Prince Silver (CSE:PRNC,OTC:HWTNF) is a Vancouver-based exploration company advancing the Prince Silver project in southeastern Nevada. In July 2025, the company completed the transformational acquisition of Stampede Metals Corporation and rebranded from Hawthorn Resources to Prince Silver Corp. The flagship Prince project is a district-scale, past-producing silver-gold-zinc-manganese carbonate replacement system, historically mined for silver and base metals in the early to mid-1900s.
Aerial view of the Prince silver projectFully funded and technically refreshed, the company’s near-term priority is to validate and build upon the 129 historic drill holes (over 16,600 m) completed on the property, with the goal of converting the large JORC-compliant exploration target into a maiden NI 43-101 mineral resource.
A drill program is scheduled to begin in early September 2025, targeting the validation of legacy data, step-outs along mineralized trends, and continuity across the deposit’s multiple mantos, veins, and breccia zones. In parallel, the company will undertake metallurgical test work, geophysical refinement, and updated geological modeling to support a modern pit-constrained resource and underpin a longer-term development strategy.
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With a strong asset foundation, a clean capital structure and an experienced technical team, Prince Silver is well-positioned to capitalize on the current macro tailwinds in the silver and manganese markets.
Prince Silver (CSE:PRNC,OTC:HWTNF) is a Vancouver-based exploration company focused on unlocking value at the Prince silver project in southeastern Nevada. In July 2025, the company completed a transformational acquisition of Stampede Metals Corporation and subsequently rebranded from Hawthorn Resources to Prince Silver Corp. The flagship asset is a district-scale, past-producing silver-gold-zinc-manganese carbonate replacement system, historically mined for silver and base metals through the early to mid-1900s.
Aerial view of the Prince silver project
Fully funded and technically refreshed, the company’s immediate objective is to validate and expand upon the 129 historic drill holes (over 16,600 m) completed on the property and convert the large JORC-compliant exploration target into a maiden NI 43-101 mineral resource. The upcoming drill program, expected to begin in early Sept 2025, is designed to validate legacy data, step out along mineralized trends, and establish continuity across the deposit's multiple mantos, veins and breccia zones. The company will also initiate metallurgical test work, geophysical refinement and updated geological modeling to support a modern pit-constrained resource and longer-term development plan.
The Prince silver project is a large-scale, polymetallic carbonate replacement deposit (CRD) located just west of Pioche, a historic mining district in southeastern Nevada. The project hosts a structurally and stratigraphically controlled system of silver-rich mantos, breccias and fissure veins emplaced along northeast-trending faults within the Cambrian Pioche Shale. Historical underground production between 1912 and 1949 totaled approximately 1.12 million tons (Mt) at average grades of 100 grams per ton (g/t) silver, 4.5 percent zinc, 2.8 percent lead, and 10 percent manganese, predominantly from shallow workings in the Main and Ridge Zones.
Geological mapping, relogging and compilation of 129 historic drill holes (16,606 m) have defined a JORC exploration target ranging between 25 and 43 Mt, grading approximately 37 to 40 g/t silver, 1.5 percent zinc, and 0.8 percent lead. This target includes three dominant mineralized zones: Ridge, Main and Prince Extended. Mineralization is generally tabular, strataform and laterally continuous, with multiple stacked mantos and vein swarms, often associated with jasperoid, manganese-rich breccias and semi-massive to massive sulfides. The projects’ mineralization remains open along strike and at depth in all directions.
Historical drill results
Historical drill results showing mineralization at the Prince Silver Project is near surface and open in all directions of modelled mineralized horizons
Prince Silver’s 2025 Phase-1 drill program (~6,500 m of RC drilling) is designed to:
A follow-up Phase-2 program (expected in 2026) would target resource expansion along the 2.5-km trend and scout new targets identified via geophysics and structural interpretation. In parallel, the company plans to conduct metallurgical testing to evaluate optimal processing options. Surface rights include 20 unpatented lode claims and 12 patented claims under lease option. The lease agreement includes nominal cash payments and a staged buyout option upon completion of a preliminary economic assessment. The project has good access via gravel roads, with power available on site, and is within 15 km of Pioche community infrastructure.
A large, early-stage porphyry target in Nevada featuring over 200 claims. Historical geophysics identified multiple IP-resistivity anomalies, and a single 700 m drill hole encountered extensive skarn alteration before terminating in mineralization. No current plans for exploration in 2025.
