Fremrinámur sits in one of Iceland's most remote and least-traveled areas, the northeast highlands. It is part of the Northern Volcanic Zone, the volcanic belt that runs through north Iceland. Few visitors make the journey; those who do find geothermal features and volcanic landscapes with no tourism infrastructure at all.
One system, several volcanic features
The Smithsonian profile describes a system containing the Ketildyngja shield and the Sveinar fissure swarm, which extends toward the north coast. Its latest confirmed eruption is listed at approximately 1200 BCE, associated with Búrfellshraun; an 1823 report is explicitly discredited.
That makes the volcanic-system name more useful than treating Fremrinámur as a single cone. The catalogue does not establish a visitor route. Identify the exact feature and a permitted approach before planning a journey.