Mount Mageik

{{Infobox mountain

| name = Mount Mageik

| photo = MountMageik.jpg

| photo_caption = Mount Mageik (left) and Mount Martin (right)

| elevation_ft = 7101

| elevation_ref = {{cite gvp|vnum=312150|name=Mageik|accessdate=2020-09-09}}

| prominence_ft = 4449

| prominence_ref= [https://www.peakbagger.com/peak.aspx?pid=394 Peakbagger.com, Mount Mageik, Alaska], Retrieved Jan. 6, 2023.

| range = Aleutian Range

| parent_peak =

| listing = List of mountains of Alaska

| location = Katmai National Park and Preserve, Alaska, USA

| coordinates = {{coord|58|11|44|N|155|15|13|W|type:mountain_scale:100000|format=dms|display=inline,title}}

| coordinates_ref = {{cite gnis|id=1405864|name=Mount Mageik|accessdate=2015-01-18}}

| map = Alaska

| topo = USGS Mount Katmai A-4

| type = Stratovolcano

| age = Pleistocene to Holocene

| volcanic_arc = Aleutian Arc

| last_eruption = 500 BCE ± 50 years no

| first_ascent =

| easiest_route =

}}

Mount Mageik {{IPAc-en|m|ə|ˈ|ɡ|iː|k}} is a stratovolcano on the Alaska Peninsula. It has no confirmed historical eruptions (one in 1946 is now deemed questionable), but its youngest eruptive products are apparently Holocene in age (8750 to 500 BCE). A young crater lies on the northeast flank of the central summit cone, and is the site of vigorous superheated fumarolic activity with prominent sulfur deposits. The volcanic cones are composed of andesite, basaltic andesite and dacite.

The volcano is mantled in ash from the 1912 eruption of Novarupta and from the 1953 eruption of nearby Trident Volcano.

File:Map of Alaska Peninsula Volcanoes.gif

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