Ronin Placer Ground-penetrating Radar Survey Report
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1 Ronin Placer Ground-penetrating Radar Survey Report Tenures: , Mining Division: Greenwood NTS Location: 082E/03 Geographic Center Coordinates: UTM Zone 11, E , N Claims Owner: Operator: Consultants: Report Author: Warren Tessari Ronin Exploration Ltd. N/A Warren Tessari Report Submission Date: October 27, 2011 Ronin July 2011 Radar Report Page 1
2 Table of Contents Table of Contents... 2 Introduction... 3 Figure 1: Index Map... 3 Claim and Data Gathering Overview... 4 Radar Equipment, Methods, and Ground Conditions... 6 Data and Diagrams... 7 Figure 2: Sample Radar Data... 7 Figure 3: Plan Map A... 8 July 7 and 12 Ground-penetrating Radar Survey Results... 9 Radar Data Result Table Itemized Cost Statements Statement of Author s Qualifications References Cited in the Report List of Software Programs Used in Support of the Exploration and Development and the Preparation of the Report Appendix A: Radar Data Ronin July 2011 Radar Report Page 2
3 INDEX MAP Introduction Figure 1: Index Map Oliver LOCATION OVERVIEW INSET N Camp McKinney Ronin Placer Claims Osoyoos Bridesville 3 KM A LEGEND Geographic Center Coordinates (UTM Zone 11, E , N ) Ronin Claims Boundaries #### Ronin Tenure Numbers Roads Streams NTS Osoyoos 082E/03 A Plan Map A UTM Zone meters 1: m Contour Spacing Ronin July 2011 Radar Report Page 3
4 Claim and Data Gathering Overview The Ronin Placer Claims encompass the majority of the surface and suspected subsurface drainage systems on the benches above Rock Creek centered roughly on the historic Denver Bar. This area, especially the current path of Rock Creek, has been explored and mined for placer gold for more than a century. In addition, Regional GeoChemical Surveys available online from BCGS Geology also indicated high gold values from soil samples on Rock Creek and several of the streams in the surrounding area. Other factors that contributed to the selection of this area for exploration and development included proximity to roads and power and a lack of conflicting interests. The majority of the claim is not privately owned, although legacy placer claims and mineral claims overlap in some areas especially towards the existing channel of Rock Creek and around the historical War Eagle and Dayton mines. The specific claims covered by this scope of work are owned and operated by Warren Tessari representing Ronin Exploration Ltd. The tenure numbers for the overall group of adjacent claims are and , and they are outlined in red on the index map in this report. The specific claim upon which this investigation was performed was This specific claim is also identified on Plan Map A in this report. Accesses to the claims are via Fish Lake Road on the east side and Mount Baldy Road on the west side of Rock (or Jolly) Creek, approximately 60km east of Osoyoos on Hiway 3. There is a substantial system of non-maintained forestry and mining trails throughout the claims. Access to the area where the radar work was performed in this study is approximately 5.4 km north of Hiway 3 on Fish Lake road. Approximately 4 km of 50 MHz radar data was gathered on July These paths were pre-selected to use the most apparently traversable ground based on readily-available satellite data and pre-data gathering orientation and line layout. Several of the lines go in and out of the claim boundary as larger forestry roads were followed. Ronin July 2011 Radar Report Page 4
5 Approximately 4.5 km of 50 MHz radar data was gathered on July These paths were laid out to be followed as best as possible disregarding terrain where feasible to fill in the blanks from the previous data set. Overall approximately 8.5km of radar data was gathered, in addition to lines gathered during first pass prospecting in October 2010 along Fish Lake Road. The purpose of the Ground-penetrating Radar (GPR) survey was to identify target areas for drilling and gathering of samples from depth to be performed at a later date. Apparent subsurface channels, both current and historical, were noted in the data and transferred to topographic field maps quantitatively using non-differential GPS coordinates attached to the data. Ronin July 2011 Radar Report Page 5
