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Geological Survey Reston, Virginia 22092 PREGEDING PAGE BLANK NOT FILMED ABSTRACT The Columbia Plateau is surrounded by a com-plex assemblage of highly deformed Precambrian Here, the bare-bedrock weathering rate is 14 m/ m.y., and h and h represent stable equilib-rium regolith thicknesses. This record is maintained in the National Geologic Map Database (NGMDB). Detailed report of standardization procedures. Weathering rate, W(h) (m/m.y.) A new geologic map by the Oregon Department of Geology and Mineral Industries (DOGAMI) covers the Mt. the geologic map of the Galice-Kerby-Waldo region (PL VI). BEDROCK GEOLOGY Lithostratigraphy Yeats and others (1996) and Snavely and Wells (1996) provided comprehensive summaries of the bedrock geology in the Luckiamute region. Geologic maps help scientists identify sites of orogenic event s (mountain-building), for instance. dary schools of Oregon and Montana. Using LIDAR they can see where the Missoula flood scrapped some areas to bedrock and deposited gravel beds in others. Most of the maps are posted and maintained by state geologic survey organizations. Washington Geology App; Washington Geologic Survey Publications Catalog; GIS Data and Databases; Presentation Archive; Lidar; Story Maps; Geologic Maps. Bedrock and Geologic History The Blue Mountains landscape resulted from the erosion of bedrock as it was uplifted during about the last 15 million years. Dashed lines represent alluvial surface low-ering rates (labeled e and e [m/m.y.]). This digital map database, compiled from previously published and unpublished data, and new mapping by the authors, represents the general distribution of bedrock and surficial deposits of the Deer Island 7.5-minute quadrangle. Unfortunately, in many places the bedrock is covered by water, dirt, plants, pavement, buildings, or other coverings which obscure the area's bedrock. Multipurpose bedrock, surficial, and environmental geologic maps have recently been completed for portions of the Valley and Ridge province of southwest VA. Characteristics of bedrock and surficial geologic terranes and structural features at various levels of detail. The geology at the John Day Fossil Beds can be split into two broad categories: physical and historical. incipient channels in many arid . Multipurpose bedrock, surficial, and environmental geologic maps have recently been completed for portions of the Valley and Ridge province of southwest VA. The geology of the Burns Butte 7.5ʹ quadrangle was mapped by the Oregon Department of Geology and Mineral Industries (DOGAMI) during 2019 and 2020 (Figure 1 1; Plate 1). Purchase this map online through Shop ISGS*, or contact the Sales and Information Office for more information. OREGON LINCOLN IDAHO FRANKLIN s ke e r m nt r n tn e c e e y t s t d r p ak m h s nt s e h r n e am ne s h on a e s e es ke le ia t s r ia nt r . The map area contains the westernmost portion of the Columbia River Gorge National Scenic area as well as the rapidly growing areas surrounding the Clark County, Washington, cities of Camas and Washougal. The volcanic and volcaniclastic rocks within the area are calc-alkaline and range in composition from olivine basalt to rhyolite. Changes in U.S. Quaternary Geology and Geomorphology of the Lower Deschutes River Canyon, Oregon Jim E. O'Connorl. Millions of years later came a series of floods so high it covered the entire Willamette Valley with four hundred feet of water at its height. The CSZ runs roughly north to south for over 1100 km just offshore. Bedrock in geology is solid rock that lies under loose softer material (regolith) within the crust of Earth or another terrestrial planet. Bibliography: p. 38-39. In the following we report the results of a simple test of (4) using topographic maps from the Coast Ranges of Oregon, USA, which appear to support this technique, yielding a ratio of m/n equal to 1.0 for low gradient channels and greater than 1.0 for slopes steeper than 0.2 where debris flows dominate erosion. Beer 49% 48% . In September 1966, he returned to Montana State University to pursue a degree of Master of Science in Applied Science (Earth Sciences, . Friday, March 13, 5:30-8:30 p.m. and Saturday, March 14, 8:45 a.m.