength of the propagating
electromagnetic wave in the ground. Resolution increases with
increasing frequency (shorter wavelength). Depth of investigation
varies from less than one meter in mineralogical clay soils like montmorillonite
to more than 5,400 meters in polar ice. Depth of investigation increases
with decreasing frequency but with decreasing resolution. Typical
depths of investigation in fresh-water saturated, clay-free sands are about
30 meters. Depths of investigation (and resolution) are controlled
by electrical properties through conduction losses, dielectric relaxation
in water, electrochemical reactions at the mineralogical clay-water interface,
scattering losses, and (rarely) magnetic relaxation losses in iron bearing
minerals. Scattering losses are the result of spatial scales of heterogeneity
approaching the size of the wavelength in the ground (like the difference
between an ice cube and a snowball in scattering visible light).
Detectability of objects in the ground depends upon their size, shape,
and orientation relative to the antenna, contrast with the host medium,
as well as radiofrequency noise and interferences. This is representative
but greatly oversimplified: see tutorial.
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Copyright 2003 SILESIA GROUP INC., all rights reserved.
Copyright © Silesia Group Inc 1994