A legacy polymetallic silver-lead-zinc project with limited historical data. Considered non-core for now; the company’s resources remain focused on advancing Prince Silver.
Ralph Shearing is a professional geologist and mine developer with over 35 years in mineral exploration development and public company management. Since 1987, he has held senior executive positions with public junior mining and exploration companies, primarily with Luca Mining Corp., a company he founded in 1986 and successfully guided through the exploration, initial development and construction, and pre-production phases of the Tahuehueto mine, located in Durango, México. He currently acts as Qualified Person for Prince Silver’s technical disclosure.
Rob Scott has more than 25 years of experience in accounting, corporate compliance, corporate finance, and merchant and commercial banking. He has played a key role in raising more than $200 million in equity financing. Scott has held senior executive and board positions with several TSX-V listed companies, including Great Bear Resources, ValOre Metals, Riverside Resources, Capitan Silver and First Helium.
Robert Wrixon is a seasoned executive and engineer with over 20 years’ experience across ASX- and LSE-listed mining companies. He holds a PhD in mineral engineering from UC Berkeley and brings deep technical, corporate development and M&A experience.
Darrell Rader is the president and CEO of Minaurum Gold, a silver-focused explorer in Mexico, and a prominent figure in North American silver exploration. He has directly raised over $150 million for mineral exploration and development and has strong relationships with institutional investors and bankers. He founded Defiance Silver, a silver developer, and previously was the head of corporate development with silver miner IMPACT Silver. Rader holds a BBA in Finance from Simon Fraser University.
A veteran mining executive, Neil MacRae has more than two decades of experience in investor relations and has held various investor relations roles with companies such as First Majestic Silver, Sherwood Copper (merged with Capstone in 2008), Farallon Mining (sold to Nyrstar in 2011), and Santacruz Silver Mining. He provides strategic direction on corporate visibility and capital markets positioning.
Advancing the large-scale Prince Silver project in Nevada
Hawthorn Resources Corp. (HWTN) has announced a name and symbol change to Prince Silver Corp. (PRNC) and a consolidation of its issued and outstanding common shares on the basis of zero point seven five (0.75) post-consolidated common share for every one (1) pre-consolidated common shares.
As a result, the outstanding shares of the company will be reduced to approximately 16,054,125 common shares.
The shares will begin trading on a consolidated basis and with a new name, symbol, and CUSIP number on July 11, 2025.
Please note that all open orders will be canceled at the end of business on July 10, 2025. Dealers are reminded to re-enter their orders taking into account the share consolidation.
_________________________________
Hawthorn Resources Corp. (HWTN) a annoncé un changement de nom et de symbole pour devenir Prince Silver Corp. (PRNC) et une consolidation de ses actions ordinaires émises et en circulation sur la base de zéro point sept cinq (0,75) actions ordinaires post-consolidation pour chaque une (1) action ordinaire pré-consolidation.
En conséquence, le nombre d'actions en circulation de la société sera réduit à environ 16 054 125 actions ordinaires.
Les actions commenceront à être négociées sur une base consolidée et avec un nouveau nom, symbole et numéro CUSIP le 11 juillet 2025.
Veuillez noter que toutes les ordres en cours seront annulés à la fermeture des bureaux le 10 juillet 2025. Les courtiers sont rappelés de ressaisir leurs commandes en tenant compte de la consolidation des actions.
| Trading on a Consolidated Basis/Négociation sur une Base Consolidée : | Le 11 juillet/July 2025 |
| Record Date/Date d'Enregistrement : | Le 11 juillet/July 2025 |
| Anticipated Payment Date/Date de Paiement Prévue : | Le 11 juillet/July 2025 |
| New Name/Nouveau Nom : | |
| New Symbol/Nouveau Symbole : | PRNC |
| NEW/NOUVEAU CUSIP : | 74174A 10 2 |
| NEW/NOUVEAU ISIN : | CA 74174A 10 2 1 |
| Old Symbol/Vieux Symbole : | HWTN |
| Old/Vieux CUSIP & ISIN : | 42047G101/CA42047G1019 |
If you have any questions or require further information please contact Listings at (416) 367-7340 or E-mail: Listings@thecse.com.
Pour toute question ou information complémentaire, veuillez contacter Listings au 416 367-7340 ou par courriel à: Listings@thecse.com.
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Tom Evans, Cloudbreak's MD, commented; "I am excited and delighted we have been able to secure exclusivity on this fantastic opportunity to acquire this asset, in a jurisdiction with significant activity and recent proven success. Located only 40km southwest of the Telfer Gold-Copper Mine operated by Greatland Gold Plc.