-5:00 p.m. Geology of Central Oregon suspended due to COVID-19 (Coronavirus) pandemic. User account menu. Using examples from the Willamette Valley of Oregon, terroir of the region will be discussed because it is strongly influenced by the bedrock geology and soils. He has been teaching high school in southern Oregon for over a dozen years now and is a member of . The maps, at both 1:100,000 and 1:24,000 scales, show generalized and detailed bedrock geology grouped by lithology and environmental hazard associations. Digital Geologic map of the Hood River Valley, Hood R iver and Wasco C ounties . If you need higher-resolution images for any content in this item, please contact us at repository@u.library.arizona.edu. The map was originally compiled on 1:400,000-scale quarters of the early 1980's version of the Oregon base map for publication at 1:500,000. From the south beach of Seward Park's Bailey Peninsula, the panorama is dominated by Mount Rainier and Lake Washington. Rocks of Late Jurassic age are assigned to the Otter Point Formation and are a complex mixture of types that include graywacke sandstone, greenstone, and chert. SURFICIAL AND BEDROCK GEOLOGIC MAP OF THE DIXON MOUNTAIN 7.5' QUADRANGLE, SOUTHWEST MONTANA Nathan W. Harkins † Diana K. Latta ‡ David J. Anastasio § Frank J. Pazzaglia § Earth and Environmental Sciences Department Lehigh University, Bethlehem, PA Montana Bureau of Mines and Geology Open File Report MBMG 495 2004 The geology of the Deer Island quadrangle is dominated by four main packages of deposits separated by regional unconformities: Paleogene bedrock, Miocene flood-basalt flows of the Columbia River Basalt Group, late Miocene and Pliocene alluvial deposits of the ancestral Columbia River, and Quaternary deposits of the modern river and its tributaries. Bedrock consists largely of basalt and basaltic andesite flows that erupted during late Oligocene time from one or more vents located outside the map area. The flanks of the basin consist of Eocene through Miocene volcanic and sedimentary rocks that rise to elevations exceeding 2000 ft (610 m). The maps, at both 1:100,000 and 1:24,000 scales, show generalized and detailed bedrock geology grouped by lithology and environmental hazard associations. Geological map data. The bedrock geology of the project area has generally been mapped on a reconnaissance basis. Geology. This item was digitized from a paper original and/or a microfilm copy. Ferns, H.C . From the Atlantic coast on the east to the Appalachian Plateau on the west, Maryland has a great variety of geology and landforms. Figure 1. GEOLOGY presented on May 26, 1982 Title: THE BEDROCK GEOLOGY OF THE SOUTHEAST PART OF SHASTA VALLEY, SISKIYOU COUNTY, CALIFORNIA. It is for informational purposes and may not be suitable for legal purposes. AAPG geologic province: Columbia basin. Geologic features were generalized in the Geologic Map of Illinois at scale 1/500,000 (Kolata 2005). INTRODUCTION The Dalton Highway was originally buff t as a haul road for construction of the trans-Alaska pipeline, and has now been opened to the public from L i vengood to the southern Brooks Range.Reconnaissance geological quadrangle maps at 1:250,000 scale show the bedrock geology of the region crossed by the highway between Livengood and the North Slope; several of these maps were Since 1993, the USGS-STATEMAP geological mapping program has mapped eight quadrangles in the Dixon-Oregon-Rochelle area (Oregon and The primary objective of the U.S.-Mexico border project is to provide framework geology through geologic mapping activities to support border-wide science investigations including assessing and evaluating groundwater, energy and mineral, and ecological resources, and identifying and . Wonderfully designed map of the world showing the bedrock geology of oceans and land. The Oregon Coast Range is an ideal geomorphic laboratory, with homogeneous bedrock lithology, uniform annual precipitation rates and remaining unglaciated during the Pleistocene (Kobor and Roering, 2004). canic arc of Oregon USA include failure of debris dams [1], capture of surface drainage by the groundwater . Marli has authored and co-authored several books on the geology of Oregon and Washington, including Roadside Geology of Oregon, Roadside Geology of Washington, Oregon Rocks! [no type designated]. The oldest dated lava flows yield a -K-Ar age of 9.2 .6 m.y,and the youngest flows are younger than 10,000 years. F IGURE 1.