6 Radar Equipment, Methods, and Ground Conditions 50 MHz radar data was gathered by towing the radar transducer across targeted areas by foot. Field markers were placed to correspond with radar line starts and stops, and GPS tracks were gathered with the coordinates embedded in the radar data for future reference and evaluation. For this study the 50MHz Rough Terrain Antenna made by MALÅ Geoscience was used. The transmitter and receiver are both contained in a single, snake-like unit. The system operates at 50MHz with trace spacing based on elapsed time. The X3M/CU-II control module was connected to a Garmin GPS Map 76C to provide continual satellite positioning information for correlation to the radar data. All depth measurements were based on an estimated radar velocity for the expected soil type. For the purposes of this survey, all depths were relative rather than absolute and intended to be verified and corrected in the future through other forms of testing such as drilling. Specifically, depth was indicated by nanoseconds corresponding to the signal travel time to and from the radar unit. Based on the estimated soil conditions, a depth approximation in meters was also provided by the radar unit. Depth was limited overall due to extremely high ground water. The spring and early summer of 2011 had been abnormally wet and subsurface and surface water was apparent in many places. There appears to be an abundance of overlying glacial till in all areas, which is typically excellent material for radar penetration, however water saturation made depth estimates difficult. The topography, as shown on the index map, is variable and slopes overall towards the stream bed of Rock Creek and its tributaries. Both surface evidence and subsurface data indications show mixedsize material ranging from sand, to cobbles to boulders, and varying from very well to very poorly sorted throughout the area. Although penetration was limited overall, indications of subsurface channels were noted in the data. As well, areas of greatest saturation were mapped as supporting evidence for locating subsurface channels. Additional radar data should be gathered later in the season when saturation has diminished somewhat, perhaps during winter when snow is covering deadfall, and when more target areas have been identified based on historical research, soil and silt sampling, etc. Ronin July 2011 Radar Report Page 6
7 Data and Diagrams Figure 2: Sample Radar Data RADAR LINE 77 HYPERBOLAS HORIZONS HORIZONS APPARENT WATER SATURATION This figure is an example of 50MHz radar data gathered during the survey. The salient features include subsurface horizons or layers, apparent water saturation, and hyperbolas indicating features such as boulders or tree roots. The depth in the data is given in nanoseconds, which is the most accurate representation of signal return. Any depth estimates are based on an estimated velocity and are intended to be verified during further testing. Distances along the ground were not taken from legend across the bottom of the data. Real-time GPS tags were employed instead and transferred as waypoints to Garmin MapSource and Google Earth Pro. During to the alluvial drilling/sampling program that will occur based the radar data gathering and analysis, the signatures will be confirmed where possible. Features such as water saturation, larger cobbles and boulders, and reflective layers such as iron/magnetite from old flow channels have corresponded very closely to the interpreted radar data in previous studies in the area. Lines of radar data were gathered for the overall area and in each individual proposed hole location for the placer test drilling program. Based on the data, the proposed hole sites will be adjusted to provide sampling points corresponding to likely subsurface channels. Ronin July 2011 Radar Report Page 7
8 Figure 3: Plan Map A PLAN MAP A: RADAR LINES GATHERED N LEGEND Ronin Placer Claims Contours Fish Lake Road Streams Approximate Geographic Center of Radar Lines: 11 U Radar Data Lines Gathered with Line Numbers (See Appendix A for Data) 1: m Contour Spacing Ronin July 2011 Radar Report Page 8
9 July 7 and 12 Ground-penetrating Radar Survey Results The following results are taken directly from the data files captured by the MALÅ X3M/CU-II control module connected to the Garmin GPS Map 76C. The "Depth" and "Noted Signatures/Indications" columns were added by the radar technician for analysis, and specify the approximate depth to and description of the significant or typical apparent feature described. Lines 79 and 80 ran mostly parallel to the suspected subsurface channels, and the rest of the lines ran roughly perpendicular. Line 80 turns and crosses the suspected main channel, and this shows clearly in the data in that area. In occasional lines, the saturation was consistent enough that comments are made about the line overall, but no other signatures were noted with sufficient distinctive features to mention in this report. In those instances, time and positional data is indicated as "n/a" due to the lack of specific subsurface indications despite careful analysis. The positional data is given in decimal degrees because that is the format stored and exported by the MALÅ X3M/CU-II control module. Ronin July 2011 Radar Report Page 9
