| Tokawa
Park in summer has lots of families who enjoy breeze from the “water.” |
| Not much water for Mizunashi River |
The Park itself is on the line of contact between Hadano Basin and “Oyama Subgroup 大山亜層群” for Tanzawa Group of geological feature 丹沢層群. We can regard the place as the point where the wrinkles of Philippine Plate start at the aboveground level. This birth story of Hadano tells Tokawa Park is a good place for collecting many kinds of rocks tumbling down from Tanzawa Mountains especially from the surface of shortened crust. In addition, the water systems of steep Tanzawa slopes carry rocks not only from Oyama Subgroup but also from a bit far Togatake and Susugaya Subgroups.
| Mt.
Oyama over there from Tokawa Park. Rolling stones come this far from there, baby. |
The birth order of these geolotical groups is, the oldest Togatake 塔ヶ岳亜層群, the middle Oyama, then the youngest Susugaya 煤ヶ谷亜層群 Subgroups. Togatake and Oyama Subgroup areas have rocks evolved from volcanic magma, mainly Andesites, that cooled rapidly near the surface. They were originally from very active underwater volcanoes so that the chemical reaction with the sea water lets them be colored green. In large rocks procured from the area we can often observe chunks of volcanic bomb trapped and fixed in the volcanic ashes by tectonic pressure. Some good and polished example is situated artfully in the slope of Tokawa Park when we come down from the visitor center to the river. Some are good for using as benches. 😉 Actually, Togatake Subgroup has a strong connection with Yadoriki area 寄. I tell you about it when we look the pebbles in Yadoriki Stream.
| Mr.
Kiyoshi Sudoh of Kanagawa Earth Science Association was our instructor for stone hunting. This rock has volcanic bombs inside, like |
| Bomb
trapped, or so called tuff breccia, of Tanzawa. By the way, the rock itself looks perfect to have lunch on it, don’t you think? |
The dry riverbed of Mizunashi River in Tokawa Park is wide. We walk gravelly fields for some time to reach to the water. Though, for stone hunters of Tanzawa’s tectonic journey it’s a fairly convenient space. We stroll there, even without rainboots, and pick up interesting pebbles. Each doubtlessly has marks of Crash of Titans. The stones here were formulated some 15 to 17 million years ago 240km offshore from the point as undersea volcanic tuff (and occasionally basalt). i.e. The rocks here were the memory of active volcanoes older than Mt. Fuji (; the last eruption was in 1707) or Hakone Mountains (; it’s still erupting). They were carried by the Philippines Plate and arrived here about 5 million years ago. Larger and thicker Eurasian Plate with heavy basalt and peridotite did not yield easily to the pressure from the Philippines Plate. Before came here, the uplift from the bottom of the ocean started to wrinkle at the point of Crush of Titans. Around Tokawa Park area the crustal shortening become ferocious on shore and many fault lines created crumbling rocks. Oh, yes. It’s in present tense. Philippines Plate continues advancing 10cm per year. Do the math. 1 million years produce steady and never- conceding 100km progress ... In the process, many kinds of chemical reactions occurred for tuff and basalt. These straight volcanic products turned into another kind of rocks with different textures and colors. The pebbles we find here underwent such transformations in the relatively shallow part of the Plate, compared with the other areas of Tanzawa. Next week, I’ll show off my catch here. 😊
| Lots of catch here! |
At the entrance of Tokawa Park, there is Tanzawa Visitor Centre. The contact address is
Hadano Visitor Center for Tanzawa-Oyama Quasi-national Park
丹沢大山国定公園・自然公園秦野ビジターセンター
1513 Horiyamashita, Hadano, Kanagawa Prefecture, 259-1304
〒259-1304 秦野市堀山下1513
Phone: 0463-87-9300
https://www.kanagawa-park.or.jp/tanzawavc/
























