Summary of Physical and Chemical Characteristics
of the Focus Arc-Trench Systems


This is an evolving compilation/worksheet; those wishing to add or correct information should contact the Editors for this section Gray Bebout and Tim Elliott.
Sources of Data:
Jarrard (1986); von Huene and Scholl (1991, 1996); Kirby et al. (1991, 1996); Plank and Langmuir (1998).

Arc-Trench
System
Convergence
Rate (mm/year)
Age of Subducting
Oceanic Lithosphere (Ma)
Thermal
Parameter (Phi)**
Sediment
Thickness (m)
Sediment
Type(s)
Sediment Confidence
Level (1-5)†
Izu-Bonin-Mariana (IBM)
Izu-Bonin 50 135   ~600 drilling planned 1999 4
Mariana 47.5 165   400-500 pelagic brown clay, chert and porcellanite ± limestone volcaniclastic turbidites 1
Central America (w/Mexico)
Central America 77
(70-90)
22-23>   425 hemipelagic, diatome-rich mud, pelagic carbonate 1
Mexico 52 15   200 hemipelagic muddy silt, brown pelagic clay  
Tonga
Tonga 164-240 120 ± 20   <100 pelagic brown clay, chert, porcellanite (Site 595/596) 1
Aleutians
Aleutians 62 54 (50-65)   350 diatom ooze, greenish gray clay, silty clay 1
Cascadia
Cascadia 35 8   1500 volcaniclastic fan deposits and more distal turbidites 4
Banda
Banda 67 ~160   500-900 carbonate turbidites clay, radiolarian clay 1
Lesser Antilles
N. Antilles 24 68   200- 1000's ashy mud, radiolite clay, zeolite clay, and calc, ferruginous claystone 2
S. Antilles 24 68   1750    
Andes
Peru 100 45   125 clay, brown pelagic clay (Site 321) silicic green clay, nanno ooze 3
North Chile 100 82     ? 5
Central Chile 98 48     ? 5
South Chile 97 40-5     ? 5

**Thermal parameter from Kirby et al. (1991, 1996). Phi = (age of subducting lithosphere) x (vertical descent rate).
Sediment confidence levels from Fig. 14 of Plank and Langmuir (1998).