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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).
Delectability of objects in the ground depends upon their size, shape,
and orientation relative to the antenna, contrast with the host
medium,
as well as radio frequency noise and interference's. This is
representative
but greatly oversimplified: see tutorial.
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