Large amounts of natural gas, composed mainly of methane, can occur in
arctic sedimentary basins in the form of gas hydrates under appropria
te temperature and pressure conditions. Gas hydrates are solids, compo
sed of rigid cages of water molecules that trap molecules of gas. Thes
e substances are regarded as a potential unconventional source of natu
ral gas because of their enormous gas-storage capacity. Most published
gas hydrate resource estimates are highly simplified and based on lim
ited geological data. The gas hydrate resource assessment for northern
Alaska presented in this paper is based on a ''play analysis'' scheme
, in which geological factors controlling the accumulation and preserv
ation of gas hydrates are individually evaluated and risked for each h
ydrate play. This resource assessment identified two gas hydrate plays
; the in-place gas resources within the gas hydrates of northern Alask
a are estimated to range from 6.7 to 66.8 trillion cubic metres of gas
(236 to 2,357 trillion cubic feet of gas), at the 0.50 and 0.05 proba
bility levels respectively. The mean in-place hydrate resource estimat
e for northern Alaska is calculated to be 16.7 trillion cubic metres o
f gas (590 trillion cubic feet of gas). If this assessment is valid, t
he amount of natural gas stored as gas hydrates in northern Alaska cou
ld be almost seven times larger then the estimated total remaining rec
overable conventional natural gas resources in the entire United State
s.