This two-part article comprises brief introductions to (1) volcanism and its products in general and to the broad pattern of Quaternary volcanism and tephrostratigraphy in North Island, and (2) the ensuing tephra-derived soils of North Island. Part 1 derives mainly from Smith et al. (2006), Leonard et al. (2007), and Lowe (2008a). Other useful reviews include those of Neall (2001), Graham (2008: Chapter 7), Wilson et al. (2009), and Cole et al. (2010). Recent reviews on tephras include Shane (2000), Alloway et al. (2007), Lowe (2008b, 2011), and Lowe et al. (2008a, 2008b). A history of tephra studies in New Zealand was reported by Lowe (1990). Part 2 describes the distribution and character of the main tephra-derived soils, these being Enti...
The genesis of soils developed in either tephra or loess on stable sites differs markedly from that ...
The stratigraphic relationships and distribution of 36 named late Quaternary (≤c. 50 000 yr B P.) si...
Tephras provide one of the most reliable methods of time control and synchronisation within Quaterna...
This two-part article comprises brief introductions to (1) volcanism and its products in general and...
During the Quaternary, much of central North Island, New Zealand, was repeatedly overwhelmed or modi...
During the Quaternary, much of central North Island, New Zealand, was repeatedly overwhelmed or modi...
The development of volcanic "ash" studies in New Zealand can be traced through three broad periods (...
In this article, I show how an Ultisol, representative of a globally-important group of soils with c...
This paper summarises the occurrence and distribution of late Quaternary tephras in the Hamilton (Mi...
In this article, I show how an Ultisol, representative of a globally-important group of soils with c...
This paper summarises recent studies on Quaternary tephra deposits in New Zealand, and refers to a r...
The development of tephra studies in New Zealand may be divided into four main periods: Period 1, la...
Studies on distal airfall tephra layers preserved in lake sediments and peats in northern New Zealan...
ABSTRACT: The clay mineralogy of a sequence of 36 andesitic ephra nd associated paleosols dating fro...
The genesis of soils developed in either tephra or loess on stable sites differs markedly from that ...
The stratigraphic relationships and distribution of 36 named late Quaternary (≤c. 50 000 yr B P.) si...
Tephras provide one of the most reliable methods of time control and synchronisation within Quaterna...
This two-part article comprises brief introductions to (1) volcanism and its products in general and...
During the Quaternary, much of central North Island, New Zealand, was repeatedly overwhelmed or modi...
During the Quaternary, much of central North Island, New Zealand, was repeatedly overwhelmed or modi...
The development of volcanic "ash" studies in New Zealand can be traced through three broad periods (...
In this article, I show how an Ultisol, representative of a globally-important group of soils with c...
This paper summarises the occurrence and distribution of late Quaternary tephras in the Hamilton (Mi...
In this article, I show how an Ultisol, representative of a globally-important group of soils with c...
This paper summarises recent studies on Quaternary tephra deposits in New Zealand, and refers to a r...
The development of tephra studies in New Zealand may be divided into four main periods: Period 1, la...
Studies on distal airfall tephra layers preserved in lake sediments and peats in northern New Zealan...
ABSTRACT: The clay mineralogy of a sequence of 36 andesitic ephra nd associated paleosols dating fro...
The genesis of soils developed in either tephra or loess on stable sites differs markedly from that ...
The stratigraphic relationships and distribution of 36 named late Quaternary (≤c. 50 000 yr B P.) si...
Tephras provide one of the most reliable methods of time control and synchronisation within Quaterna...