Samaranta Mining Corporation (TSX VENTURE:SAX) ("Samaranta") announces it has
commenced a tightly spaced 501 line kilometer Magnetometer and Gamma
Spectrometer survey on four separate blocks, including the Guadalupe property,
located adjacent to the northern boundary of the Frontino Gold Mines in
Antioquia, Colombia.


Samaranta engaged the services of MPX Geophysics of Markham Ontario ("MPX") to
undertake the Helicopter Magnetometer and Gamma Spectrometer (Radiometrics)
survey. The survey consists of 501 line kilometers in east-west direction at 75
meter line spacing covering four separate blocks all of which are located in the
Segovia batholith within the area of Frontino Gold Mines.


The purpose of the survey is to develop an understanding of the structure and
alteration on Samaranta's properties. In particular, the geological similarities
and or the possible extension of Frontino Gold Mines on to the Guadalupe
concessions. Samaranta intends to undertake a detailed geophysical
interpretation of the Magnetometer and Gamma Spectrometer survey once the final
data is received.


Dr. Volkmar Hable President and CEO of Samaranta stated, "The airborne survey
will develop areas of interest and give us a clear idea of structural trends of
the quarts veins on the Guadalupe property. When the interpretation is completed
Samaranta will immediately start the process of generating viable drill targets
by mobilizing crews to undertake trenching and geological sampling."


About Samaranta:

Samaranta's key asset is the Guadalupe property that is strategically located on
the northern boundary of the Frontino Gold Mine ("FGM"). FGM has been in
production since about 1852 with recorded production totaling about 4.6 million
ounces. Both Guadalupe and FGM are underlain primarily by the same granodioritic
rocks of the Segovia batholith. The Segovia Gold Belt is a region of
granodioritic rocks measuring approximately 300 km in length by up to 75 km in
width defined by a strong fault zone system trending approximately north-south.
Gold mineralization within this belt is primarily associated with quartz veins
and narrow vein swarms that are spatially related to the major north to
northeast trending fault structures.


Technical information in this news release has been reviewed by Derrick
Strickland, P.Geo., a qualified person as defined in NI 43-101.


SAMARANTA MINING CORPORATION

Volkmar Hable, President

Visit our website at www.samaranta.ca.

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