—Index map showing topographic sheets and geologic folios published for southwestern Oregon. We will attempt to trace geochemical signatures of the bedrock as it breaks down . The major geological factors are: The volcanic mountains of the Cascades. Prints and layouts can be customized or edited to your needs, just cm long (15.7 in) hammer for scale. Ireland Quadrangle, Baker and Grant Counties, Oregon, was prepared by M.L. Oregon Bedrock Geology cross stitch PDF pattern download BlondeBoxshell 5 out of 5 stars (187) $ 4.40. The creation of Willamette Falls is the story of two floods. The "captive" pebbles wear circular holes in the bedrock. The Gales Creek fault (GCF) is a 60-km-long, northwest-striking dextral fault system (west of Portland, Oregon) that accommodates northward motion and uplift of the Oregon Coast Range. Compile project data from sources listed below. Timeline of Oregon's Main Geologic Events --from Oregon Rocks! Personius (1995) and Reneau and Dietrich (1991) documented uplift and sediment yield rates in the OCR, other studies of erosion BEDROCK FORMS GEOLOGY & SOILS: SOUTHERN OREGON 200 MILLION YEARS ACO PACIFIC OCEAN COAST REACHES IDAHO The Juan de Fuca tectonic plate begins to gradually subduct under the North American tectonic plate • Ocean islands and pieces of the ocean bottom are "stuck" onto the West Coast as accreted terrane, creating Oregon's oldest mountains GEOLOGIC MAPS OF WASHINGTON QUADRANT MAPS (scale 1:250,000) WASHINGTON STATE . -to be available in April Using the cross-section, you can come up with a geologic timeline like the one above. Add to Favorites . At the center of the Earth is the molten metal core, surrounded by the rocky mantle and then the outer crust . The item Geologic map of the Washougal quadrangle, Clark County, Washington, and Multnomah County, Oregon, by Russell C. Evarts, Jim E. O'Connor, and Terry L. Tolan represents a specific, individual, material embodiment of a distinct intellectual or artistic creation found in University of Missouri-Kansas City Libraries. Geologic Background Most of the bedrock of this part of the coastal region was laid down on the sea floor during the Tertiary Period when the Pacific Ocean extended inland over part of western Oregon. Bedrock in Oregon (2 C) Biogeology of Oregon (1 C) C. Caves of Oregon (11 C, 59 F) D. Deposition (geology) in Oregon (9 C) E. Earthquakes in Oregon (2 C, 6 F) Effects of tectonics in Oregon (3 C) Erosion in Oregon (12 C, 15 F) F. The Preliminary Interpretive Report 2004-3B, "Bedrock geologic map of the Livengood SW C-3 and SE C-4 quadrangles, Tolovana mining district, Alaska," is the bedrock geologic map of an approximately 123-square-mile area in the central Livengood Quadrangle, Alaska. This record is maintained in the National Geologic Map Database (NGMDB). The Coaledo Field Trip commences at the Alfred Tyson Park in Elkton. We found that streams draining catchments with permeable bedrock geology at the Drift Creek watershed in the Oregon Coast Range had longer mean transit times than catchments with poorly permeable bedrock at the HJ Andrews Experimental Forest in the Oregon Cascades. The following links will take you to state geologic maps. . [and others] represents a specific, individual, material embodiment of a distinct intellectual or artistic creation found in Indiana State Library. Geologic map of the Deer Island quadrangle, Columbia County, Oregon and Cowlitz County, Washington Metadata Updated: March 22, 2021 This digital map database, compiled from previously published and unpublished data, and new mapping by the authors, represents the general distribution of bedrock and surficial deposits of the Deer Island 7.5 . To learn more about your state survey, visit The Association of American State Geologists . Bedrock is comprised of an Eocene to Oligocene sequence of basaltic volcanic rocks, marine sedimentary rocks, and mafic intrusives of varying composition (Figure 3). This archived document is maintained by the Oregon State Library as part of the Oregon Documents Depository Program. Shaded relief base map compiled from U.S. Geological Survey 30-m elevation data and National Oceanic and Atmospheric Administration as a function of regolith thickness, h (m). similar geology and climate. 