ALBA MINERALS INC
TSXV
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AA

AA
ALBA MINERALS INC
CA Flag
TSXV
 
Next Earning
Market Cap
EPS
Div Yield
P/E
Next Earning
Market Cap
EPS
Div Yield
P/E

AA Stock Chart

Financials

Valuation
Enterprise Value/EBITDA, TTM
Enterprise Value, FQ
Market Cap — Basic
Number of Employees
Number of Shareholders
Price/Earnings, TTM
Price/Revenue, TTM
Price/Book Ratio, FY
Price/Sales Ratio, FY
Balance Sheet
Current Ratio, FQ
Debt to Equity, FQ
Net Debt, FQ
Quick Ratio, FQ
Total Assets, FQ
Total Debt, FQ
Operating Metrics
Return on Assets, TTM
Return on Equity, TTM
Return on Invested Capital, TTM
Revenue per Employee, TTM
Price History
Average Volume (10 day)
Beta - 1 Year
Price - 52 Week High
Price - 52 Week Low
Dividends
Dividends Paid, FY
Dividends per Share, FY
Expected Annual Dividends
Dividends Yield
Margins
Net Margin, TTM
Gross Margin, TTM
Operating Margin, TTM
Pretax Margin, TTM
Income Statement
Basic EPS, Net Income
Earnings per Share, Basic, TTM
EBITDA, TTM
Gross Profit, FY
Last Annual EPS
Last Annual Revenue, FY
Net Income, FY
Total Revenue, FY
Free Cash Flow, TTM

Profile

Sector: Basic Materials
Industry: Gold
Employees: ---
Alba Minerals Ltd., formerly Acrex Ventures Ltd., is a Canada-based company, which is engaged in sourcing and exploration of mineral properties in North America. The Company is engaged in the acquisition, exploration and development of mineral properties segment. It focuses on the development of gold, platinum group metals (PGM's) and base metals properties. The Company, through its subsidiary, Acrex Minerals (U.S.) Inc., owns the Rainbow Canyon property, which is located approximately 40 kilometers east of Reno, in Washoe County, Nevada, the United States. It holds approximately five claims, which cover an area of over 40 hectares. The Company focuses on undertaking a program of geological mapping, geochemical sampling, geophysical surveying, trenching and sampling to prepare the property for an initial drill program. The Rainbow Canyon property is situated within the Walker Lane structural belt, and is underlain by mafic to felsic volcanic rock of Tertiary age.

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