The impact of the 1783–1784 AD Laki eruption on global aerosol formation processes and cloud condensation nuclei [PDF]
The 1783–1784 AD Laki flood lava eruption commenced on 8 June 1783 and released 122 Tg of sulphur dioxide gas over the course of 8 months into the upper troposphere and lower stratosphere above Iceland. Previous studies have examined the impact of the
Carslaw, K. S. +13 more
core +2 more sources
Geoarchaeological tsunami deposits at Palaikastro (Crete) and the Late Minoan IA eruption of Santorini [PDF]
The explosive eruption at Santorini in the Aegean Sea during the second millennium BCE was the largest Holocene volcanic upheaval in the Eastern Mediterranean region.
Bruins, Hendrik J., +19 more
core +2 more sources
Volcano-ice interactions at Prestahnukur, Iceland : rhyolite eruption during the last interglacial-glacial transition. [PDF]
Prestahnukur is a 570m high rhyolite glaciovolcanic edifice in Iceland's Western Rift Zone with a volume of 0.6 km3. Uniform whole rock, mineral and glass compositions suggest that Prestahnukur was constructed during the eruption of one magma batch.
McGarvie, David W. +4 more
core +5 more sources
Atmospheric impact of the 1783-1784 Laki Eruption: Part II - Climatic effect of sulphate aerosol [PDF]
The long 1783-1784 eruption of Laki in southern Iceland, was one of the first eruptions to have been linked to an observed climate anomaly, having been held responsible for cold temperatures over much of the Northern Hemisphere in the period 1783-1785.
Highwood, E. J. +7 more
core +2 more sources
Cutaneous larva migrans in children: A case series from Southern India
Cutaneous larva migrans or creeping eruptions is a parasitic skin infection caused by hookworm larva. It is common in warmer tropical and subtropical countries.
Indira Subhadarshini Paul +1 more
doaj +1 more source
Cutaneos larva migrans in travelers [PDF]
The symptoms, medical history, and treatment of 98 patients with cutaneous larva migrans (creeping eruption) who attended a travel-related-disease clinic during a period of 4 years are reviewed.
Nothdurft, H. D. +3 more
core +1 more source
Unusual presentations of cutaneous larva migrans
Cutaneous larva migrans (also known as creeping eruption, sand worm eruption, plumbers itch, duck hunters itch) is caused by penetration of skin by third-stage larvae of animal hookworms; first reported by Lee in 1874.
Anca Chiriac +8 more
doaj +1 more source
Modeling the distribution of the volcanic aerosol cloud from the 1783–1784 Laki eruption [PDF]
We conducted simulations of the atmospheric transformation and transport of the emissions of the 1783–1784 Laki basaltic flood lava eruption (64.10°N, 17.15°W) using the NASA Goddard Institute for Space Studies modelE climate model coupled to a sulfur ...
Alan Robock +13 more
core +1 more source
Atmospheric and environmental effects of the 1783-1784 Laki eruption: A review and reassessment [PDF]
The 1783–1784 Laki flood lava eruption in Iceland emitted ∼122 megatons (Mt) SO2 into the atmosphere and maintained a sulfuric aerosol veil that hung over the Northern Hemisphere for >5 months. The eruption columns extended to 9–13 km and released ∼95
Thordarson, Thorvaldur, Self, Stephen
core +1 more source
Creeping Eruption and Intestinal Strongyloidiasis [PDF]
exaly +3 more sources

