Walkabout Resources Ltd
ASX:WKT
Walkabout Resources Ltd
Walkabout Resources Ltd. is a mineral exploration company. The company is headquartered in Perth, Western Australia. The company went IPO on 2006-11-07. The firm is focused on discovering and developing a range of products, such as graphite, gold, base metals, and lithium. Its projects include the Lindi Jumbo Graphite project, Eureka Lithium project, and United Kingdom project. The Lindi Jumbo Graphite Project is situated in south-eastern Tanzania, approximately 200km from the port of Mtwara. The Eureka Lithium project includes two exploration prospecting licenses EPL’s 6308 and 6309 located in the extreme south of Namibia approximately 25 kilometers north of the Orange River and the border of South Africa. In the United Kingdom project, the Company is managing two main exploration joint ventures, one in Northern Ireland and the other in Scotland. In Northern Ireland and Scotland are several geological terranes bound by regional-scale faults that are interpreted to have controlled mineralized fluid flow in the region.
Walkabout Resources Ltd. is a mineral exploration company. The company is headquartered in Perth, Western Australia. The company went IPO on 2006-11-07. The firm is focused on discovering and developing a range of products, such as graphite, gold, base metals, and lithium. Its projects include the Lindi Jumbo Graphite project, Eureka Lithium project, and United Kingdom project. The Lindi Jumbo Graphite Project is situated in south-eastern Tanzania, approximately 200km from the port of Mtwara. The Eureka Lithium project includes two exploration prospecting licenses EPL’s 6308 and 6309 located in the extreme south of Namibia approximately 25 kilometers north of the Orange River and the border of South Africa. In the United Kingdom project, the Company is managing two main exploration joint ventures, one in Northern Ireland and the other in Scotland. In Northern Ireland and Scotland are several geological terranes bound by regional-scale faults that are interpreted to have controlled mineralized fluid flow in the region.