Technological advances in geophysics since the 80's have improved greatly with the success of Mobile MT in the Paterson Province, we intend to start off with this geophysical survey, to use as another vector and data layer to refine and rank drill targets not only for copper but for gold as well.
I am excited, for the Company and its shareholders, as we progress this great opportunity and I look forward to updating the market as our exploration programs progress."
Location
The Paterson Project (Figure 1) directly surrounds the Kintyre Uranium Deposit and is located 40km south-south-west of Greatland Gold Plc's Telfer Gold-Copper Mine.
Figure 1: Location Plan
Exploration Completed
The Wanderer Prospect (Figure 2 and 3) was drilled between 1987 and 1990 by CRA (at significantly lower prevailing copper and gold prices) as part of its uranium exploration expenditure across its nearby Kintyre Project. The majority of drilling was only drilled to 100m from the surface, with multiple holes logged as ending in mineralisation. No follow‐up drilling has occurred in the 35 years since then. Forty-two drill holes were drilled at the Wanderer Prospect on E45/5358 tenement.
Multiple significant drilling intercepts include:
Figure 2: Wanderer Prospect Drill Section
Figure 3: Wanderer Prospect- Drill Collar Plan and Mineralised Trend
Deal Terms
Cloudbreak has paid a A$20,000 option fee to secure two months exclusive due diligence across the Paterson Project. If Cloudbreak elects to proceed, it can acquire a 90% interest in the project via the issue of 330,000,000 shares to Mammoth Minerals Ltd (ASX:M79, "Mammoth"). Mammoth is to retain a 10% free carried interest in the Project until the completion of a Definitive Feasibility Study with a positive NPV.
Tenure
The Project consists of three granted exploration licences E45/5358, E45/5391 and E45/6244 covering a land area of 888km2.
The ground is contiguous to the west, of the Cottesloe base-metal project held by Wishbone Gold Plc.
Regional Geology
The Paterson Orogen is a 2,000km long arcuate belt of folded and metamorphosed sedimentary and igneous rocks that range in age from predominantly Palaeoproterozoic to Neoproterozoic with limited outcrops of Archaean rocks.
The eastern margin of the Paterson Orogen is masked by younger Proterozoic to Phanerozoic sedimentary rocks (Officer and Canning Basins) with sedimentary units of the late Proterozoic Savory Basin on-lapping to the southwest. The main outcropping stratigraphic packages across the bulk of the Paterson Project are the lowermost member of the Mesoproterozoic to Neoproterozoic Yeneena Group, the Coolbro Sandstone, and the Paleoproterozoic Rudall Metamorphic Complex.
Local Geology
The Paleoproterozoic Rudall Metamorphic Complex hosts the Central Tenements surrounding the Kintyre Uranium deposit. At and around Kintyre, the prospective Yandagooge Formation outcrops within the Yandagooge Inlier, consisting of a "basement high" of Rudall Metamorphic Complex surrounded by Neoproterozoic sandstone and Permian glacial tillite. The basement sequence has undergone a minimum of four deformation episodes and is unconformably overlain by Neoproterozoic sandstone and conglomerate deposits of the Yeneena Basin, which have seen at least one major deformation episode.
The dominant host-rock to mineralisation at Kintyre is a garnet-rich, chert-banded, calc-silicate magnetite schistose rock, sandwiched between carbonates and shales of the Yandagooge Formation. These are amphibolite facies metamorphosed rocks, later retrogressively metamorphosed to greenschist facies during or prior to the principal mineralisation phase. Late in syn-D3 or during D4 uranium-bearing, hydrothermal fluids were introduced into the system, depositing pitchblende within northeast dipping dilational zones developed in the S3 cleavage.
In the Kintyre area, the Yandagooge Inlier is surrounded by Coolbro Sandstone, which comprises a thick quartz sandstone sequence with intercalated carbonaceous mudstone and shale interbeds (Jackson & Andrew, 1990). The Coolbro Sandstone, which represents the basal formation of the low-grade metamorphic Neoproterozoic Yeneena Supergroup, exhibits a strong slaty cleavage and has been isoclinally folded and deformed around NW trending axes.
