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New Destiny Mining Results for Airborne LiDAR Survey at Treasure Mountain Silver Property Tulameen, BC
Vancouver, British Columbia--(Newsfile Corp. - July 9, 2024) - New Destiny Mining Corp. (TSXV: N...
About this update from New Destiny Mining Corp.
[{"type":"text","content":"\nNew Destiny Mining Results for Airborne LiDAR Survey at Treasure Mountain Silver Property Tulameen, BCVancouver, British Columbia--(Newsfile Corp. - July 9, 2024) - New Destiny Mining Corp. (TSXV: NED), (the \"Company\" or \"NED\") announces that it has conducted an initial interpretation of the results from a LiDAR survey completed at its Treasure Mountain North property, located near Tulameen in southern British Columbia. The survey was conducted last season and a preliminary interpretation was completed by the company's technical staff.Figure 1. LiDAR DEM and features identified with rose diagrams of the different types of lineamentsTo view an enhanced version of this graphic, please visit:https://images.newsfilecorp.com/files/5001/215977_77863e3d3454ebeb_001full.jpgThe Treasure Mountain North property sits within the Intermontane Belt, which hosts several past and current producing gold, silver, lead, zinc and/or molybdenum mines. The property shows multiple types of mineralization that includes, polymetallic veins, gold-bearing quartz veins, and porphyry-related mineralization.A helicopter-borne LiDAR survey was completed over an area of 108.2 km2 at the Treasure Mountain North property in 2022 (Figure 1). The survey resulted in two products: a digital elevation model (DEM) and an orthophoto mosaic. The purpose of the survey was to obtain a high-resolution topographic base and updated orthophotos of the area. The DEM was used to identify lineaments related to geological and geomorphological features. Figure 2. Image of the orthomosaic from the LiDAR survey showing lineaments identifiedTo view an enhanced version of this graphic, please visit:https://images.newsfilecorp.com/files/5001/215977_77863e3d3454ebeb_002full.jpgLineaments were identified using a combination of the 1 m resolution DEM (Figure 1) and the 10 cm resolution orthomosaic (Figure 2). The lineaments were interpreted to be either faults/fractures or traces of bedding and associated fold axis (Figure 1). The bedding traces show a dominant trend of NW-SE and a secondary trend of NNW-SSE, these bedding traces can be readily identified on the orthomosaic and even some fold axis have been determined that have a similar NW-SE trend (Figure 1). The faults and/or fractures identified by this dataset show a contrasting trend, with a dominant NE-SW trend (Figure 1). \"...