Sentence examples for eruption n from inspiring English sources

The number of buildings impacted during the Fogo eruption (n = 260) is comparable to most recent impacts (in the hundreds), however, there are relatively few recent examples of lava flows that have destroyed such a large proportion of a community's buildings and infrastructure (Table 1).

During follow-up, 16 children were excluded from the study due to missed appointments (n = 5), parents' decision not to continue participating (n = 6), absence of tooth eruption (n = 3) or change in the place of residence (n = 2) (Fig.  1).

Thirty two skin samples were tested; 20 inflammatory skin lesions with the following clinical and pathological diagnoses: Atopic/nummular Dermatitis n = 7, Drug eruption n = 2, Psoriasis n = 1, Allergic contact dermatitis n = 1 and Cutaneus T-cell Lymphoma (Mycosis Fungoides) n = 9. 12 Normal skin samples were collected at the Chaim Sheba Medical Center.

Patients reported some beneficial changes, including decreased fatigue (N = 8), decreased headache (N = 2), decrease in eczematous eruptions (N = 1).

The events recorded most frequently were skin infections (n = 33), eczema (n = 20), and drug-related eruptions (n = 15).

The first data is the famous Old Faithful Geyser eruption data (n = 272) obtained from Härdle (1991, p. 201).

These three eruptions occurred at Etna (n = 2) and Vulcano (n = 1), Italy, which lie in the 'Cradle of Volcanology', aptly named due to the availability of written records dating back to 1500 BC (Siebert et al. 2010).

The eruptive history of Towada is divided into pre-, syn-, and post-caldera stages (Hayakawa 1985); the large caldera-forming eruptions occurred during Episodes N (36 ka) and L (15.5 ka), which emplaced the Ofudo and Hachinohe Ignimbrites, respectively.

An eruption occurred during the year n has an associated ΔLODeff = ΔLO Dn−1 − ΔLO D n−2

In spring 2010, eruptions of Eyjafjallajökull volcano (63.63° N, 19.62° W) in Iceland had a major impact on aviation because ash from the April May summit eruption was transported with northwesterly winds toward Europe and the North Atlantic.

where λ i is the large-eruption rate of volcano i, and λ :=λ 1+⋯+λ n, the global large-eruption rate; these rates are taken to be constant in time see the next paragraph for the generalisation.