The Central Tenements around the Kintyre deposit are predominantly covered by outcropping northwest-southeast trending, northerly dipping, and folded Coolbro sandstone. Aeolian sand covers areas in the west-central and southeast portions of the tenement. It is believed that these areas are directly underlain by an inlier of the Yandagooge Formation Rudall Metamorphics (Jackson & Andrew, 1990). Rudall Metamorphics outcrop in the west-central area and near the south-eastern corner of the tenement. The north eastern edge of the tenement has outcropping northwest-southeast trending, northerly dipping, and folded Broadhurst Formation.
Exploration Potential and Prospectivity
The Paterson Province hosts several major copper and gold operations, including the Nifty copper mine and the world-class Telfer gold mine. More recently, several new copper-gold discoveries have been made at Winu (Rio Tinto) and Havieron (Greatland Resources PLC???).
A review of a compilation of available geophysical data reprocessed using modern techniques highlights multiple anomalies, including a large "bullseye" magnetic anomaly at Wanderer Prospect within the Central Tenements. The Wanderer Copper-Gold Prospect, first discovered by CRA in 1987, reveals the presence of significant copper, gold and molybdenum values in a wide zone of iron‐oxide alteration extending across more than 1 km of strike. In addition, geochemical assemblage (Cu-Au-Mo) is potentially indicative of a porphyry intrusion as the source of mineralisation. Several other targets with low-magnetics/high gravity signatures have been identified.
At a regional scale, the Paterson Province has potential for large intrusive-related copper and gold targets undercover, requiring geophysical methods, such as Mobile MT by Expert Geophysics Limited, that has been successfully used in the Paterson Province as means of primary target identification.
A review of geophysical and structural data (Figure 4), has identified several compelling exploration opportunities around the existing Wanderer copper-gold project.
Figure 4: RTP Magnetics Left and Gravity Right, illustrating numerous coincident magnetic low and gravity high targets
Cloudbreak Discovery PLC | Peter Huljich, ChairmanTom Evans, Managing Director | Tel: +44 207 887 6139Tel: +44 7851 703440 |
Novum Securities (Financial Adviser) | David Coffman / Anastassiya Eley | Tel: +44 7399 9400 |
Competent Persons Statement
The Information in this report that relates to exploration results, mineral resources or ore reserves is based on information compiled by Mr Edward Mead, who is a Fellow of the Australasian Institute of Mining and Metallurgy. Mr Mead is a consultant to Cloudbreak Discovery Plc and employed by Doraleda Pty Ltd. Mr Mead has sufficient experience which is relevant to the style of mineralisation and type of deposits under consideration and to the activity that he is undertaking to qualify as a Competent Person as defined in the 2012 edition of the `Australian Code for Reporting Exploration Results, Mineral Resources and Ore Reserves' (the JORC Code). Mr Mead consents to the inclusion of this information in the form and context in which it appears in this report.
