Draft:Wrede Creek
Creek and ultramafic complex in BC, Canada
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{{subst:AfC submission/coi|$1}}
| Wrede Creek | |
|---|---|
  Wrede Creek Location of the mouth of Wrede Creek at the Ingenika River | |
| Etymology | Bernhard "Ben" Wrede |
| Location | |
| Country | Canada |
| Province | British Columbia |
| District | Cassiar District |
| Physical characteristics | |
| Mouth | |
• location | Ingenika River |
• coordinates | 56°47′19″N 125°42′01″W |
| Basin features | |
| Progression | Ingenika River → Williston Lake → Peace River → Slave River → Great Slave Lake → Mackenzie River → Beaufort Sea |
Submission declined on 17 April 2026 by Namita Tudu (talk).
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Submission declined on 31 March 2026 by ChrysGalley (talk). This draft appears to be generated by a large language model (such as ChatGPT). You cannot use LLMs to generate article content.
Declined by ChrysGalley 17 days ago.LLM-generated pages with the below issues may be deleted without notice. These tools are prone to specific issues that violate our policies:
Instead, only summarize in your own words a range of independent, reliable, published sources that discuss the subject. See the advice page on large language models for more information. | |
Comment: We can't accept drafts written by LLM, see WP:NEWLLM. ChrysGalley (talk) 14:48, 31 March 2026 (UTC)
Wrede Creek is a tributary of the Ingenika River in the Cassiar District of northern British Columbia, Canada. It flows through the Omineca Mountains and is part of the Arctic Ocean drainage basin.
History and Etymology
The creek is named for Bernhard "Ben" Wrede, a German born trapper. In 1896, Wrede set out on an expedition and had disappeared. In the next year, Wrede's remains and camp were found at the creek.[1]
The name was officially recorded between 1912 and 1914 by Frank Swannell, a British Columbia Land Surveyor (BCLS), during his surveys of the Cassiar Land District. [1]
Geology
The Wrede Creek ultramafic complex is a zoned body situated within the Upper Triassic Takla Group volcanic rocks. K-Ar dating of hornblende pegmatite within the dunite core had ages of 219 ± 10 Ma to 225 ± 6 Ma. Secondary biotite from similar hornblende dated to 175 ± 6 Ma. These ages correlate to Middle-High Jurassic plutonism.[2]
Geography
Wrede Creek originates in the Omineca Mountains and flows generally eastward. It joins the Ingenika River. Its waters eventually reach the Beaufort Sea via the Peace and Mackenzie river systems.[1]
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