194. The two-color map, Geology and Mineral Resources Map of the Mt. Info: Oregon geologic map data Found the internet! Well Water Program. map U.S. Geological Survey Open-File Report 95-0680 paper 197777 publication date Jennings (1977) Source of geologic information of California The state geologic maps were processed digitally, as follows: the source material was scanned, the lines and polygons were edited and proofed, attributes were added and proofed, the maps were transformed from scanner units to geographic coordinates, and . The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The most common lava flows are platy jointed, cliff-forming basaltic ande- Thesis: "Geologic structure and exhumation accompanying Yakutat terrane collision, southern Alaska", 49 p. Punke, M. L., PhD, 2005 Thesis: "Paleoenvironmental reconstruction of an active margin coast from the Pleistocene to the present: examples from southwestern Oregon, 171 p. Blair, Mehgan, MS, 2005 A geologic map of the United States reveals a continuous bedrock formation, more than 400 million years old, stretching from northern Georgia all the way through Maine. Surface Geology; 3D Geology; Subsurface Geology; Education and Outreach; Energy, Mining and Minerals. Wine 16% 40% . The project will focus on physical and chemical weathering of volcanic rocks and factors that can influence the weathering processes, including climate and vegetation. Log In Sign Up. A target date for resuming regular operations is undetermined at this time. Bedrock Geology of Oregon Quadrangle, Ogle County, Illinois. Bedrock lithologies in the western Crater Mountains consist of silicic to mafic volcanic rocks of late Oligocene to middle Miocene age (Gray and others, 1988) with latite flows capping granite bedrock are here combined with detailed tensiomet-ric data in the area contributing to the trench. Hydrologic and physiographic characteristics of the basin are related to underlying geologic mate-rials. A Guide to Geology Sites in the Centennial State. Bela, J.L., compiler, 1982, Geologic and neotectonic evaluation of north-central Oregon-The Dalles 1 degree by 2 degree quadrangle: Oregon Department of Geology and Mineral Industries Geological Map Series GMS-27, 2 sheets, scale 1:250,000. Mount Rainier is a reminder that Seward Park owes its existence to the Cascade volcanos, which began erupting some 40 million years ago and through erosion supplied the bedrock that makes up the Bailey Peninsula. Maryland Geology. • Bedrock geology • Soils: texture, structure, depth of soil, drainage, color, age • Orientation of slope • Elevation "80% of the quality in wine Janet H. Curran2, Robin A. Beebee3, Gordon E. Grant4, and Andrei Sarna-Wojcickis The morphology of the Deschutes River canyon downstream of the Pelton-Round Butte dam complex is the product of the regional geologic history, the composition of Summary: Named for gravels and sands deposited by ancestral Columbia River near Troutdale, Multnomah Co, OR. GIS style files. A Guide to 60 Amazing Geologic Sites, and Colorado Rocks! Both trench outflows and the patterns of soil moisture status are com-pared to patterns of the upslope contributing areas and topographic index derived using both soil surface and bedrock surface topography. -FINE ART PRINTING- Each print is made to order and hand printed in Portland, Oregon. Bedrock lithologies in the northern Growler Mountains consist of silicic to mafic volcanic rocks and some associated volcaniclastic sediments of Oligocene to middle Miocene age (Gray and others, 1988). Both of these categories are . Portland State University, Portland Oregon . 6, p. 831-930. Frank Hladky, registered geologist who worked for DOGAMI (Oregon Department of Geology and Mineral Industries) for 22 years, came to talk to GSOC about how he used his geological background to transform himself into a high school science teacher. The item Geologic map of the Carlton quadrangle,Yamhill County, Oregon, by Karen L. Wheeler . Abstract approved: Approximately 25 square miles of the southeast part of Shasta Valley are included in the thesis area, which lies about 12 miles northeast of Weed, California. Preliminary integrated geologic map databases for the United States - western states: California, Nevada, Arizona, Washington, Oregon, Idaho, and Utah. Ireland quadrangle, a traditional mining area on the border between Baker and Grant Counties. Geology Faculty Publications and Presentations Geology 12-2014 . U.S.