Table 1: Significant Assays (>0.3% Cu or 0.3ppm Au)
Hole | From (m) | To (m) | Interval (m) | Cu % | Au | Mo ppm |
87WDRC1 | 25 | 28 | 3 | 0.30% | 0 | 6 |
87WDRC10 | 53 | 54 | 1 | 0.31% | 0.25 | 350 |
87WDRC12 | 111 | 115 | 4 | 0.70% | 0.35 | 18 |
87WDRC13 | 101 | 102 | 1 | 0.34% | 0.07 | 34 |
87WDRC13 | 102 | 103 | 1 | 0.35% | 0.09 | 40 |
87WDRC13 | 105 | 106 | 1 | 1.11% | 0.12 | 18 |
87WDRC13 | 108 | 109 | 1 | 0.45% | 0.04 | 33 |
87WDRC13 | 109 | 110 | 1 | 0.88% | 0.06 | 37 |
87WDRC13 | 110 | 111 | 1 | 0.63% | 0.16 | 43 |
87WDRC13 | 111 | 112 | 1 | 0.83% | 0.09 | 38 |
87WDRC14 | 77 | 78 | 1 | 1.22% | 0.15 | 145 |
87WDRC14 | 107 | 110 | 3 | 0.56% | 0.17 | 74 |
87WDRC14 | 110 | 112 | 2 | 0.25% | 0.65 | 18 |
87WDRC14 | 114 | 115 | 1 | 2.11% | 0.59 | 26 |
87WDRC14 | 115 | 116 | 1 | 1.17% | 0.17 | 29 |
87WDRC14 | 116 | 118 | 2 | 2.68% | 0.28 | 22 |
87WDRC14 | 118 | 120 | 2 | 1.82% | 0.15 | 30 |
87WDRC17 | 0 | 5 | 5 | 0.01% | 0.38 | 21 |
87WDRC2 | 84 | 85 | 1 | 0.53% | 0.02 | 460 |
87WDRC2 | 88 | 89 | 1 | 0.89% | 0.04 | 280 |
87WDRC2 | 89 | 90 | 1 | 1.15% | 0.04 | 1270 |
87WDRC2 | 90 | 91 | 1 | 1.68% | 0.03 | 1000 |
87WDRC2 | 91 | 92 | 1 | 4.00% | 0.09 | 610 |
87WDRC2 | 92 | 93 | 1 | 3.61% | 0.06 | 620 |
87WDRC2 | 93 | 94 | 1 | 6.51% | 0.06 | 220 |
87WDRC2 | 94 | 95 | 1 | 1.20% | 0.01 | 15 |
87WDRC2 | 95 | 97 | 2 | 2.34% | 0.03 | 44 |
87WDRC2 | 97 | 99 | 2 | 0.52% | 0.03 | 40 |
87WDRC2 | 99 | 101 | 2 | 0.32% | 0.01 | 49 |
87WDRC22 | 75 | 80 | 5 | 0.62% | 0.16 | 13 |
87WDRC22 | 80 | 85 | 5 | 0.10% | 0.3 | 9 |
87WDRC24 | 70 | 73 | 3 | 0.33% | 0.04 | 34 |
87WDRC24 | 73 | 77 | 4 | 0.71% | 0.09 | 41 |
87WDRC24 | 77 | 80 | 3 | 0.61% | 0.06 | 30 |
87WDRC26 | 82 | 86 | 4 | 0.68% | 0.09 | 28 |
87WDRC3 | 83 | 84 | 1 | 0.45% | 0.01 | 7 |
87WDRC3 | 85 | 86 | 1 | 0.52% | 0.07 | 140 |
87WDRC3 | 86 | 88 | 2 | 0.42% | 0.03 | 69 |
87WDRC6 | 84 | 85 | 1 | 5.18% | 0.29 | 620 |
87WDRC6 | 85 | 86 | 1 | 2.60% | 0.22 | 720 |
87WDRC6 | 86 | 87 | 1 | 2.56% | 0.21 | 350 |
87WDRC6 | 87 | 88 | 1 | 2.31% | 0.18 | 290 |
87WDRC6 | 88 | 89 | 1 | 3.05% | 0.11 | 169 |
87WDRC6 | 89 | 90 | 1 | 1.01% | 0.1 | 81 |
87WDRC6 | 90 | 91 | 1 | 0.57% | 0.04 | 59 |
87WDRC6 | 91 | 92 | 1 | 0.42% | 0.03 | 42 |
87WDRC6 | 92 | 93 | 1 | 0.72% | 0.04 | 121 |
87WDRC7 | 98 | 103 | 5 | 0.31% | 0.01 | 46 |
87WDRC7 | 103 | 104 | 1 | 3.27% | 0.22 | 560 |
87WDRC7 | 104 | 105 | 1 | 0.71% | 0.08 | 360 |
87WDRC7 | 105 | 106 | 1 | 0.34% | 0.09 | 1330 |
87WDRC8 | 83 | 84 | 1 | 0.88% | 0.11 | 200 |
87WDRC8 | 84 | 85 | 1 | 2.01% | 0.26 | 280 |
87WDRC8 | 85 | 86 | 1 | 2.18% | 0.14 | 178 |
87WDRC8 | 86 | 87 | 1 | 2.02% | 0.15 | 260 |
87WDRC8 | 87 | 88 | 1 | 3.23% | 0.18 | 420 |
87WDRC8 | 88 | 89 | 1 | 2.59% | 0.11 | 210 |
87WDRC8 | 89 | 90 | 1 | 1.81% | 0.08 | 200 |
