BEACH CHANGES IN AN EXTENSIVE AREA BETWEEN OTSU FISHING PORT AND TAKADO POINT IN NORTHERN IBARAKI PREFECTURE

Author(s):  
Takaaki UDA ◽  
Takahiro OJIMA ◽  
Michio SUMIYA ◽  
Yasuhiro OKI ◽  
Toshiro SAN-NAMI
2010 ◽  
Vol 40 (3) ◽  
pp. 749-762
Author(s):  
Hirokazu GOTO ◽  
Yuichi HATAYA ◽  
Yasuyuki YOKOTA ◽  
Takeshi MIZUNOYA ◽  
Yoshiro HIGANO

1995 ◽  
Vol 17 (7) ◽  
pp. 338-345 ◽  
Author(s):  
Satoshi MATSUBARA ◽  
Akira KATO ◽  
Fumihiko MATSUYAMA
Keyword(s):  

1987 ◽  
Vol 33 (115) ◽  
pp. 300-310 ◽  
Author(s):  
T.J.H. Chinn ◽  
A. Dillon

Abstract“Whisky Glacier” on James Ross Island, Antarctic Peninsula, comprises anévéand clean ice trunk surrounded by an extensive area of debris-covered ice resembling a rock glacier. The debris-free trunk of the glacier abuts abruptly against the broad, totally debris-covered tongue at a number of concentric zones where debris-laden beds crop out at the surface in a manner similar to the “inner moraine” formations of many polar glaciers.Ice structures and foliation suggest that “Whisky Glacier” is a polythermal glacier which is wet-based under the debris-free zone, and dry-based under the debris-covered zone. It is surmised that the glacier sole crosses the freezing front close to where the basal debris beds are upwarped towards the surface. Here, basal water is confined, and freezes to the under side of the glacier in thick beds of regelation ice which are uplifted to the surface along with the debris-laden beds. Ablation losses effectively cease beneath the blanket of debris covering the tongue.The transition from wet-based to dry-based conditions at the glacier sole is a powerful mechanism for entraining debris into a glacier and, in the case of “Whisky Glacier”, for lifting debris to the surface. It is suggested that this may be a mechanism for forming some polar rock glaciers.


2012 ◽  
Vol 78 (5) ◽  
pp. 348-352 ◽  
Author(s):  
Toshiyuki Usami ◽  
Mizuho Itoh ◽  
Satomi Morii ◽  
Takuya Miyamoto ◽  
Masato Kaneda ◽  
...  

1994 ◽  
Vol 78 (Appendix) ◽  
pp. 281-281
Author(s):  
Sigeyuki Takemura ◽  
Hirosi Maeda ◽  
Yoshihide Mitani ◽  
Kimitoshi Tanaka
Keyword(s):  

Diversity ◽  
2021 ◽  
Vol 13 (11) ◽  
pp. 574
Author(s):  
Wasiatus Sa’diyah ◽  
Akira Hashimoto ◽  
Gen Okada ◽  
Moriya Ohkuma

The diversity of sporocarp-inhabiting fungi (SCIF) was examined using six samples of xylarialean fungi from two different forests in Ibaraki Prefecture, Japan: a moist forest in the Sakuragawa area and an urban dry forest in the Tsukuba area. These fungi were enumerated using direct observation and dilution plate methods. We obtained 44 isolates, and careful morphological and molecular phylogenetic studies of these isolates revealed that approximately 30% of the operating taxonomic units were undescribed or cryptic species related to known fungi. Although typical mycoparasitic fungi, such as helotialean fungi and Trichoderma spp., were not isolated, the genera Acremonium, Acrodontium, and Simplicillium were detected. Comparisons of SCIF communities between the two forests suggested that the number of isolated species in the Sakuragawa area was lower than that in the Tsukuba area. Soil-borne fungi, such as Aspergillus, Beauveria, Penicillium, and Talaromyces, or polypores/corticioid mushrooms, are frequently detected in the Tsukuba area. Factors affecting SCIF communities in the two forests are discussed. Some noteworthy fungi are briefly described with notes on taxonomy, ecology, and molecular phylogeny.


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