-Mexico Border Geologic Framework. [bedrock]: Whetten and others, 1988, USGS I -1198 G Port Townsend [surficial]: Pessl and others, 1989, See report for details on how each source was used. geologic map Oregon, Oregon geology, Geology of Oregon, Earth Science, bedrock Geologic Map of Oregon Oregon displays an amazing variety of fascinating geology, from its accreted terranes on the southern coast and in the Blue Mountains area to its Miocene age Columbia River flood basalt to its active volcanism in the Cascade Range. July 14, 2017. Add to Favorites Ontario Bedrock Geology cross stitch PDF pattern download BlondeBoxshell 5 out of 5 stars (187) $ 4.40. Young Wine Maker 1973 Leysin, Switzerland . The group is delighted to examine the river bedrock of Tyee sandstone. Specif ically, the late fvliocene and Pliocene rocks of southern and eastern Oregon, the Paleozoic rocks of central and northeastern Oregon, and the Triassic rocks of northeastern Oregon ore poorly understood. Bedrock Geology of The Northern Columbia Plateau and Adjacent Areas DONALD A. SWANSON U.S. Geological Survey Menlo Park, California 94025 THOMAS L. WRIGHT and IAS. Oregon Department of Geology and Mineral Industries Open-File Report O-12-03 25. These data were digitized by USGS NMD Thematic Map Unit and then reprojected to the new (late 1980's) Oregon 1:500,000-scale state base map. In some places, such as the north side of the Wallowa or Strawberry Mountains, faulting localized the uplift, visible today as abrupt and straight mountain fronts. Special mention should be made also of Frank M. Anderson, who Deposit is great piedmont fan lying on . Part or all of this report is presented in Portable Document Format (PDF). Maryland is part of six physiographic provinces (shown in the figure below). The NGMDB is a Congressionally mandated national archive of geoscience maps, reports, and stratigraphic information, developed according to standards defined by the cooperators, i.e., the USGS and the Association of American State Geologists (AASG). The large letters on both the timeline and cross-section refer to the 7 locations described here while the many small numbers on the cross-section and time line . Category:Geology of Oregon . Geologic Information Portal. Publication: Hodge, E.T., 1938, Geology of the Lower Columbia River: Geological Society of America Bulletin, v. 49, no. The geology of the Pacific Northwest includes the composition (including rock, minerals, and soils), structure, physical properties and the processes that shape the Pacific Northwest region of North America.The region is part of the Ring of Fire: the subduction of the Pacific and Farallon Plates under the North American Plate is responsible for many of the area's scenic features as well as . Twelve of the sixteen essential elements for wine grapes come from the soil. Two 36" × 30" map sheets; sheet 1 contains map and legends; sheet 2 includes descriptive stratigraphic column, cross section, and descriptive text. The ancient folded mountains of the Coast Range. Mercator projection that includes key with eras and types. Supplemental_Information: The 16 layers listed below are present as shape files. Huge basalt flows that oozed out over the landscape. Informational graphics on the sides with bonus info about the . It is evident that most of central and eastern Oregon is in need of more detailed mapping. First came a flood of lava creating the foundational basalt bedrock that shaped the falls we know today. Methodology. r/geology. Outcropping bedrock is great stuff, because it allows geologist to determine the local geology, and helps them put together the geologic history of the earth. The NGMDB is a Congressionally mandated national archive of geoscience maps, reports, and stratigraphic information, developed according to standards defined by the cooperators, i.e., the USGS and the Association of American State Geologists (AASG). All around the world the geology and soils make up an important component of the terroir of the