87WDRC8 | 90 | 92 | 2 | 0.39% | 0.01 | 43 |
87WDRC8 | 92 | 94 | 2 | 0.70% | 0.03 | 77 |
88WDD03 | 89 | 90 | 1 | 0.67% | 0.04 | 53 |
88WDD03 | 90 | 91 | 1 | 0.36% | 0.03 | 40 |
88WDD03 | 190 | 191 | 1 | 0.61% | 0.08 | 78 |
88WDD03 | 191 | 192 | 1 | 0.43% | 0.06 | 87 |
88WDRC27 | 43 | 44 | 1 | 0.19% | 0.99 | 24 |
88WDRC28 | 58 | 62 | 4 | 0.48% | 0 | 11 |
88WDRC36 | 90 | 95 | 5 | 0.32% | 0.02 | 9 |
88WDRC36 | 95 | 100 | 5 | 0.46% | 0.1 | 20 |
Table 2: Collar location and Hole Type
Hole ID | Easting | Northing | RL (m) | Total Depth (m) | Dip | Azimuth | Hole Type |
87WDRC1 | 402140 | 7521450 | 430 | 104 | -60 | 180 | RC |
87WDRC2 | 402180 | 7521450 | 430 | 120 | -60 | 180 | RC |
87WDRC3 | 402220 | 7521450 | 430 | 120 | -60 | 180 | RC |
87WDRC4 | 402200 | 7521410 | 430 | 120 | -60 | 180 | RC |
87WDRC5 | 402170 | 7521410 | 430 | 120 | -60 | 180 | RC |
87WDRC6 | 402160 | 7521450 | 430 | 116 | -60 | 180 | RC |
87WDRC7 | 402180 | 7521470 | 430 | 120 | -60 | 180 | RC |
87WDRC8 | 402200 | 7521450 | 430 | 109 | -60 | 180 | RC |
87WDRC9 | 402260 | 7521450 | 430 | 98 | -60 | 180 | RC |
87WDRC10 | 402060 | 7521460 | 430 | 89 | -60 | 180 | RC |
87WDRC11 | 402030 | 7521480 | 430 | 120 | -60 | 180 | RC |
87WDRC12 | 402010 | 7521440 | 430 | 120 | -60 | 180 | RC |
87WDRC13 | 401250 | 7521520 | 450 | 120 | -90 | 0 | RC |
87WDRC14 | 401250 | 7521480 | 450 | 120 | -90 | 0 | RC |
87WDRC15 | 401210 | 7521520 | 450 | 114 | -90 | 0 | RC |
87WDRC16 | 401250 | 7521560 | 450 | 109 | -90 | 0 | RC |
87WDRC17 | 401290 | 7521520 | 450 | 115 | -90 | 0 | RC |
87WDRC18 | 401330 | 7521490 | 450 | 119 | -90 | 0 | RC |
87WDRC19 | 401170 | 7521600 | 450 | 120 | -90 | 0 | RC |
87WDRC20 | 401210 | 7521560 | 450 | 120 | -90 | 0 | RC |
87WDRC21 | 401250 | 7521440 | 450 | 120 | -90 | 0 | RC |
87WDRC22 | 401642 | 7521465 | 450 | 98 | -60 | 180 | RC |
87WDRC23 | 401658 | 7521465 | 450 | 100 | -60 | 180 | RC |
87WDRC24 | 401675 | 7521465 | 450 | 100 | -60 | 180 | RC |
87WDRC25 | 401700 | 7521465 | 450 | 96 | -60 | 180 | RC |
87WDRC26 | 401662 | 7521493 | 450 | 100 | -60 | 180 | RC |
88WDRC27 | 401245 | 7521605 | 450 | 80 | -60 | 240 | RC |
88WDRC28 | 401280 | 7521600 | 450 | 81 | -60 | 240 | RC |
88WDRC29 | 401220 | 7521690 | 450 | 69 | -60 | 250 | RC |
88WDRC30 | 401140 | 7521760 | 451 | 54 | -60 | 250 | RC |
88WDRC31 | 401135 | 7521800 | 448 | 69 | -60 | 240 | RC |
88WDRC32 | 401250 | 7521750 | 450 | 106 | -90 | 0 | RC |
88WDRC33 | 401250 | 7521700 | 440 | 87 | -60 | 200 | RC |
88WDRC34 | 401250 | 7521335 | 450 | 105 | -90 | 0 | RC |
88WDRC35 | 401950 | 7521360 | 430 | 106 | -90 | 0 | RC |
88WDRC36 | 401950 | 7521285 | 450 | 106 | -90 | 0 | RC |
88WDRC37 | 401950 | 7521425 | 440 | 106 | -90 | 0 | RC |
87WDD01 | 401950 | 7521500 | 415 | 287.7 | -61 | 181 | DD |
87WDD02 | 401985 | 7521555 | 440 | 117 | -70 | 180 | DD |
88WDD03 | 401250 | 7521500 | 420 | 212.7 | -90 | 0 | DD |
88WDD04 | 402180 | 7521480 | 434 | 200.8 | -90 | 0 | DD |
90WDD05 | 401950 | 7521425 | 440 | 409.9 | -90 | 0 | DD |
