Au Gold Corp. (V:AUGC)
Business Focus: Gold Mining
Insider Filings
Latest 10 SEDI filings for AUGC within the last 6 months
See all filings within the past 6 months
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Company News
Feb 06, 2024 14:15 ET
Au Gold Corp Announces Director Resignation
Vancouver, British Columbia
– TheNewswire -- February 6, 2024 –
Au Gold Corp (TSXV:AUGC) (“AUGC” or the
“Company”) announces that founding director
Garrett Ainsworth has resigned from the Board of the Company to allow
him to focus on his main role.
Jan 22, 2024 07:00 ET
Au Gold Corp Provides Ponderosa Update and Displays Core and AME RoundUp Conference
Vancouver, British Columbia
– TheNewswire - January
22, 2024 – Au Gold Corp
(TSXV:AUGC) (“AUGC” or the
“Company”) is pleased to provide an update on
its Ponderosa Gold Project, located near Merritt, BC.
Valuation Ratios
Industry
Sector
Beta
3.61
--
--
Price to Sales - TTM
--
3.74
4.48
Price to Book - most recent quarter
0.38
2.10
1.97
Price to Cash Flow per share - TTM
--
10.40
9.54
Price to Free Cash Flow per share - TTM
--
26.23
19.74
Short Report
| Date | Number of Shares Shorted | Net Change |
|---|---|---|
| Mar 15, 2024 | 57 | -1,165 |
| Feb 29, 2024 | 1,222 | 551 |
| Feb 15, 2024 | 671 | 290 |
Business Summary
| Sector: Basic Materials | Industry: Gold |
Au Gold Corp. is a Canada-based early-stage gold exploration company. The Company is focused on the Ponderosa property, located approximately 20 kilometers (km) southwest of Merritt, BC, within the Spences Bridge Gold Belt. The property consists of four contiguous mineral claims covering an area of 1.8 km by 2.3 km (420 hectares). The Tomahawk Zone property area is identified through historical prospecting as a quartz rubble pile roughly three meters in diameter. The Flat Iron Zone is situated approximately 100 meters south of the Tomahawk Zone. The T-Bone Zone is situated approximately 200 meters northeast of the Tomahawk Zone and represents the coincident gold-arsenic soil geochemistry on the property aside from Axel Ridge. The Rib Eye Zone has narrow excavation that exposed a zone of hydrothermally altered volcanic strata completely converted to orange, white and tan clay with intermittent clear and white silica veinlets.
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