wine. U.S. Geological Survey, Portland, Oregon Within the Deschutes River basin of central Oregon, the geology, hydrology, and physiography influence geomorphic and ecologic processes at a variety of temporal and spatial scales. The secret to unlocking the story of Oregon's groundwater requires a basic understanding of the geology of the region. The information provided here are intended for use in the synoptic study of large areas, and are likely not suitable for detailed study of geog. The bedrock geology of the project area has generally been mapped on a reconnaissance basis. central Oregon Coast Range (OCR) study area, which is underlain by the Eocene Tyee Formation and overlying Elkton Formation. We also found that differences in permeability contrasts within the subsurface . One map on folded leaf in pocket with title: Geologic map of the St. Helens Quadrangle, Oregon-Washington. The Geology of Central Oregon workshops are currently on hiatus from their regular in-person programming. To provide to the public a digital geologic map database of Oregon. Drinking Habits Drink 1982 2012 . Some of the bedrock units (geologic formations) were erupted from local volcanoes, while others were carried into the sea by rivers. This project is based in the High Cascades of central Oregon and the Deschutes Basin and integrates studies of bedrock, soil, and water chemistry. The Washougal 7.5' quadrangle spans the boundary between the Portland Basin and the Columbia River Gorge, approximately 30 km east of Portland, Oregon. What layer is bedrock in real life? A physiographic province is a geographic area in which the geology (including lithology and structure) and climate . 806 GEOLOGY, October 2006 Figure 2. New geologic mapping and geophysical models confirm inferred offsets from earlier geophysical surveys and document ∼12 km of right-lateral offset of a basement . The Columbia River flows west and north through the Portland Basin at an elevation near sea level and exits through a confined bedrock valley less than 2.5 km wide about 16 km north of Saint Helens. Rules, Regulations and Forms; Geothermal Resources; Oil and . The rocks exposed in the area range This map from the State of Oregon on the Portland area is super cool. In this paper, we focus on the characteristics of the pumice deposit, bedrock geology, and identify the sources
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bedrock geology of oregon
- 2018-1-4
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- 2018年シモツケ鮎新製品情報 はコメントを受け付けていません
あけましておめでとうございます。本年も宜しくお願い致します。
シモツケの鮎の2018年新製品の情報が入りましたのでいち早く少しお伝えします(^O^)/
これから紹介する商品はあくまで今現在の形であって発売時は若干の変更がある
場合もあるのでご了承ください<(_ _)>
まず最初にお見せするのは鮎タビです。
これはメジャーブラッドのタイプです。ゴールドとブラックの組み合わせがいい感じデス。
こちらは多分ソールはピンフェルトになると思います。
タビの内側ですが、ネオプレーンの生地だけでなく別に柔らかい素材の生地を縫い合わして
ます。この生地のおかげで脱ぎ履きがスムーズになりそうです。
こちらはネオブラッドタイプになります。シルバーとブラックの組み合わせデス
こちらのソールはフェルトです。
次に鮎タイツです。
こちらはメジャーブラッドタイプになります。ブラックとゴールドの組み合わせです。
ゴールドの部分が発売時はもう少し明るくなる予定みたいです。
今回の変更点はひざ周りとひざの裏側のです。
鮎釣りにおいてよく擦れる部分をパットとネオプレーンでさらに強化されてます。後、足首の
ファスナーが内側になりました。軽くしゃがんでの開閉がスムーズになります。
こちらはネオブラッドタイプになります。
こちらも足首のファスナーが内側になります。
こちらもひざ周りは強そうです。
次はライトクールシャツです。
デザインが変更されてます。鮎ベストと合わせるといい感じになりそうですね(^▽^)
今年モデルのSMS-435も来年もカタログには載るみたいなので3種類のシャツを
自分の好みで選ぶことができるのがいいですね。
最後は鮎ベストです。
こちらもデザインが変更されてます。チラッと見えるオレンジがいいアクセント
になってます。ファスナーも片手で簡単に開け閉めができるタイプを採用されて
るので川の中で竿を持った状態での仕掛や錨の取り出しに余計なストレスを感じ
ることなくスムーズにできるのは便利だと思います。
とりあえず簡単ですが今わかってる情報を先に紹介させていただきました。最初
にも言った通りこれらの写真は現時点での試作品になりますので発売時は多少の
変更があるかもしれませんのでご了承ください。(^o^)
bedrock geology of oregon
- 2017-12-12
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- 初雪、初ボート、初エリアトラウト はコメントを受け付けていません
気温もグッと下がって寒くなって来ました。ちょうど管理釣り場のトラウトには適水温になっているであろう、この季節。
行って来ました。京都府南部にある、ボートでトラウトが釣れる管理釣り場『通天湖』へ。
この時期、いつも大放流をされるのでホームページをチェックしてみると金曜日が放流、で自分の休みが土曜日!
これは行きたい!しかし、土曜日は子供に左右されるのが常々。とりあえず、お姉チャンに予定を聞いてみた。
「釣り行きたい。」
なんと、親父の思いを知ってか知らずか最高の返答が!ありがとう、ありがとう、どうぶつの森。
ということで向かった通天湖。道中は前日に降った雪で積雪もあり、釣り場も雪景色。
昼前からスタート。とりあえずキャストを教えるところから始まり、重めのスプーンで広く探りますがマスさんは口を使ってくれません。
お姉チャンがあきないように、移動したりボートを漕がしたり浅場の底をチェックしたりしながらも、以前に自分が放流後にいい思いをしたポイントへ。
これが大正解。1投目からフェザージグにレインボーが、2投目クランクにも。
さらに1.6gスプーンにも釣れてきて、どうも中層で浮いている感じ。
お姉チャンもテンション上がって投げるも、木に引っかかったりで、なかなか掛からず。
しかし、ホスト役に徹してコチラが巻いて止めてを教えると早々にヒット!
その後も掛かる→ばらすを何回か繰り返し、充分楽しんで時間となりました。
結果、お姉チャンも釣れて自分も満足した釣果に良い釣りができました。
「良かったなぁ釣れて。また付いて行ってあげるわ」
と帰りの車で、お褒めの言葉を頂きました。