Malter River

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Geography 🔗

Source 🔗

The Malter River originates from the Western Maltreks' extensive karst aquifer system. After its tributaries combine into the main channel, the river flows visibly for only a few miles across the highland valley floor. At the valley's end, it encounters massive limestone formations where it disappears underground, continuing its journey through vast cave systems. This underground river network eventually feeds into the extensive Rannek karst system, creating one of Senera's largest subterranean watersheds.

Course 🔗

The river's visible course, though brief, is characterized by deep, clear pools and swift rapids. Its disappearance point, locally known as the Great Swallow, marks where the river plunges into a massive cave mouth, creating a spectacular waterfall during high flow seasons.

Parent Location
The Maltreks	Malter River
Malterdale	Malter River
Western Lowlands	Malter River Malterdale Rannek Marches
Senera	Brams River The Maltreks Gulf of Inespell The Narrows Port Surrey-on-the-Brams Eastonton Ranterg Mountains Surrey-on-the-Brams Great Surrey Reach Mt Thraltor Malter River Eastern Senera Aitarel River Tidemark Malterdale Rannek Marches The Admiralty's Helm
Location Type
river	Brams River Loasnah Potam Malter River Aitarel River River Diber Samain River Dustain River