10 Radar Data Result Table 3 to 6 Ronin July 2011 Radar Report Page 10
11 Itemized Cost Statements Ground-penetrating Radar (GPR) GPR Technicians and Equipment: (5 $ per day) $ GPR Crew Travel To/From Site/Sherwood Park AB: (24 $ per hour) $ (2048 $1.15 per km) $ Data Analysis and Formatting (16 $90 per hour) $ Meals, 2-Technician Crew: (7 days incl. work and $ per day) $ Communications $74.00 Report Generation $ TOTAL $ Ronin July 2011 Radar Report Page 11
12 Statement of Author s Qualifications This report was prepared by Warren Tessari, Operations Manager and Senior Technician for Maverick Inspection Ltd. Maverick Inspection has extensive experience in specialized non-destructive data gathering including infrared thermography, laser imaging, remote video inspection, and ground-penetrating radar. Mr. Tessari also heads Research and Development at Maverick Inspection Ltd. and for over a decade has been actively creating, applying, and testing radar and other untraditional nondestructive methodologies applicable for aggregate and mineral exploration in Alberta and British Columbia. Additional analysis was performed by Maverick s most experienced radar technician and GPR Department Manager, James Harrison, who has extensive experience with a wide range of radar applications in Canada and abroad including specialized utility locates, facility-wide subsurface locates and mapping, mining applications, forensics and archeology projects, data support for engineering studies, etc. Mr. Harrison specializes in the development of new techniques and methods for data gathering, software-based analysis, and the introduction and testing of radar in new industries and markets. The analysis and interpretation of the data was based on known signatures of subsurface features such as water saturation, changes in subsurface horizons, objects that differentiated from the background, and other known phenomenon. Apparent signatures were noted for further, targeted investigation, and comments were made on the data based on previous experience and technical knowledge of Ground-penetrating Radar. Ronin July 2011 Radar Report Page 12
13 References Cited in the Report There are no specific references cited in this report. BCGS Geology Maps were used as a resource during exploration and correlation of the data. The report pertains to the specific data and field conditions, and it does not rely on previous studies or reports apart from basic map data available online from BCGS. Ronin July 2011 Radar Report Page 13
14 List of Software Programs Used in Support of the Exploration and Development and the Preparation of the Report BCGS Geology Maps Garmin MapSource Google Earth Pro RAMAC Ground Vision Microsoft Word 2007 Ronin July 2011 Radar Report Page 14
15 Appendix A: Radar Data The individual lines of radar data are included below for reference. Each is included in its entire length, but divided where necessary to fit the page. Due to the resolution of the 50 MHz system and the scope of the investigation, the scale as shown should be more than sufficient for a qualified individual to note the pertinent features. There is no Line 76 because it was a start/stop without data. See Figure 3: Plan Map A for the relative positions of each line. RADAR LINE 71 RADAR LINE 72 Ronin July 2011 Radar Report Page 15
16 RADAR LINE 73A RADAR LINE 73B RADAR LINE 74A Ronin July 2011 Radar Report Page 16
17 RADAR LINE 74B RADAR LINE 75A RADAR LINE 75B Ronin July 2011 Radar Report Page 17
18 RADAR LINE 77A RADAR LINE 77B RADAR LINE 78 Ronin July 2011 Radar Report Page 18
19 RADAR LINE 79A RADAR LINE 79B RADAR LINE 80A Ronin July 2011 Radar Report Page 19
20 RADAR LINE 80B RADAR LINE 81A RADAR LINE 81B Ronin July 2011 Radar Report Page 20
21 RADAR LINE 82A RADAR LINE 82B RADAR LINE 83A Ronin July 2011 Radar Report Page 21
22 RADAR LINE 83B RADAR LINE 83C RADAR LINE 84 Ronin July 2011 Radar Report Page 22
23 RADAR LINE 85 RADAR LINE 86 Ronin July 2011 Radar Report Page 23
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